---
_id: '1257'
abstract:
- lang: eng
text: We consider products of random matrices that are small, independent identically
distributed perturbations of a fixed matrix (Formula presented.). Focusing on
the eigenvalues of (Formula presented.) of a particular size we obtain a limit
to a SDE in a critical scaling. Previous results required (Formula presented.)
to be a (conjugated) unitary matrix so it could not have eigenvalues of different
modulus. From the result we can also obtain a limit SDE for the Markov process
given by the action of the random products on the flag manifold. Applying the
result to random Schrödinger operators we can improve some results by Valko and
Virag showing GOE statistics for the rescaled eigenvalue process of a sequence
of Anderson models on long boxes. In particular, we solve a problem posed in their
work.
acknowledgement: Open access funding provided by Institute of Science and Technology
(IST Austria). The work of C. Sadel was supported by NSERC Discovery Grant 92997-2010
RGPIN and by the People Programme (Marie Curie Actions) of the EU 7th Framework
Programme FP7/2007-2013, REA Grant 291734.
article_processing_charge: Yes (via OA deal)
author:
- first_name: Christian
full_name: Sadel, Christian
id: 4760E9F8-F248-11E8-B48F-1D18A9856A87
last_name: Sadel
orcid: 0000-0001-8255-3968
- first_name: Bálint
full_name: Virág, Bálint
last_name: Virág
citation:
ama: Sadel C, Virág B. A central limit theorem for products of random matrices and
GOE statistics for the Anderson model on long boxes. Communications in Mathematical
Physics. 2016;343(3):881-919. doi:10.1007/s00220-016-2600-4
apa: Sadel, C., & Virág, B. (2016). A central limit theorem for products of
random matrices and GOE statistics for the Anderson model on long boxes. Communications
in Mathematical Physics. Springer. https://doi.org/10.1007/s00220-016-2600-4
chicago: Sadel, Christian, and Bálint Virág. “A Central Limit Theorem for Products
of Random Matrices and GOE Statistics for the Anderson Model on Long Boxes.” Communications
in Mathematical Physics. Springer, 2016. https://doi.org/10.1007/s00220-016-2600-4.
ieee: C. Sadel and B. Virág, “A central limit theorem for products of random matrices
and GOE statistics for the Anderson model on long boxes,” Communications in
Mathematical Physics, vol. 343, no. 3. Springer, pp. 881–919, 2016.
ista: Sadel C, Virág B. 2016. A central limit theorem for products of random matrices
and GOE statistics for the Anderson model on long boxes. Communications in Mathematical
Physics. 343(3), 881–919.
mla: Sadel, Christian, and Bálint Virág. “A Central Limit Theorem for Products of
Random Matrices and GOE Statistics for the Anderson Model on Long Boxes.” Communications
in Mathematical Physics, vol. 343, no. 3, Springer, 2016, pp. 881–919, doi:10.1007/s00220-016-2600-4.
short: C. Sadel, B. Virág, Communications in Mathematical Physics 343 (2016) 881–919.
corr_author: '1'
date_created: 2018-12-11T11:50:59Z
date_published: 2016-05-01T00:00:00Z
date_updated: 2025-09-22T09:02:32Z
day: '01'
ddc:
- '510'
- '539'
department:
- _id: LaEr
doi: 10.1007/s00220-016-2600-4
ec_funded: 1
external_id:
isi:
- '000374659800005'
file:
- access_level: open_access
checksum: 4fb2411d9c2f56676123165aad46c828
content_type: application/pdf
creator: system
date_created: 2018-12-12T10:15:02Z
date_updated: 2020-07-14T12:44:42Z
file_id: '5119'
file_name: IST-2016-703-v1+1_s00220-016-2600-4.pdf
file_size: 800792
relation: main_file
file_date_updated: 2020-07-14T12:44:42Z
fulldoi: https://doi.org/10.1007/s00220-016-2600-4
has_accepted_license: '1'
intvolume: ' 343'
isi: 1
issue: '3'
language:
- iso: eng
license: https://creativecommons.org/licenses/by/4.0/
month: '05'
oa: 1
oa_version: Published Version
page: 881 - 919
project:
- _id: 25681D80-B435-11E9-9278-68D0E5697425
call_identifier: FP7
grant_number: '291734'
name: International IST Postdoc Fellowship Programme
- _id: B67AFEDC-15C9-11EA-A837-991A96BB2854
name: IST Austria Open Access Fund
publication: Communications in Mathematical Physics
publication_status: published
publisher: Springer
publist_id: '6067'
pubrep_id: '703'
quality_controlled: '1'
scopus_import: '1'
status: public
title: A central limit theorem for products of random matrices and GOE statistics
for the Anderson model on long boxes
tmp:
image: /images/cc_by.png
legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
short: CC BY (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 343
year: '2016'
...
---
_id: '1258'
abstract:
- lang: eng
text: When plants grow in close proximity basic resources such as light can become
limiting. Under such conditions plants respond to anticipate and/or adapt to the
light shortage, a process known as the shade avoidance syndrome (SAS). Following
genetic screening using a shade-responsive luciferase reporter line (PHYB:LUC),
we identified DRACULA2 (DRA2), which encodes an Arabidopsis homolog of mammalian
nucleoporin 98, a component of the nuclear pore complex (NPC). DRA2, together
with other nucleoporins, participates positively in the control of the hypocotyl
elongation response to plant proximity, a role that can be considered dependent
on the nucleocytoplasmic transport of macromolecules (i.e. is transport dependent).
In addition, our results reveal a specific role for DRA2 in controlling shade-induced
gene expression. We suggest that this novel regulatory role of DRA2 is transport
independent and that it might rely on its dynamic localization within and outside
of the NPC. These results provide mechanistic insights in to how SAS responses
are rapidly established by light conditions. They also indicate that nucleoporins
have an active role in plant signaling.
acknowledgement: M.G. received an FPI fellowship from the Spanish Ministerio de Economía
y Competitividad (MINECO). A.G. and A.F.-A. received FPU fellowships from the Spanish
Ministerio de Educación. S.P. received an FI fellowship from the Agència de Gestió
D'ajuts Universitaris i de Recerca (AGAUR - Generalitat de Catalunya). C.T. received
a Marie Curie IEF postdoctoral contract funded by the European Commission. I.R.-V.
received initially an FPI fellowship from the Spanish MINECO and later a Beatriu
de Pinós contract from AGAUR. Our research is supported by grants from the Spanish
MINECO-FEDER [BIO2008-00169, BIO2011-23489 and BIO2014-59895-P] and Generalitat
de Catalunya [2011-SGR447 and Xarba] to J.F.M.-G., and Generalitat Valenciana [PROMETEO/2009/112,
PROMETEOII/2014/006] to M.R.P. and J.L.M. We acknowledge the support of the Spanish
MINECO for the ‘Centro de Excelencia Severo Ochoa 2016-2019’ [award SEV-2015-0533].
We thank the CRAG greenhouse service for plant care; Chus Burillo for technical
help; Sergi Portolés and Carles Rentero for assistance with mutagenesis; Mark Estelle
(UCSD, USA) for providing sar1-4, sar3-1 and sar3-3 seeds; Juanjo López-Moya (CRAG,
Barcelona; 35S:HcPro plasmid) and Dolors Ludevid (CRAG; C307 plasmid) for providing
DNA plasmids; and Manuel Rodríguez-Concepción (CRAG) and Miguel Blázquez (IBMCP,
Valencia, Spain) for comments on the manuscript.
article_processing_charge: No
author:
- first_name: Marcal
full_name: Gallemi Rovira, Marcal
id: 460C6802-F248-11E8-B48F-1D18A9856A87
last_name: Gallemi Rovira
orcid: 0000-0003-4675-6893
- first_name: Anahit
full_name: Galstyan, Anahit
last_name: Galstyan
- first_name: Sandi
full_name: Paulišić, Sandi
last_name: Paulišić
- first_name: Christiane
full_name: Then, Christiane
last_name: Then
- first_name: Almudena
full_name: Ferrández Ayela, Almudena
last_name: Ferrández Ayela
- first_name: Laura
full_name: Lorenzo Orts, Laura
last_name: Lorenzo Orts
- first_name: Irma
full_name: Roig Villanova, Irma
last_name: Roig Villanova
- first_name: Xuewen
full_name: Wang, Xuewen
last_name: Wang
- first_name: José
full_name: Micol, José
last_name: Micol
- first_name: Maria
full_name: Ponce, Maria
last_name: Ponce
- first_name: Paul
full_name: Devlin, Paul
last_name: Devlin
- first_name: Jaime
full_name: Martínez García, Jaime
last_name: Martínez García
citation:
ama: Gallemi M, Galstyan A, Paulišić S, et al. DRACULA2 is a dynamic nucleoporin
with a role in regulating the shade avoidance syndrome in Arabidopsis. Development.
2016;143(9):1623-1631. doi:10.1242/dev.130211
apa: Gallemi, M., Galstyan, A., Paulišić, S., Then, C., Ferrández Ayela, A., Lorenzo
Orts, L., … Martínez García, J. (2016). DRACULA2 is a dynamic nucleoporin with
a role in regulating the shade avoidance syndrome in Arabidopsis. Development.
Company of Biologists. https://doi.org/10.1242/dev.130211
chicago: Gallemi, Marçal, Anahit Galstyan, Sandi Paulišić, Christiane Then, Almudena
Ferrández Ayela, Laura Lorenzo Orts, Irma Roig Villanova, et al. “DRACULA2 Is
a Dynamic Nucleoporin with a Role in Regulating the Shade Avoidance Syndrome in
Arabidopsis.” Development. Company of Biologists, 2016. https://doi.org/10.1242/dev.130211.
ieee: M. Gallemi et al., “DRACULA2 is a dynamic nucleoporin with a role in
regulating the shade avoidance syndrome in Arabidopsis,” Development, vol.
143, no. 9. Company of Biologists, pp. 1623–1631, 2016.
ista: Gallemi M, Galstyan A, Paulišić S, Then C, Ferrández Ayela A, Lorenzo Orts
L, Roig Villanova I, Wang X, Micol J, Ponce M, Devlin P, Martínez García J. 2016.
DRACULA2 is a dynamic nucleoporin with a role in regulating the shade avoidance
syndrome in Arabidopsis. Development. 143(9), 1623–1631.
mla: Gallemi, Marçal, et al. “DRACULA2 Is a Dynamic Nucleoporin with a Role in Regulating
the Shade Avoidance Syndrome in Arabidopsis.” Development, vol. 143, no.
9, Company of Biologists, 2016, pp. 1623–31, doi:10.1242/dev.130211.
short: M. Gallemi, A. Galstyan, S. Paulišić, C. Then, A. Ferrández Ayela, L. Lorenzo
Orts, I. Roig Villanova, X. Wang, J. Micol, M. Ponce, P. Devlin, J. Martínez García,
Development 143 (2016) 1623–1631.
date_created: 2018-12-11T11:50:59Z
date_published: 2016-05-03T00:00:00Z
date_updated: 2025-09-22T09:05:00Z
day: '03'
department:
- _id: EvBe
doi: 10.1242/dev.130211
external_id:
isi:
- '000389588100018'
fulldoi: https://doi.org/10.1242/dev.130211
intvolume: ' 143'
isi: 1
issue: '9'
language:
- iso: eng
month: '05'
oa_version: None
page: 1623 - 1631
publication: Development
publication_status: published
publisher: Company of Biologists
publist_id: '6068'
quality_controlled: '1'
scopus_import: '1'
status: public
title: DRACULA2 is a dynamic nucleoporin with a role in regulating the shade avoidance
syndrome in Arabidopsis
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 143
year: '2016'
...
---
_id: '1259'
abstract:
- lang: eng
text: We consider the Bogolubov–Hartree–Fock functional for a fermionic many-body
system with two-body interactions. For suitable interaction potentials that have
a strong enough attractive tail in order to allow for two-body bound states, but
are otherwise sufficiently repulsive to guarantee stability of the system, we
show that in the low-density limit the ground state of this model consists of
a Bose–Einstein condensate of fermion pairs. The latter can be described by means
of the Gross–Pitaevskii energy functional.
acknowledgement: Partial financial support from the DFG grant GRK 1838, as well as
the Austrian Science Fund (FWF), project Nr. P 27533-N27 (R.S.), is gratefully acknowledged.
article_number: '13'
article_processing_charge: Yes (via OA deal)
author:
- first_name: Gerhard
full_name: Bräunlich, Gerhard
last_name: Bräunlich
- first_name: Christian
full_name: Hainzl, Christian
last_name: Hainzl
- first_name: Robert
full_name: Seiringer, Robert
id: 4AFD0470-F248-11E8-B48F-1D18A9856A87
last_name: Seiringer
orcid: 0000-0002-6781-0521
citation:
ama: Bräunlich G, Hainzl C, Seiringer R. Bogolubov–Hartree–Fock theory for strongly
interacting fermions in the low density limit. Mathematical Physics, Analysis
and Geometry. 2016;19(2). doi:10.1007/s11040-016-9209-x
apa: Bräunlich, G., Hainzl, C., & Seiringer, R. (2016). Bogolubov–Hartree–Fock
theory for strongly interacting fermions in the low density limit. Mathematical
Physics, Analysis and Geometry. Springer. https://doi.org/10.1007/s11040-016-9209-x
chicago: Bräunlich, Gerhard, Christian Hainzl, and Robert Seiringer. “Bogolubov–Hartree–Fock
Theory for Strongly Interacting Fermions in the Low Density Limit.” Mathematical
Physics, Analysis and Geometry. Springer, 2016. https://doi.org/10.1007/s11040-016-9209-x.
ieee: G. Bräunlich, C. Hainzl, and R. Seiringer, “Bogolubov–Hartree–Fock theory
for strongly interacting fermions in the low density limit,” Mathematical Physics,
Analysis and Geometry, vol. 19, no. 2. Springer, 2016.
ista: Bräunlich G, Hainzl C, Seiringer R. 2016. Bogolubov–Hartree–Fock theory for
strongly interacting fermions in the low density limit. Mathematical Physics,
Analysis and Geometry. 19(2), 13.
mla: Bräunlich, Gerhard, et al. “Bogolubov–Hartree–Fock Theory for Strongly Interacting
Fermions in the Low Density Limit.” Mathematical Physics, Analysis and Geometry,
vol. 19, no. 2, 13, Springer, 2016, doi:10.1007/s11040-016-9209-x.
short: G. Bräunlich, C. Hainzl, R. Seiringer, Mathematical Physics, Analysis and
Geometry 19 (2016).
corr_author: '1'
date_created: 2018-12-11T11:50:59Z
date_published: 2016-06-01T00:00:00Z
date_updated: 2025-09-22T09:02:01Z
day: '01'
ddc:
- '510'
- '539'
department:
- _id: RoSe
doi: 10.1007/s11040-016-9209-x
external_id:
isi:
- '000377379300001'
file:
- access_level: open_access
checksum: 9954f685cc25c58d7f1712c67b47ad8d
content_type: application/pdf
creator: system
date_created: 2018-12-12T10:09:13Z
date_updated: 2020-07-14T12:44:42Z
file_id: '4736'
file_name: IST-2016-702-v1+1_s11040-016-9209-x.pdf
file_size: 506242
relation: main_file
file_date_updated: 2020-07-14T12:44:42Z
fulldoi: https://doi.org/10.1007/s11040-016-9209-x
has_accepted_license: '1'
intvolume: ' 19'
isi: 1
issue: '2'
language:
- iso: eng
month: '06'
oa: 1
oa_version: Published Version
project:
- _id: 25C878CE-B435-11E9-9278-68D0E5697425
call_identifier: FWF
grant_number: P27533_N27
name: Structure of the Excitation Spectrum for Many-Body Quantum Systems
publication: Mathematical Physics, Analysis and Geometry
publication_status: published
publisher: Springer
publist_id: '6066'
pubrep_id: '702'
quality_controlled: '1'
scopus_import: '1'
status: public
title: Bogolubov–Hartree–Fock theory for strongly interacting fermions in the low
density limit
tmp:
image: /images/cc_by.png
legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
short: CC BY (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 19
year: '2016'
...
---
_id: '1260'
abstract:
- lang: eng
text: In this work, the Gardner problem of inferring interactions and fields for
an Ising neural network from given patterns under a local stability hypothesis
is addressed under a dual perspective. By means of duality arguments, an integer
linear system is defined whose solution space is the dual of the Gardner space
and whose solutions represent mutually unstable patterns. We propose and discuss
Monte Carlo methods in order to find and remove unstable patterns and uniformly
sample the space of interactions thereafter. We illustrate the problem on a set
of real data and perform ensemble calculation that shows how the emergence of
phase dominated by unstable patterns can be triggered in a nonlinear discontinuous
way.
article_number: '1650067'
article_processing_charge: No
article_type: original
arxiv: 1
author:
- first_name: Daniele
full_name: De Martino, Daniele
id: 3FF5848A-F248-11E8-B48F-1D18A9856A87
last_name: De Martino
orcid: 0000-0002-5214-4706
citation:
ama: De Martino D. The dual of the space of interactions in neural network models.
International Journal of Modern Physics C. 2016;27(6). doi:10.1142/S0129183116500674
apa: De Martino, D. (2016). The dual of the space of interactions in neural network
models. International Journal of Modern Physics C. World Scientific Publishing.
https://doi.org/10.1142/S0129183116500674
chicago: De Martino, Daniele. “The Dual of the Space of Interactions in Neural Network
Models.” International Journal of Modern Physics C. World Scientific Publishing,
2016. https://doi.org/10.1142/S0129183116500674.
ieee: D. De Martino, “The dual of the space of interactions in neural network models,”
International Journal of Modern Physics C, vol. 27, no. 6. World Scientific
Publishing, 2016.
ista: De Martino D. 2016. The dual of the space of interactions in neural network
models. International Journal of Modern Physics C. 27(6), 1650067.
mla: De Martino, Daniele. “The Dual of the Space of Interactions in Neural Network
Models.” International Journal of Modern Physics C, vol. 27, no. 6, 1650067,
World Scientific Publishing, 2016, doi:10.1142/S0129183116500674.
short: D. De Martino, International Journal of Modern Physics C 27 (2016).
corr_author: '1'
date_created: 2018-12-11T11:51:00Z
date_published: 2016-06-01T00:00:00Z
date_updated: 2025-09-22T09:01:25Z
day: '01'
department:
- _id: GaTk
doi: 10.1142/S0129183116500674
external_id:
arxiv:
- '1505.02963'
isi:
- '000377674800010'
fulldoi: https://doi.org/10.1142/S0129183116500674
intvolume: ' 27'
isi: 1
issue: '6'
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://arxiv.org/abs/1505.02963
month: '06'
oa: 1
oa_version: Preprint
publication: International Journal of Modern Physics C
publication_status: published
publisher: World Scientific Publishing
publist_id: '6065'
quality_controlled: '1'
scopus_import: '1'
status: public
title: The dual of the space of interactions in neural network models
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 27
year: '2016'
...
---
_id: '1261'
abstract:
- lang: eng
text: 'We consider a non-standard finite-volume discretization of a strongly non-linear
fourth order diffusion equation on the d-dimensional cube, for arbitrary . The
scheme preserves two important structural properties of the equation: the first
is the interpretation as a gradient flow in a mass transportation metric, and
the second is an intimate relation to a linear Fokker-Planck equation. Thanks
to these structural properties, the scheme possesses two discrete Lyapunov functionals.
These functionals approximate the entropy and the Fisher information, respectively,
and their dissipation rates converge to the optimal ones in the discrete-to-continuous
limit. Using the dissipation, we derive estimates on the long-time asymptotics
of the discrete solutions. Finally, we present results from numerical experiments
which indicate that our discretization is able to capture significant features
of the complex original dynamics, even with a rather coarse spatial resolution.'
acknowledgement: This research was supported by the DFG Collaborative Research Centers TRR 109, ‘
Discretization in Geometry and Dynamics ’ and 1060 ‘ The Mathematics of Emergent
Effects ’ .
article_processing_charge: No
arxiv: 1
author:
- first_name: Jan
full_name: Maas, Jan
id: 4C5696CE-F248-11E8-B48F-1D18A9856A87
last_name: Maas
orcid: 0000-0002-0845-1338
- first_name: Daniel
full_name: Matthes, Daniel
last_name: Matthes
citation:
ama: Maas J, Matthes D. Long-time behavior of a finite volume discretization for
a fourth order diffusion equation. Nonlinearity. 2016;29(7):1992-2023.
doi:10.1088/0951-7715/29/7/1992
apa: Maas, J., & Matthes, D. (2016). Long-time behavior of a finite volume discretization
for a fourth order diffusion equation. Nonlinearity. IOP Publishing. https://doi.org/10.1088/0951-7715/29/7/1992
chicago: Maas, Jan, and Daniel Matthes. “Long-Time Behavior of a Finite Volume Discretization
for a Fourth Order Diffusion Equation.” Nonlinearity. IOP Publishing, 2016.
https://doi.org/10.1088/0951-7715/29/7/1992.
ieee: J. Maas and D. Matthes, “Long-time behavior of a finite volume discretization
for a fourth order diffusion equation,” Nonlinearity, vol. 29, no. 7. IOP
Publishing, pp. 1992–2023, 2016.
ista: Maas J, Matthes D. 2016. Long-time behavior of a finite volume discretization
for a fourth order diffusion equation. Nonlinearity. 29(7), 1992–2023.
mla: Maas, Jan, and Daniel Matthes. “Long-Time Behavior of a Finite Volume Discretization
for a Fourth Order Diffusion Equation.” Nonlinearity, vol. 29, no. 7, IOP
Publishing, 2016, pp. 1992–2023, doi:10.1088/0951-7715/29/7/1992.
short: J. Maas, D. Matthes, Nonlinearity 29 (2016) 1992–2023.
corr_author: '1'
date_created: 2018-12-11T11:51:00Z
date_published: 2016-06-10T00:00:00Z
date_updated: 2025-09-22T09:00:50Z
day: '10'
department:
- _id: JaMa
doi: 10.1088/0951-7715/29/7/1992
external_id:
arxiv:
- '1505.03178'
isi:
- '000378862800006'
fulldoi: https://doi.org/10.1088/0951-7715/29/7/1992
intvolume: ' 29'
isi: 1
issue: '7'
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://arxiv.org/abs/1505.03178
month: '06'
oa: 1
oa_version: Preprint
page: 1992 - 2023
publication: Nonlinearity
publication_status: published
publisher: IOP Publishing
publist_id: '6062'
quality_controlled: '1'
scopus_import: '1'
status: public
title: Long-time behavior of a finite volume discretization for a fourth order diffusion
equation
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 29
year: '2016'
...
---
_id: '12613'
abstract:
- lang: eng
text: 'We use high-resolution digital elevation models (DEMs) from unmanned aerial
vehicle (UAV) surveys to document the evolution of four ice cliffs on the debris-covered
tongue of Lirung Glacier, Nepal, over one ablation season. Observations show that
out of four cliffs, three different patterns of evolution emerge: (i) reclining
cliffs that flatten during the ablation season; (ii) stable cliffs that maintain
a self-similar geometry; and (iii) growing cliffs, expanding laterally. We use
the insights from this unique data set to develop a 3-D model of cliff backwasting
and evolution that is validated against observations and an independent data set
of volume losses. The model includes ablation at the cliff surface driven by energy
exchange with the atmosphere, reburial of cliff cells by surrounding debris, and
the effect of adjacent ponds. The cliff geometry is updated monthly to account
for the modifications induced by each of those processes. Model results indicate
that a major factor affecting the survival of steep cliffs is the coupling with
ponded water at its base, which prevents progressive flattening and possible disappearance
of a cliff. The radial growth observed at one cliff is explained by higher receipts
of longwave and shortwave radiation, calculated taking into account atmospheric
fluxes, shading, and the emission of longwave radiation from debris surfaces.
The model is a clear step forward compared to existing static approaches that
calculate atmospheric melt over an invariant cliff geometry and can be used for
long-term simulations of cliff evolution and to test existing hypotheses about
cliffs'' survival.'
article_processing_charge: No
article_type: original
author:
- first_name: Pascal
full_name: Buri, Pascal
last_name: Buri
- first_name: Evan S.
full_name: Miles, Evan S.
last_name: Miles
- first_name: Jakob F.
full_name: Steiner, Jakob F.
last_name: Steiner
- first_name: Walter W.
full_name: Immerzeel, Walter W.
last_name: Immerzeel
- first_name: Patrick
full_name: Wagnon, Patrick
last_name: Wagnon
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: 'Buri P, Miles ES, Steiner JF, Immerzeel WW, Wagnon P, Pellicciotti F. A physically
based 3‐D model of ice cliff evolution over debris‐covered glaciers. Journal
of Geophysical Research: Earth Surface. 2016;121(12):2471-2493. doi:10.1002/2016jf004039'
apa: 'Buri, P., Miles, E. S., Steiner, J. F., Immerzeel, W. W., Wagnon, P., &
Pellicciotti, F. (2016). A physically based 3‐D model of ice cliff evolution over
debris‐covered glaciers. Journal of Geophysical Research: Earth Surface.
American Geophysical Union. https://doi.org/10.1002/2016jf004039'
chicago: 'Buri, Pascal, Evan S. Miles, Jakob F. Steiner, Walter W. Immerzeel, Patrick
Wagnon, and Francesca Pellicciotti. “A Physically Based 3‐D Model of Ice Cliff
Evolution over Debris‐covered Glaciers.” Journal of Geophysical Research: Earth
Surface. American Geophysical Union, 2016. https://doi.org/10.1002/2016jf004039.'
ieee: 'P. Buri, E. S. Miles, J. F. Steiner, W. W. Immerzeel, P. Wagnon, and F. Pellicciotti,
“A physically based 3‐D model of ice cliff evolution over debris‐covered glaciers,”
Journal of Geophysical Research: Earth Surface, vol. 121, no. 12. American
Geophysical Union, pp. 2471–2493, 2016.'
ista: 'Buri P, Miles ES, Steiner JF, Immerzeel WW, Wagnon P, Pellicciotti F. 2016.
A physically based 3‐D model of ice cliff evolution over debris‐covered glaciers.
Journal of Geophysical Research: Earth Surface. 121(12), 2471–2493.'
mla: 'Buri, Pascal, et al. “A Physically Based 3‐D Model of Ice Cliff Evolution
over Debris‐covered Glaciers.” Journal of Geophysical Research: Earth Surface,
vol. 121, no. 12, American Geophysical Union, 2016, pp. 2471–93, doi:10.1002/2016jf004039.'
short: 'P. Buri, E.S. Miles, J.F. Steiner, W.W. Immerzeel, P. Wagnon, F. Pellicciotti,
Journal of Geophysical Research: Earth Surface 121 (2016) 2471–2493.'
date_created: 2023-02-20T08:14:28Z
date_published: 2016-11-22T00:00:00Z
date_updated: 2023-02-24T11:34:54Z
day: '22'
doi: 10.1002/2016jf004039
extern: '1'
fulldoi: https://doi.org/10.1002/2016jf004039
intvolume: ' 121'
issue: '12'
keyword:
- Earth-Surface Processes
- Geophysics
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1002/2016JF004039
month: '11'
oa: 1
oa_version: Published Version
page: 2471-2493
publication: 'Journal of Geophysical Research: Earth Surface'
publication_identifier:
eissn:
- 2169-9011
issn:
- 2169-9003
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
scopus_import: '1'
status: public
title: A physically based 3‐D model of ice cliff evolution over debris‐covered glaciers
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 121
year: '2016'
...
---
_id: '12614'
abstract:
- lang: eng
text: Debris-covered glaciers in the Himalaya may have spatially-averaged rates
of surface height change that are similar to those observed on bare-ice glaciers,
despite the insulating effects of thick debris. Spatially heterogeneous melt patterns
caused by the development and evolution of ice cliffs and supraglacial pond systems
result in substantial mass losses over time. However, mechanisms controlling the
formation and survival of cliffs and ponds remain largely unknown. To study the
distribution and characteristics of these surface features we deploy an unmanned
aerial vehicle (UAV) over a stretch of the debris-covered Langtang Glacier, Nepal.
Acquired images are processed into high-resolution orthomosaics and elevation
models with the Structure from Motion (SfM) photogrammetry algorithm. Ice cliffs
and ponds are classified using object-based image analysis (OBIA) and their morphology
and spatial distribution are analysed and evaluated using object, pixel and point
cloud approaches. Results show that ice cliffs are predominantly north-facing,
and larger ice cliffs are generally coupled with supraglacial ponds, which may
affect their evolution considerably. The spatial distribution of ice cliffs indicates
that they are more likely to form in areas where high strain rates are expected.
The spatial configuration of ponds over the entire tongue reveals high pond density
near confluences, possibly due to closure of conduits via transverse compression.
We conclude that the combination of OBIA and UAV imagery is a valuable tool in
the semi-automatic and objective analysis of surface features on debris-covered
glaciers. The technique may also have potential for upscaling to the use of spaceborne
imagery, and the use of UAV-derived point clouds to analyse ice cliff undercuts
is promising.
article_processing_charge: No
article_type: original
author:
- first_name: P.D.A.
full_name: Kraaijenbrink, P.D.A.
last_name: Kraaijenbrink
- first_name: J.M.
full_name: Shea, J.M.
last_name: Shea
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: S.M. de
full_name: Jong, S.M. de
last_name: Jong
- first_name: W.W.
full_name: Immerzeel, W.W.
last_name: Immerzeel
citation:
ama: Kraaijenbrink PDA, Shea JM, Pellicciotti F, Jong SM de, Immerzeel WW. Object-based
analysis of unmanned aerial vehicle imagery to map and characterise surface features
on a debris-covered glacier. Remote Sensing of Environment. 2016;186:581-595.
doi:10.1016/j.rse.2016.09.013
apa: Kraaijenbrink, P. D. A., Shea, J. M., Pellicciotti, F., Jong, S. M. de, &
Immerzeel, W. W. (2016). Object-based analysis of unmanned aerial vehicle imagery
to map and characterise surface features on a debris-covered glacier. Remote
Sensing of Environment. Elsevier. https://doi.org/10.1016/j.rse.2016.09.013
chicago: Kraaijenbrink, P.D.A., J.M. Shea, Francesca Pellicciotti, S.M. de Jong,
and W.W. Immerzeel. “Object-Based Analysis of Unmanned Aerial Vehicle Imagery
to Map and Characterise Surface Features on a Debris-Covered Glacier.” Remote
Sensing of Environment. Elsevier, 2016. https://doi.org/10.1016/j.rse.2016.09.013.
ieee: P. D. A. Kraaijenbrink, J. M. Shea, F. Pellicciotti, S. M. de Jong, and W.
W. Immerzeel, “Object-based analysis of unmanned aerial vehicle imagery to map
and characterise surface features on a debris-covered glacier,” Remote Sensing
of Environment, vol. 186. Elsevier, pp. 581–595, 2016.
ista: Kraaijenbrink PDA, Shea JM, Pellicciotti F, Jong SM de, Immerzeel WW. 2016.
Object-based analysis of unmanned aerial vehicle imagery to map and characterise
surface features on a debris-covered glacier. Remote Sensing of Environment. 186,
581–595.
mla: Kraaijenbrink, P. D. A., et al. “Object-Based Analysis of Unmanned Aerial Vehicle
Imagery to Map and Characterise Surface Features on a Debris-Covered Glacier.”
Remote Sensing of Environment, vol. 186, Elsevier, 2016, pp. 581–95, doi:10.1016/j.rse.2016.09.013.
short: P.D.A. Kraaijenbrink, J.M. Shea, F. Pellicciotti, S.M. de Jong, W.W. Immerzeel,
Remote Sensing of Environment 186 (2016) 581–595.
date_created: 2023-02-20T08:14:35Z
date_published: 2016-12-01T00:00:00Z
date_updated: 2023-02-24T11:31:58Z
day: '01'
doi: 10.1016/j.rse.2016.09.013
extern: '1'
fulldoi: https://doi.org/10.1016/j.rse.2016.09.013
intvolume: ' 186'
keyword:
- Computers in Earth Sciences
- Geology
- Soil Science
language:
- iso: eng
month: '12'
oa_version: None
page: 581-595
publication: Remote Sensing of Environment
publication_identifier:
issn:
- 0034-4257
publication_status: published
publisher: Elsevier
quality_controlled: '1'
scopus_import: '1'
status: public
title: Object-based analysis of unmanned aerial vehicle imagery to map and characterise
surface features on a debris-covered glacier
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 186
year: '2016'
...
---
_id: '12615'
abstract:
- lang: eng
text: 'We apply the process-based, distributed TOPKAPI-ETH glacio-hydrological model
to a glacierized catchment (19% glacierized) in the semiarid Andes of central
Chile. The semiarid Andes provides vital freshwater resources to valleys in Chile
and Argentina, but only few glacio-hydrological modelling studies have been conducted,
and its dominant hydrological processes remain poorly understood. The catchment
contains two debris-free glaciers reaching down to 3900 m asl (Bello and Yeso
glaciers) and one debris-covered avalanche-fed glacier reaching to 3200 m asl
(Piramide Glacier). Our main objective is to compare the mass balance and runoff
contributions of both glacier types under current climatic conditions. We use
a unique dataset of field measurements collected over two ablation seasons combined
with the distributed TOPKAPI-ETH model that includes physically oriented parameterizations
of snow and ice ablation, gravitational distribution of snow, snow albedo evolution
and the ablation of debris-covered ice. Model outputs indicate that while the
mass balance of Bello and Yeso glaciers is mostly explained by temperature gradients,
the Piramide Glacier mass balance is governed by debris thickness and avalanches
and has a clear non-linear profile with elevation as a result. Despite the thermal
insulation effect of the debris cover, the mass balance and contribution to runoff
from debris-free and debris-covered glaciers are similar in magnitude, mainly
because of elevation differences. However, runoff contributions are distinct in
time and seasonality with ice melt starting approximately four weeks earlier from
the debris-covered glacier, what is of relevance for water resources management.
At the catchment scale, snowmelt is the dominant contributor to runoff during
both years. However, during the driest year of our simulations, ice melt contributes
42 ± 8% and 67 ± 6% of the annual and summer runoff, respectively. Sensitivity
analyses show that runoff is most sensitive to temperature and precipitation gradients,
melt factors and debris cover thickness. '
article_processing_charge: No
article_type: original
author:
- first_name: A.
full_name: Ayala, A.
last_name: Ayala
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: S.
full_name: MacDonell, S.
last_name: MacDonell
- first_name: J.
full_name: McPhee, J.
last_name: McPhee
- first_name: S.
full_name: Vivero, S.
last_name: Vivero
- first_name: C.
full_name: Campos, C.
last_name: Campos
- first_name: P.
full_name: Egli, P.
last_name: Egli
citation:
ama: Ayala A, Pellicciotti F, MacDonell S, et al. Modelling the hydrological response
of debris-free and debris-covered glaciers to present climatic conditions in the
semiarid Andes of central Chile. Hydrological Processes. 2016;30(22):4036-4058.
doi:10.1002/hyp.10971
apa: Ayala, A., Pellicciotti, F., MacDonell, S., McPhee, J., Vivero, S., Campos,
C., & Egli, P. (2016). Modelling the hydrological response of debris-free
and debris-covered glaciers to present climatic conditions in the semiarid Andes
of central Chile. Hydrological Processes. Wiley. https://doi.org/10.1002/hyp.10971
chicago: Ayala, A., Francesca Pellicciotti, S. MacDonell, J. McPhee, S. Vivero,
C. Campos, and P. Egli. “Modelling the Hydrological Response of Debris-Free and
Debris-Covered Glaciers to Present Climatic Conditions in the Semiarid Andes of
Central Chile.” Hydrological Processes. Wiley, 2016. https://doi.org/10.1002/hyp.10971.
ieee: A. Ayala et al., “Modelling the hydrological response of debris-free
and debris-covered glaciers to present climatic conditions in the semiarid Andes
of central Chile,” Hydrological Processes, vol. 30, no. 22. Wiley, pp.
4036–4058, 2016.
ista: Ayala A, Pellicciotti F, MacDonell S, McPhee J, Vivero S, Campos C, Egli P.
2016. Modelling the hydrological response of debris-free and debris-covered glaciers
to present climatic conditions in the semiarid Andes of central Chile. Hydrological
Processes. 30(22), 4036–4058.
mla: Ayala, A., et al. “Modelling the Hydrological Response of Debris-Free and Debris-Covered
Glaciers to Present Climatic Conditions in the Semiarid Andes of Central Chile.”
Hydrological Processes, vol. 30, no. 22, Wiley, 2016, pp. 4036–58, doi:10.1002/hyp.10971.
short: A. Ayala, F. Pellicciotti, S. MacDonell, J. McPhee, S. Vivero, C. Campos,
P. Egli, Hydrological Processes 30 (2016) 4036–4058.
date_created: 2023-02-20T08:14:40Z
date_published: 2016-07-28T00:00:00Z
date_updated: 2023-02-24T11:29:28Z
day: '28'
doi: 10.1002/hyp.10971
extern: '1'
fulldoi: https://doi.org/10.1002/hyp.10971
intvolume: ' 30'
issue: '22'
keyword:
- Water Science and Technology
language:
- iso: eng
month: '07'
oa_version: None
page: 4036-4058
publication: Hydrological Processes
publication_identifier:
issn:
- 0885-6087
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: Modelling the hydrological response of debris-free and debris-covered glaciers
to present climatic conditions in the semiarid Andes of central Chile
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 30
year: '2016'
...
---
_id: '12616'
abstract:
- lang: eng
text: This paper presents a methodology for hydrograph separation in mountain watersheds,
which aims at identifying flow sources among ungauged headwater sub-catchments
through a combination of observed streamflow and data on natural tracers including
isotope and dissolved solids. Daily summer and bi-daily spring season water samples
obtained at the outlet of the Juncal River Basin in the Andes of Central Chile
were analysed for all major ions as well as stable water isotopes, δ18O and δD.
Additionally, various samples from rain, snow, surface streams and exfiltrating
subsurface water (springs) were sampled throughout the catchment. A principal
component analysis was performed in order to address cross-correlation in the
tracer dataset, reduce the dimensionality of the problem and uncover patterns
of variability. Potential sources were identified in a two-component U-space that
explains 94% of the observed tracer variability at the catchment outlet. Hydrograph
separation was performed through an Informative-Bayesian model. Our results indicate
that the Juncal Norte Glacier headwater sub-catchment contributed at least 50%
of summer flows at the Juncal River Basin outlet during the 2011–2012 water year
(a hydrologically dry period in the Region), even though it accounts for only
27% of the basin area. Our study confirms the value of combining solute and isotope
information for estimating source contributions in complex hydrologic systems,
and provides insights regarding experimental design in high-elevation semi-arid
catchments. The findings of this study can be useful for evaluating modelling
studies of the hydrological consequences of the rapid decrease in glacier cover
observed in this region, by providing insights into the origin of river water
in basins with little hydrometeorological information.
article_processing_charge: No
article_type: original
author:
- first_name: Maximiliano
full_name: Rodriguez, Maximiliano
last_name: Rodriguez
- first_name: Nils
full_name: Ohlanders, Nils
last_name: Ohlanders
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: Mark W.
full_name: Williams, Mark W.
last_name: Williams
- first_name: James
full_name: McPhee, James
last_name: McPhee
citation:
ama: Rodriguez M, Ohlanders N, Pellicciotti F, Williams MW, McPhee J. Estimating
runoff from a glacierized catchment using natural tracers in the semi-arid Andes
cordillera. Hydrological Processes. 2016;30(20):3609-3626. doi:10.1002/hyp.10973
apa: Rodriguez, M., Ohlanders, N., Pellicciotti, F., Williams, M. W., & McPhee,
J. (2016). Estimating runoff from a glacierized catchment using natural tracers
in the semi-arid Andes cordillera. Hydrological Processes. Wiley. https://doi.org/10.1002/hyp.10973
chicago: Rodriguez, Maximiliano, Nils Ohlanders, Francesca Pellicciotti, Mark W.
Williams, and James McPhee. “Estimating Runoff from a Glacierized Catchment Using
Natural Tracers in the Semi-Arid Andes Cordillera.” Hydrological Processes.
Wiley, 2016. https://doi.org/10.1002/hyp.10973.
ieee: M. Rodriguez, N. Ohlanders, F. Pellicciotti, M. W. Williams, and J. McPhee,
“Estimating runoff from a glacierized catchment using natural tracers in the semi-arid
Andes cordillera,” Hydrological Processes, vol. 30, no. 20. Wiley, pp.
3609–3626, 2016.
ista: Rodriguez M, Ohlanders N, Pellicciotti F, Williams MW, McPhee J. 2016. Estimating
runoff from a glacierized catchment using natural tracers in the semi-arid Andes
cordillera. Hydrological Processes. 30(20), 3609–3626.
mla: Rodriguez, Maximiliano, et al. “Estimating Runoff from a Glacierized Catchment
Using Natural Tracers in the Semi-Arid Andes Cordillera.” Hydrological Processes,
vol. 30, no. 20, Wiley, 2016, pp. 3609–26, doi:10.1002/hyp.10973.
short: M. Rodriguez, N. Ohlanders, F. Pellicciotti, M.W. Williams, J. McPhee, Hydrological
Processes 30 (2016) 3609–3626.
date_created: 2023-02-20T08:14:45Z
date_published: 2016-07-22T00:00:00Z
date_updated: 2023-02-24T11:26:54Z
day: '22'
doi: 10.1002/hyp.10973
extern: '1'
fulldoi: https://doi.org/10.1002/hyp.10973
intvolume: ' 30'
issue: '20'
keyword:
- Water Science and Technology
language:
- iso: eng
month: '07'
oa_version: None
page: 3609-3626
publication: Hydrological Processes
publication_identifier:
issn:
- 0885-6087
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: Estimating runoff from a glacierized catchment using natural tracers in the
semi-arid Andes cordillera
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 30
year: '2016'
...
---
_id: '12617'
abstract:
- lang: eng
text: This study presents volume and mass changes of seven (five partially debris-covered,
two debris-free) glaciers in the upper Langtang catchment in Nepal. We use a digital
elevation model (DEM) from 1974 stereo Hexagon satellite data and seven DEMs derived
from 2006–2015 stereo or tri-stereo satellite imagery (e.g., SPOT6/7). The availability
of multiple independent DEM differences allows the identification of a robust
signal and narrowing down of the uncertainty about recent volume changes. The
volume changes calculated over several multiyear periods between 2006 and 2015
consistently indicate that glacier thinning has accelerated with respect to the
period 1974–2006. We calculate an ensemble-mean elevation change rate of –0.45 ± 0.18 m a−1
for 2006–2015, while for the period 1974–2006 we compute a rate of −0.24 ± 0.08 m a−1.
However, the behavior of glaciers in the study area is heterogeneous, and the
presence or absence of debris does not seem to be a good predictor for mass balance
trends. Debris-covered tongues have nonlinear thinning profiles, and we show that
recent accelerations in thinning correlate with the presence of supraglacial cliffs
and lakes. At stagnating glacier areas near the glacier front, however, thinning
rates decreased with time or remained constant. The April 2015 Nepal earthquake
triggered large avalanches in the study catchment. Analysis of two post-earthquake
DEMs revealed that the avalanche deposit volumes remaining 6 months after the
earthquake are negligible in comparison to 2006–2015 elevation changes. However,
the deposits compensate about 40 % the mass loss of debris-covered tongues of
1 average year.
article_processing_charge: No
article_type: original
author:
- first_name: Silvan
full_name: Ragettli, Silvan
last_name: Ragettli
- first_name: Tobias
full_name: Bolch, Tobias
last_name: Bolch
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: Ragettli S, Bolch T, Pellicciotti F. Heterogeneous glacier thinning patterns
over the last 40 years in Langtang Himal, Nepal. The Cryosphere. 2016;10(5):2075-2097.
doi:10.5194/tc-10-2075-2016
apa: Ragettli, S., Bolch, T., & Pellicciotti, F. (2016). Heterogeneous glacier
thinning patterns over the last 40 years in Langtang Himal, Nepal. The Cryosphere.
Copernicus Publications. https://doi.org/10.5194/tc-10-2075-2016
chicago: Ragettli, Silvan, Tobias Bolch, and Francesca Pellicciotti. “Heterogeneous
Glacier Thinning Patterns over the Last 40 Years in Langtang Himal, Nepal.” The
Cryosphere. Copernicus Publications, 2016. https://doi.org/10.5194/tc-10-2075-2016.
ieee: S. Ragettli, T. Bolch, and F. Pellicciotti, “Heterogeneous glacier thinning
patterns over the last 40 years in Langtang Himal, Nepal,” The Cryosphere,
vol. 10, no. 5. Copernicus Publications, pp. 2075–2097, 2016.
ista: Ragettli S, Bolch T, Pellicciotti F. 2016. Heterogeneous glacier thinning
patterns over the last 40 years in Langtang Himal, Nepal. The Cryosphere. 10(5),
2075–2097.
mla: Ragettli, Silvan, et al. “Heterogeneous Glacier Thinning Patterns over the
Last 40 Years in Langtang Himal, Nepal.” The Cryosphere, vol. 10, no. 5,
Copernicus Publications, 2016, pp. 2075–97, doi:10.5194/tc-10-2075-2016.
short: S. Ragettli, T. Bolch, F. Pellicciotti, The Cryosphere 10 (2016) 2075–2097.
date_created: 2023-02-20T08:14:51Z
date_published: 2016-09-14T00:00:00Z
date_updated: 2023-02-24T10:54:02Z
day: '14'
doi: 10.5194/tc-10-2075-2016
extern: '1'
fulldoi: https://doi.org/10.5194/tc-10-2075-2016
intvolume: ' 10'
issue: '5'
keyword:
- Earth-Surface Processes
- Water Science and Technology
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.5194/tc-10-2075-2016
month: '09'
oa: 1
oa_version: Published Version
page: 2075-2097
publication: The Cryosphere
publication_identifier:
issn:
- 1994-0424
publication_status: published
publisher: Copernicus Publications
quality_controlled: '1'
scopus_import: '1'
status: public
title: Heterogeneous glacier thinning patterns over the last 40 years in Langtang
Himal, Nepal
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 10
year: '2016'
...
---
_id: '12618'
abstract:
- lang: eng
text: Mountain ranges are the world’s natural water towers and provide water resources
for millions of people. However, their hydrological balance and possible future
changes in river flow remain poorly understood because of high meteorological
variability, physical inaccessibility, and the complex interplay between climate,
cryosphere, and hydrological processes. Here, we use a state-of-the art glacio-hydrological
model informed by data from high-altitude observations and the latest climate
change scenarios to quantify the climate change impact on water resources of two
contrasting catchments vulnerable to changes in the cryosphere. The two study
catchments are located in the Central Andes of Chile and in the Nepalese Himalaya
in close vicinity of densely populated areas. Although both sites reveal a strong
decrease in glacier area, they show a remarkably different hydrological response
to projected climate change. In the Juncal catchment in Chile, runoff is likely
to sharply decrease in the future and the runoff seasonality is sensitive to projected
climatic changes. In the Langtang catchment in Nepal, future water availability
is on the rise for decades to come with limited shifts between seasons. Owing
to the high spatiotemporal resolution of the simulations and process complexity
included in the modeling, the response times and the mechanisms underlying the
variations in glacier area and river flow can be well constrained. The projections
indicate that climate change adaptation in Central Chile should focus on dealing
with a reduction in water availability, whereas in Nepal preparedness for flood
extremes should be the policy priority.
article_processing_charge: No
article_type: original
author:
- first_name: Silvan
full_name: Ragettli, Silvan
last_name: Ragettli
- first_name: Walter W.
full_name: Immerzeel, Walter W.
last_name: Immerzeel
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: Ragettli S, Immerzeel WW, Pellicciotti F. Contrasting climate change impact
on river flows from high-altitude catchments in the Himalayan and Andes Mountains.
PNAS. 2016;113(33):9222-9227. doi:10.1073/pnas.1606526113
apa: Ragettli, S., Immerzeel, W. W., & Pellicciotti, F. (2016). Contrasting
climate change impact on river flows from high-altitude catchments in the Himalayan
and Andes Mountains. PNAS. Proceedings of the National Academy of Sciences.
https://doi.org/10.1073/pnas.1606526113
chicago: Ragettli, Silvan, Walter W. Immerzeel, and Francesca Pellicciotti. “Contrasting
Climate Change Impact on River Flows from High-Altitude Catchments in the Himalayan
and Andes Mountains.” PNAS. Proceedings of the National Academy of Sciences,
2016. https://doi.org/10.1073/pnas.1606526113.
ieee: S. Ragettli, W. W. Immerzeel, and F. Pellicciotti, “Contrasting climate change
impact on river flows from high-altitude catchments in the Himalayan and Andes
Mountains,” PNAS, vol. 113, no. 33. Proceedings of the National Academy
of Sciences, pp. 9222–9227, 2016.
ista: Ragettli S, Immerzeel WW, Pellicciotti F. 2016. Contrasting climate change
impact on river flows from high-altitude catchments in the Himalayan and Andes
Mountains. PNAS. 113(33), 9222–9227.
mla: Ragettli, Silvan, et al. “Contrasting Climate Change Impact on River Flows
from High-Altitude Catchments in the Himalayan and Andes Mountains.” PNAS,
vol. 113, no. 33, Proceedings of the National Academy of Sciences, 2016, pp. 9222–27,
doi:10.1073/pnas.1606526113.
short: S. Ragettli, W.W. Immerzeel, F. Pellicciotti, PNAS 113 (2016) 9222–9227.
date_created: 2023-02-20T08:14:58Z
date_published: 2016-08-01T00:00:00Z
date_updated: 2023-02-24T10:48:43Z
day: '01'
doi: 10.1073/pnas.1606526113
extern: '1'
external_id:
pmid:
- '27482082'
fulldoi: https://doi.org/10.1073/pnas.1606526113
intvolume: ' 113'
issue: '33'
keyword:
- Multidisciplinary
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1073/pnas.1606526113
month: '08'
oa: 1
oa_version: Published Version
page: 9222-9227
pmid: 1
publication: PNAS
publication_identifier:
eissn:
- 1091-6490
issn:
- 0027-8424
publication_status: published
publisher: Proceedings of the National Academy of Sciences
quality_controlled: '1'
scopus_import: '1'
status: public
title: Contrasting climate change impact on river flows from high-altitude catchments
in the Himalayan and Andes Mountains
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 113
year: '2016'
...
---
_id: '12619'
abstract:
- lang: eng
text: Mass losses originating from supraglacial ice cliffs at the lower tongues
of debris-covered glaciers are a potentially large component of the mass balance,
but have rarely been quantified. In this study, we develop a method to estimate
ice cliff volume losses based on high-resolution topographic data derived from
terrestrial and aerial photogrammetry. We apply our method to six cliffs monitored
in May and October 2013 and 2014 using four different topographic datasets collected
over the debris-covered Lirung Glacier of the Nepalese Himalayas. During the monsoon,
the cliff mean backwasting rate was relatively consistent in 2013 (3.8 ± 0.3 cm
w.e. d−1) and more heterogeneous among cliffs in 2014 (3.1
± 0.7 cm w.e. d−1), and the geometric variations between
cliffs are larger. Their mean backwasting rate is significantly lower in winter
(October 2013–May 2014), at 1.0 ± 0.3 cm w.e. d−1. These
results are consistent with estimates of cliff ablation from an energy-balance
model developed in a previous study. The ice cliffs lose mass at rates six times
higher than estimates of glacier-wide melt under debris, which seems to confirm
that ice cliffs provide a large contribution to total glacier melt.
article_processing_charge: No
article_type: original
author:
- first_name: FANNY
full_name: BRUN, FANNY
last_name: BRUN
- first_name: PASCAL
full_name: BURI, PASCAL
last_name: BURI
- first_name: EVAN S.
full_name: MILES, EVAN S.
last_name: MILES
- first_name: PATRICK
full_name: WAGNON, PATRICK
last_name: WAGNON
- first_name: JAKOB
full_name: STEINER, JAKOB
last_name: STEINER
- first_name: ETIENNE
full_name: BERTHIER, ETIENNE
last_name: BERTHIER
- first_name: SILVAN
full_name: RAGETTLI, SILVAN
last_name: RAGETTLI
- first_name: PHILIP
full_name: KRAAIJENBRINK, PHILIP
last_name: KRAAIJENBRINK
- first_name: WALTER W.
full_name: IMMERZEEL, WALTER W.
last_name: IMMERZEEL
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: BRUN F, BURI P, MILES ES, et al. Quantifying volume loss from ice cliffs on
debris-covered glaciers using high-resolution terrestrial and aerial photogrammetry.
Journal of Glaciology. 2016;62(234):684-695. doi:10.1017/jog.2016.54
apa: BRUN, F., BURI, P., MILES, E. S., WAGNON, P., STEINER, J., BERTHIER, E., …
Pellicciotti, F. (2016). Quantifying volume loss from ice cliffs on debris-covered
glaciers using high-resolution terrestrial and aerial photogrammetry. Journal
of Glaciology. Cambridge University Press. https://doi.org/10.1017/jog.2016.54
chicago: BRUN, FANNY, PASCAL BURI, EVAN S. MILES, PATRICK WAGNON, JAKOB STEINER,
ETIENNE BERTHIER, SILVAN RAGETTLI, PHILIP KRAAIJENBRINK, WALTER W. IMMERZEEL,
and Francesca Pellicciotti. “Quantifying Volume Loss from Ice Cliffs on Debris-Covered
Glaciers Using High-Resolution Terrestrial and Aerial Photogrammetry.” Journal
of Glaciology. Cambridge University Press, 2016. https://doi.org/10.1017/jog.2016.54.
ieee: F. BRUN et al., “Quantifying volume loss from ice cliffs on debris-covered
glaciers using high-resolution terrestrial and aerial photogrammetry,” Journal
of Glaciology, vol. 62, no. 234. Cambridge University Press, pp. 684–695,
2016.
ista: BRUN F, BURI P, MILES ES, WAGNON P, STEINER J, BERTHIER E, RAGETTLI S, KRAAIJENBRINK
P, IMMERZEEL WW, Pellicciotti F. 2016. Quantifying volume loss from ice cliffs
on debris-covered glaciers using high-resolution terrestrial and aerial photogrammetry.
Journal of Glaciology. 62(234), 684–695.
mla: BRUN, FANNY, et al. “Quantifying Volume Loss from Ice Cliffs on Debris-Covered
Glaciers Using High-Resolution Terrestrial and Aerial Photogrammetry.” Journal
of Glaciology, vol. 62, no. 234, Cambridge University Press, 2016, pp. 684–95,
doi:10.1017/jog.2016.54.
short: F. BRUN, P. BURI, E.S. MILES, P. WAGNON, J. STEINER, E. BERTHIER, S. RAGETTLI,
P. KRAAIJENBRINK, W.W. IMMERZEEL, F. Pellicciotti, Journal of Glaciology 62 (2016)
684–695.
date_created: 2023-02-20T08:15:06Z
date_published: 2016-08-01T00:00:00Z
date_updated: 2023-02-24T10:36:55Z
day: '01'
doi: 10.1017/jog.2016.54
extern: '1'
fulldoi: https://doi.org/10.1017/jog.2016.54
intvolume: ' 62'
issue: '234'
keyword:
- Earth-Surface Processes
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1017/jog.2016.54
month: '08'
oa: 1
oa_version: Published Version
page: 684-695
publication: Journal of Glaciology
publication_identifier:
eissn:
- 1727-5652
issn:
- 0022-1430
publication_status: published
publisher: Cambridge University Press
quality_controlled: '1'
scopus_import: '1'
status: public
title: Quantifying volume loss from ice cliffs on debris-covered glaciers using high-resolution
terrestrial and aerial photogrammetry
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 62
year: '2016'
...
---
_id: '12620'
abstract:
- lang: eng
text: "Debris-covered glaciers are increasingly studied because it is assumed that
debris cover extent and thickness could increase in a warming climate, with more
regular rockfalls from the surrounding slopes and more englacial melt-out material.
Debris energy-balance models have been developed to account for the melt rate
enhancement/reduction due to a thin/thick debris layer, respectively. However,
such models require a large amount of input data that are not often available,
especially in remote mountain areas such as the Himalaya, and can be difficult
to extrapolate. Due to their lower data requirements, empirical models have been
used extensively in clean glacier melt modelling. For debris-covered glaciers,
however, they generally simplify the debris effect by using a single melt-reduction
factor which does not account for the influence of varying debris thickness on
melt and prescribe a constant reduction for the entire melt across a glacier.\r\n\r\nIn
this paper, we present a new temperature-index model that accounts for debris
thickness in the computation of melt rates at the debris-ice interface. The model
empirical parameters are optimized at the point scale for varying debris thicknesses
against melt rates simulated by a physically-based debris energy balance model.
The latter is validated against ablation stake readings and surface temperature
measurements. Each parameter is then related to a plausible set of debris thickness
values to provide a general and transferable parameterization. We develop the
model on Miage Glacier, Italy, and then test its transferability on Haut Glacier
d’Arolla, Switzerland.\r\n\r\nThe performance of the new debris temperature-index
(DETI) model in simulating the glacier melt rate at the point scale is comparable
to the one of the physically based approach, and the definition of model parameters
as a function of debris thickness allows the simulation of the nonlinear relationship
of melt rate to debris thickness, summarised by the Østrem curve. Its large number
of parameters might be a limitation, but we show that the model is transferable
in time and space to a second glacier with little loss of performance. We thus
suggest that the new DETI model can be included in continuous mass balance models
of debris-covered glaciers, because of its limited data requirements. As such,
we expect its application to lead to an improvement in simulations of the debris-covered
glacier response to climate in comparison with models that simply recalibrate
empirical parameters to prescribe a constant across glacier reduction in melt."
article_processing_charge: No
article_type: original
author:
- first_name: M.
full_name: Carenzo, M.
last_name: Carenzo
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
orcid: 0000-0002-5554-8087
- first_name: J.
full_name: Mabillard, J.
last_name: Mabillard
- first_name: T.
full_name: Reid, T.
last_name: Reid
- first_name: B.W.
full_name: Brock, B.W.
last_name: Brock
citation:
ama: Carenzo M, Pellicciotti F, Mabillard J, Reid T, Brock BW. An enhanced temperature
index model for debris-covered glaciers accounting for thickness effect. Advances
in Water Resources. 2016;94:457-469. doi:10.1016/j.advwatres.2016.05.001
apa: Carenzo, M., Pellicciotti, F., Mabillard, J., Reid, T., & Brock, B. W.
(2016). An enhanced temperature index model for debris-covered glaciers accounting
for thickness effect. Advances in Water Resources. Elsevier. https://doi.org/10.1016/j.advwatres.2016.05.001
chicago: Carenzo, M., Francesca Pellicciotti, J. Mabillard, T. Reid, and B.W. Brock.
“An Enhanced Temperature Index Model for Debris-Covered Glaciers Accounting for
Thickness Effect.” Advances in Water Resources. Elsevier, 2016. https://doi.org/10.1016/j.advwatres.2016.05.001.
ieee: M. Carenzo, F. Pellicciotti, J. Mabillard, T. Reid, and B. W. Brock, “An enhanced
temperature index model for debris-covered glaciers accounting for thickness effect,”
Advances in Water Resources, vol. 94. Elsevier, pp. 457–469, 2016.
ista: Carenzo M, Pellicciotti F, Mabillard J, Reid T, Brock BW. 2016. An enhanced
temperature index model for debris-covered glaciers accounting for thickness effect.
Advances in Water Resources. 94, 457–469.
mla: Carenzo, M., et al. “An Enhanced Temperature Index Model for Debris-Covered
Glaciers Accounting for Thickness Effect.” Advances in Water Resources,
vol. 94, Elsevier, 2016, pp. 457–69, doi:10.1016/j.advwatres.2016.05.001.
short: M. Carenzo, F. Pellicciotti, J. Mabillard, T. Reid, B.W. Brock, Advances
in Water Resources 94 (2016) 457–469.
date_created: 2023-02-20T08:15:11Z
date_published: 2016-08-01T00:00:00Z
date_updated: 2024-10-14T12:04:30Z
day: '01'
doi: 10.1016/j.advwatres.2016.05.001
extern: '1'
fulldoi: https://doi.org/10.1016/j.advwatres.2016.05.001
intvolume: ' 94'
keyword:
- Water Science and Technology
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1016/j.advwatres.2016.05.001
month: '08'
oa: 1
oa_version: Published Version
page: 457-469
publication: Advances in Water Resources
publication_identifier:
issn:
- 0309-1708
publication_status: published
publisher: Elsevier
quality_controlled: '1'
scopus_import: '1'
status: public
title: An enhanced temperature index model for debris-covered glaciers accounting
for thickness effect
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 94
year: '2016'
...
---
_id: '12621'
abstract:
- lang: eng
text: Near-surface air temperature is an important determinant of the surface energy
balance of glaciers and is often represented by a constant linear temperature
gradients (TGs) in models. Spatio-temporal variability in 2 m air temperature
was measured across the debris-covered Miage Glacier, Italy, over an 89 d period
during the 2014 ablation season using a network of 19 stations. Air temperature
was found to be strongly dependent upon elevation for most stations, even under
varying meteorological conditions and at different times of day, and its spatial
variability was well explained by a locally derived mean linear TG (MG–TG) of
−0.0088°C m−1. However, local temperature depressions occurred over areas of very
thin or patchy debris cover. The MG–TG, together with other air TGs, extrapolated
from both on- and off-glacier sites, were applied in a distributed energy-balance
model. Compared with piecewise air temperature extrapolation from all on-glacier
stations, modelled ablation, using the MG–TG, increased by <1%, increasing to
>4% using the environmental ‘lapse rate’. Ice melt under thick debris was relatively
insensitive to air temperature, while the effects of different temperature extrapolation
methods were strongest at high elevation sites of thin and patchy debris cover.
article_processing_charge: No
article_type: original
author:
- first_name: THOMAS E.
full_name: SHAW, THOMAS E.
last_name: SHAW
- first_name: BEN W.
full_name: BROCK, BEN W.
last_name: BROCK
- first_name: CATRIONA L.
full_name: FYFFE, CATRIONA L.
last_name: FYFFE
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: NICK
full_name: RUTTER, NICK
last_name: RUTTER
- first_name: FABRIZIO
full_name: DIOTRI, FABRIZIO
last_name: DIOTRI
citation:
ama: SHAW TE, BROCK BW, FYFFE CL, Pellicciotti F, RUTTER N, DIOTRI F. Air temperature
distribution and energy-balance modelling of a debris-covered glacier. Journal
of Glaciology. 2016;62(231):185-198. doi:10.1017/jog.2016.31
apa: SHAW, T. E., BROCK, B. W., FYFFE, C. L., Pellicciotti, F., RUTTER, N., &
DIOTRI, F. (2016). Air temperature distribution and energy-balance modelling of
a debris-covered glacier. Journal of Glaciology. Cambridge University Press.
https://doi.org/10.1017/jog.2016.31
chicago: SHAW, THOMAS E., BEN W. BROCK, CATRIONA L. FYFFE, Francesca Pellicciotti,
NICK RUTTER, and FABRIZIO DIOTRI. “Air Temperature Distribution and Energy-Balance
Modelling of a Debris-Covered Glacier.” Journal of Glaciology. Cambridge
University Press, 2016. https://doi.org/10.1017/jog.2016.31.
ieee: T. E. SHAW, B. W. BROCK, C. L. FYFFE, F. Pellicciotti, N. RUTTER, and F. DIOTRI,
“Air temperature distribution and energy-balance modelling of a debris-covered
glacier,” Journal of Glaciology, vol. 62, no. 231. Cambridge University
Press, pp. 185–198, 2016.
ista: SHAW TE, BROCK BW, FYFFE CL, Pellicciotti F, RUTTER N, DIOTRI F. 2016. Air
temperature distribution and energy-balance modelling of a debris-covered glacier.
Journal of Glaciology. 62(231), 185–198.
mla: SHAW, THOMAS E., et al. “Air Temperature Distribution and Energy-Balance Modelling
of a Debris-Covered Glacier.” Journal of Glaciology, vol. 62, no. 231,
Cambridge University Press, 2016, pp. 185–98, doi:10.1017/jog.2016.31.
short: T.E. SHAW, B.W. BROCK, C.L. FYFFE, F. Pellicciotti, N. RUTTER, F. DIOTRI,
Journal of Glaciology 62 (2016) 185–198.
date_created: 2023-02-20T08:15:17Z
date_published: 2016-02-01T00:00:00Z
date_updated: 2023-02-24T10:30:03Z
day: '01'
doi: 10.1017/jog.2016.31
extern: '1'
fulldoi: https://doi.org/10.1017/jog.2016.31
intvolume: ' 62'
issue: '231'
keyword:
- Earth-Surface Processes
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1017/jog.2016.31
month: '02'
oa: 1
oa_version: Published Version
page: 185-198
publication: Journal of Glaciology
publication_identifier:
eissn:
- 1727-5652
issn:
- 0022-1430
publication_status: published
publisher: Cambridge University Press
scopus_import: '1'
status: public
title: Air temperature distribution and energy-balance modelling of a debris-covered
glacier
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 62
year: '2016'
...
---
_id: '12622'
abstract:
- lang: eng
text: Air temperature is a key control of processes affecting snow and glaciers
in high-elevation catchments, including melt, snowfall and sublimation. It is
therefore a key input variable to models of land–surface–atmosphere interaction.
Despite this importance, its spatial variability is poorly understood and simple
assumptions are made to extrapolate it from point observations to the catchment
scale. We use a dataset of 2.75 years of air temperature measurements (from May
2012 to November 2014) at a network of up to 27 locations in the Langtang River,
Nepal, catchment to investigate air temperature seasonality and consistency between
years. We use observations from high elevations and from the easternmost section
of the basin to corroborate previous findings of shallow lapse rates. Seasonal
variability is strong, with shallowest lapse rates during the monsoon season.
Diurnal variability is also strong and should be taken into account since processes
such as melt have a pronounced diurnal variability. Use of seasonal lapse rates
seems crucial for glacio-hydrological modelling, but seasonal lapse rates seem
stable over the 2–3 years investigated. Lateral variability at transects across
valley is high and dominated by aspect, with south-facing sites being warmer than
north-facing sites and deviations from the fitted lapse rates of up to several
degrees. Local factors (e.g. topographic shading) can reduce or enhance this effect.
The interplay of radiation, aspect and elevation should be further investigated
with high-elevation transects.
article_processing_charge: No
article_type: original
author:
- first_name: Martin
full_name: Heynen, Martin
last_name: Heynen
- first_name: Evan
full_name: Miles, Evan
last_name: Miles
- first_name: Silvan
full_name: Ragettli, Silvan
last_name: Ragettli
- first_name: Pascal
full_name: Buri, Pascal
last_name: Buri
- first_name: Walter W.
full_name: Immerzeel, Walter W.
last_name: Immerzeel
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: Heynen M, Miles E, Ragettli S, Buri P, Immerzeel WW, Pellicciotti F. Air temperature
variability in a high-elevation Himalayan catchment. Annals of Glaciology.
2016;57(71):212-222. doi:10.3189/2016aog71a076
apa: Heynen, M., Miles, E., Ragettli, S., Buri, P., Immerzeel, W. W., & Pellicciotti,
F. (2016). Air temperature variability in a high-elevation Himalayan catchment.
Annals of Glaciology. International Glaciological Society. https://doi.org/10.3189/2016aog71a076
chicago: Heynen, Martin, Evan Miles, Silvan Ragettli, Pascal Buri, Walter W. Immerzeel,
and Francesca Pellicciotti. “Air Temperature Variability in a High-Elevation Himalayan
Catchment.” Annals of Glaciology. International Glaciological Society,
2016. https://doi.org/10.3189/2016aog71a076.
ieee: M. Heynen, E. Miles, S. Ragettli, P. Buri, W. W. Immerzeel, and F. Pellicciotti,
“Air temperature variability in a high-elevation Himalayan catchment,” Annals
of Glaciology, vol. 57, no. 71. International Glaciological Society, pp. 212–222,
2016.
ista: Heynen M, Miles E, Ragettli S, Buri P, Immerzeel WW, Pellicciotti F. 2016.
Air temperature variability in a high-elevation Himalayan catchment. Annals of
Glaciology. 57(71), 212–222.
mla: Heynen, Martin, et al. “Air Temperature Variability in a High-Elevation Himalayan
Catchment.” Annals of Glaciology, vol. 57, no. 71, International Glaciological
Society, 2016, pp. 212–22, doi:10.3189/2016aog71a076.
short: M. Heynen, E. Miles, S. Ragettli, P. Buri, W.W. Immerzeel, F. Pellicciotti,
Annals of Glaciology 57 (2016) 212–222.
date_created: 2023-02-20T08:15:25Z
date_published: 2016-03-01T00:00:00Z
date_updated: 2023-02-24T10:25:38Z
day: '01'
doi: 10.3189/2016aog71a076
extern: '1'
fulldoi: https://doi.org/10.3189/2016aog71a076
intvolume: ' 57'
issue: '71'
keyword:
- Earth-Surface Processes
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.3189/2016AoG71A076
month: '03'
oa: 1
oa_version: Published Version
page: 212-222
publication: Annals of Glaciology
publication_identifier:
eissn:
- 1727-5644
issn:
- 0260-3055
publication_status: published
publisher: International Glaciological Society
quality_controlled: '1'
scopus_import: '1'
status: public
title: Air temperature variability in a high-elevation Himalayan catchment
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 57
year: '2016'
...
---
_id: '12623'
abstract:
- lang: eng
text: Ice cliffs might be partly responsible for the high mass losses of debris-covered
glaciers in the Hindu Kush-Karakoram-Himalaya region. The few existing models
of cliff backwasting are point-scale models applied at few locations or assume
cliffs to be planes with constant slope and aspect, a major simplification given
the complex surfaces of most cliffs. We develop the first grid-based model of
cliff backwasting for two cliffs on debris-covered Lirung Glacier, Nepal. The
model includes an improved representation of shortwave and longwave radiation,
and their interplay with the glacier topography. Shortwave radiation varies considerably
across the two cliffs, mostly due to direct radiation. Diffuse radiation is the
major shortwave component, as the direct component is strongly reduced by the
cliffs’ aspect and slope through self-shading. Incoming longwave radiation is
higher than the total incoming shortwave flux, due to radiation emitted by the
surrounding terrain, which is 25% of the incoming flux. Melt is highly variable
in space, suggesting that simple models provide inaccurate estimates of total
melt volumes. Although only representing 0.09% of the glacier tongue area, the
total melt at the two cliffs over the measurement period is 2313 and 8282 m3,
1.23% of the total melt simulated by a glacio-hydrological model for the glacier’s
tongue.
article_processing_charge: No
article_type: original
author:
- first_name: Pascal
full_name: Buri, Pascal
last_name: Buri
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: Jakob F.
full_name: Steiner, Jakob F.
last_name: Steiner
- first_name: Evan S.
full_name: Miles, Evan S.
last_name: Miles
- first_name: Walter W.
full_name: Immerzeel, Walter W.
last_name: Immerzeel
citation:
ama: Buri P, Pellicciotti F, Steiner JF, Miles ES, Immerzeel WW. A grid-based model
of backwasting of supraglacial ice cliffs on debris-covered glaciers. Annals
of Glaciology. 2016;57(71):199-211. doi:10.3189/2016aog71a059
apa: Buri, P., Pellicciotti, F., Steiner, J. F., Miles, E. S., & Immerzeel,
W. W. (2016). A grid-based model of backwasting of supraglacial ice cliffs on
debris-covered glaciers. Annals of Glaciology. International Glaciological
Society. https://doi.org/10.3189/2016aog71a059
chicago: Buri, Pascal, Francesca Pellicciotti, Jakob F. Steiner, Evan S. Miles,
and Walter W. Immerzeel. “A Grid-Based Model of Backwasting of Supraglacial Ice
Cliffs on Debris-Covered Glaciers.” Annals of Glaciology. International
Glaciological Society, 2016. https://doi.org/10.3189/2016aog71a059.
ieee: P. Buri, F. Pellicciotti, J. F. Steiner, E. S. Miles, and W. W. Immerzeel,
“A grid-based model of backwasting of supraglacial ice cliffs on debris-covered
glaciers,” Annals of Glaciology, vol. 57, no. 71. International Glaciological
Society, pp. 199–211, 2016.
ista: Buri P, Pellicciotti F, Steiner JF, Miles ES, Immerzeel WW. 2016. A grid-based
model of backwasting of supraglacial ice cliffs on debris-covered glaciers. Annals
of Glaciology. 57(71), 199–211.
mla: Buri, Pascal, et al. “A Grid-Based Model of Backwasting of Supraglacial Ice
Cliffs on Debris-Covered Glaciers.” Annals of Glaciology, vol. 57, no.
71, International Glaciological Society, 2016, pp. 199–211, doi:10.3189/2016aog71a059.
short: P. Buri, F. Pellicciotti, J.F. Steiner, E.S. Miles, W.W. Immerzeel, Annals
of Glaciology 57 (2016) 199–211.
date_created: 2023-02-20T08:15:34Z
date_published: 2016-03-01T00:00:00Z
date_updated: 2023-02-24T10:20:24Z
day: '01'
doi: 10.3189/2016aog71a059
extern: '1'
fulldoi: https://doi.org/10.3189/2016aog71a059
intvolume: ' 57'
issue: '71'
keyword:
- Earth-Surface Processes
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.3189/2016AoG71A059
month: '03'
oa: 1
oa_version: Published Version
page: 199-211
publication: Annals of Glaciology
publication_identifier:
eissn:
- 1727-5644
issn:
- 0260-3055
publication_status: published
publisher: International Glaciological Society
quality_controlled: '1'
scopus_import: '1'
status: public
title: A grid-based model of backwasting of supraglacial ice cliffs on debris-covered
glaciers
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 57
year: '2016'
...
---
_id: '12624'
abstract:
- lang: eng
text: Supraglacial ponds on debris-covered glaciers present a mechanism of atmosphere/glacier
energy transfer that is poorly studied, and only conceptually included in mass-balance
studies of debris-covered glaciers. This research advances previous efforts to
develop a model of mass and energy balance for supraglacial ponds by applying
a free-convection approach to account for energy exchanges at the subaqueous bare-ice
surfaces. We develop the model using field data from a pond on Lirung Glacier,
Nepal, that was monitored during the 2013 and 2014 monsoon periods. Sensitivity
testing is performed for several key parameters, and alternative melt algorithms
are compared with the model. The pond acts as a significant recipient of energy
for the glacier system, and actively participates in the glacier’s hydrologic
system during the monsoon. Melt rates are 2-4 cm d-1 (total of 98.5 m3 over the
study period) for bare ice in contact with the pond, and <1 mmd-1 (total of 10.6m3)
for the saturated debris zone. The majority of absorbed atmospheric energy leaves
the pond system through englacial conduits, delivering sufficient energy to melt
2612 m3 additional ice over the study period (38.4 m3 d-1). Such melting might
be expected to lead to subsidence of the glacier surface. Supraglacial ponds efficiently
convey atmospheric energy to the glacier’s interior and rapidly promote the downwasting
process.
article_processing_charge: No
article_type: original
author:
- first_name: Evan S.
full_name: Miles, Evan S.
last_name: Miles
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: Ian C.
full_name: Willis, Ian C.
last_name: Willis
- first_name: Jakob F.
full_name: Steiner, Jakob F.
last_name: Steiner
- first_name: Pascal
full_name: Buri, Pascal
last_name: Buri
- first_name: Neil S.
full_name: Arnold, Neil S.
last_name: Arnold
citation:
ama: Miles ES, Pellicciotti F, Willis IC, Steiner JF, Buri P, Arnold NS. Refined
energy-balance modelling of a supraglacial pond, Langtang Khola, Nepal. Annals
of Glaciology. 2016;57(71):29-40. doi:10.3189/2016aog71a421
apa: Miles, E. S., Pellicciotti, F., Willis, I. C., Steiner, J. F., Buri, P., &
Arnold, N. S. (2016). Refined energy-balance modelling of a supraglacial pond,
Langtang Khola, Nepal. Annals of Glaciology. International Glaciological
Society. https://doi.org/10.3189/2016aog71a421
chicago: Miles, Evan S., Francesca Pellicciotti, Ian C. Willis, Jakob F. Steiner,
Pascal Buri, and Neil S. Arnold. “Refined Energy-Balance Modelling of a Supraglacial
Pond, Langtang Khola, Nepal.” Annals of Glaciology. International Glaciological
Society, 2016. https://doi.org/10.3189/2016aog71a421.
ieee: E. S. Miles, F. Pellicciotti, I. C. Willis, J. F. Steiner, P. Buri, and N.
S. Arnold, “Refined energy-balance modelling of a supraglacial pond, Langtang
Khola, Nepal,” Annals of Glaciology, vol. 57, no. 71. International Glaciological
Society, pp. 29–40, 2016.
ista: Miles ES, Pellicciotti F, Willis IC, Steiner JF, Buri P, Arnold NS. 2016.
Refined energy-balance modelling of a supraglacial pond, Langtang Khola, Nepal.
Annals of Glaciology. 57(71), 29–40.
mla: Miles, Evan S., et al. “Refined Energy-Balance Modelling of a Supraglacial
Pond, Langtang Khola, Nepal.” Annals of Glaciology, vol. 57, no. 71, International
Glaciological Society, 2016, pp. 29–40, doi:10.3189/2016aog71a421.
short: E.S. Miles, F. Pellicciotti, I.C. Willis, J.F. Steiner, P. Buri, N.S. Arnold,
Annals of Glaciology 57 (2016) 29–40.
date_created: 2023-02-20T08:15:42Z
date_published: 2016-03-01T00:00:00Z
date_updated: 2023-02-24T10:17:29Z
day: '01'
doi: 10.3189/2016aog71a421
extern: '1'
fulldoi: https://doi.org/10.3189/2016aog71a421
intvolume: ' 57'
issue: '71'
keyword:
- Earth-Surface Processes
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.3189/2016AoG71A421
month: '03'
oa: 1
oa_version: Published Version
page: 29-40
publication: Annals of Glaciology
publication_identifier:
eissn:
- 1727-5644
issn:
- 0260-3055
publication_status: published
publisher: International Glaciological Society
quality_controlled: '1'
scopus_import: '1'
status: public
title: Refined energy-balance modelling of a supraglacial pond, Langtang Khola, Nepal
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 57
year: '2016'
...
---
_id: '12625'
abstract:
- lang: eng
text: Debris-covered glaciers play an important role in the high-altitude water
cycle in the Himalaya, yet their dynamics are poorly understood, partly because
of the difficult fieldwork conditions. In this study we therefore deploy an unmanned
aerial vehicle (UAV) three times (May 2013, October 2013 and May 2014) over the
debris-covered Lirung Glacier in Nepal. The acquired data are processed into orthomosaics
and elevation models by a Structure from Motion workflow, and seasonal surface
velocity is derived using frequency cross-correlation. In order to obtain optimal
surface velocity products, the effects of different input data and correlator
configurations are evaluated, which reveals that the orthomosaic as input paired
with moderate correlator settings provides the best results. The glacier has considerable
spatial and seasonal differences in surface velocity, with maximum summer and
winter velocities 6 and 2.5 m a-1, respectively, in the upper part of the tongue,
while the lower part is nearly stagnant. It is hypothesized that the higher velocities
during summer are caused by basal sliding due to increased lubrication of the
bed. We conclude that UAVs have great potential to quantify seasonal and annual
variations in flow and can help to further our understanding of debris-covered
glaciers.
article_processing_charge: No
article_type: original
author:
- first_name: Philip
full_name: Kraaijenbrink, Philip
last_name: Kraaijenbrink
- first_name: Sander W.
full_name: Meijer, Sander W.
last_name: Meijer
- first_name: Joseph M.
full_name: Shea, Joseph M.
last_name: Shea
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
- first_name: Steven M.
full_name: De Jong, Steven M.
last_name: De Jong
- first_name: Walter W.
full_name: Immerzeel, Walter W.
last_name: Immerzeel
citation:
ama: Kraaijenbrink P, Meijer SW, Shea JM, Pellicciotti F, De Jong SM, Immerzeel
WW. Seasonal surface velocities of a Himalayan glacier derived by automated correlation
of unmanned aerial vehicle imagery. Annals of Glaciology. 2016;57(71):103-113.
doi:10.3189/2016aog71a072
apa: Kraaijenbrink, P., Meijer, S. W., Shea, J. M., Pellicciotti, F., De Jong, S.
M., & Immerzeel, W. W. (2016). Seasonal surface velocities of a Himalayan
glacier derived by automated correlation of unmanned aerial vehicle imagery. Annals
of Glaciology. International Glaciological Society. https://doi.org/10.3189/2016aog71a072
chicago: Kraaijenbrink, Philip, Sander W. Meijer, Joseph M. Shea, Francesca Pellicciotti,
Steven M. De Jong, and Walter W. Immerzeel. “Seasonal Surface Velocities of a
Himalayan Glacier Derived by Automated Correlation of Unmanned Aerial Vehicle
Imagery.” Annals of Glaciology. International Glaciological Society, 2016.
https://doi.org/10.3189/2016aog71a072.
ieee: P. Kraaijenbrink, S. W. Meijer, J. M. Shea, F. Pellicciotti, S. M. De Jong,
and W. W. Immerzeel, “Seasonal surface velocities of a Himalayan glacier derived
by automated correlation of unmanned aerial vehicle imagery,” Annals of Glaciology,
vol. 57, no. 71. International Glaciological Society, pp. 103–113, 2016.
ista: Kraaijenbrink P, Meijer SW, Shea JM, Pellicciotti F, De Jong SM, Immerzeel
WW. 2016. Seasonal surface velocities of a Himalayan glacier derived by automated
correlation of unmanned aerial vehicle imagery. Annals of Glaciology. 57(71),
103–113.
mla: Kraaijenbrink, Philip, et al. “Seasonal Surface Velocities of a Himalayan Glacier
Derived by Automated Correlation of Unmanned Aerial Vehicle Imagery.” Annals
of Glaciology, vol. 57, no. 71, International Glaciological Society, 2016,
pp. 103–13, doi:10.3189/2016aog71a072.
short: P. Kraaijenbrink, S.W. Meijer, J.M. Shea, F. Pellicciotti, S.M. De Jong,
W.W. Immerzeel, Annals of Glaciology 57 (2016) 103–113.
date_created: 2023-02-20T08:15:56Z
date_published: 2016-03-01T00:00:00Z
date_updated: 2023-02-24T10:11:46Z
day: '01'
doi: 10.3189/2016aog71a072
extern: '1'
fulldoi: https://doi.org/10.3189/2016aog71a072
intvolume: ' 57'
issue: '71'
keyword:
- Earth-Surface Processes
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.3189/2016AoG71A072
month: '03'
oa: 1
oa_version: Published Version
page: 103-113
publication: Annals of Glaciology
publication_identifier:
eissn:
- 1727-5644
issn:
- 0260-3055
publication_status: published
publisher: International Glaciological Society
quality_controlled: '1'
scopus_import: '1'
status: public
title: Seasonal surface velocities of a Himalayan glacier derived by automated correlation
of unmanned aerial vehicle imagery
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 57
year: '2016'
...
---
_id: '1263'
abstract:
- lang: eng
text: Linking classical microwave electrical circuits to the optical telecommunication
band is at the core of modern communication. Future quantum information networks
will require coherent microwave-to-optical conversion to link electronic quantum
processors and memories via low-loss optical telecommunication networks. Efficient
conversion can be achieved with electro-optical modulators operating at the single
microwave photon level. In the standard electro-optic modulation scheme, this
is impossible because both up- and down-converted sidebands are necessarily present.
Here, we demonstrate true single-sideband up- or down-conversion in a triply resonant
whispering gallery mode resonator by explicitly addressing modes with asymmetric
free spectral range. Compared to previous experiments, we show a 3 orders of magnitude
improvement of the electro-optical conversion efficiency, reaching 0.1% photon
number conversion for a 10 GHz microwave tone at 0.42 mW of optical pump power.
The presented scheme is fully compatible with existing superconducting 3D circuit
quantum electrodynamics technology and can be used for nonclassical state conversion
and communication. Our conversion bandwidth is larger than 1 MHz and is not fundamentally
limited.
acknowledgement: Alexander von Humboldt Foundation; Studienstiftung des Deutschen
Volkes. We would like to acknowledge our stimulating discussions with Konrad Lehnert
and Alessandro Pitanti.
article_processing_charge: No
author:
- first_name: Alfredo
full_name: Rueda, Alfredo
last_name: Rueda
- first_name: Florian
full_name: Sedlmeir, Florian
last_name: Sedlmeir
- first_name: Michele
full_name: Collodo, Michele
last_name: Collodo
- first_name: Ulrich
full_name: Vogl, Ulrich
last_name: Vogl
- first_name: Birgit
full_name: Stiller, Birgit
last_name: Stiller
- first_name: Gerhard
full_name: Schunk, Gerhard
last_name: Schunk
- first_name: Dmitry
full_name: Strekalov, Dmitry
last_name: Strekalov
- first_name: Christoph
full_name: Marquardt, Christoph
last_name: Marquardt
- first_name: Johannes M
full_name: Fink, Johannes M
id: 4B591CBA-F248-11E8-B48F-1D18A9856A87
last_name: Fink
orcid: 0000-0001-8112-028X
- first_name: Oskar
full_name: Painter, Oskar
last_name: Painter
- first_name: Gerd
full_name: Leuchs, Gerd
last_name: Leuchs
- first_name: Harald
full_name: Schwefel, Harald
last_name: Schwefel
citation:
ama: 'Rueda A, Sedlmeir F, Collodo M, et al. Efficient microwave to optical photon
conversion: An electro-optical realization. Optica. 2016;3(6):597-604.
doi:10.1364/OPTICA.3.000597'
apa: 'Rueda, A., Sedlmeir, F., Collodo, M., Vogl, U., Stiller, B., Schunk, G., …
Schwefel, H. (2016). Efficient microwave to optical photon conversion: An electro-optical
realization. Optica. Optica Publishing Group. https://doi.org/10.1364/OPTICA.3.000597'
chicago: 'Rueda, Alfredo, Florian Sedlmeir, Michele Collodo, Ulrich Vogl, Birgit
Stiller, Gerhard Schunk, Dmitry Strekalov, et al. “Efficient Microwave to Optical
Photon Conversion: An Electro-Optical Realization.” Optica. Optica Publishing
Group, 2016. https://doi.org/10.1364/OPTICA.3.000597.'
ieee: 'A. Rueda et al., “Efficient microwave to optical photon conversion:
An electro-optical realization,” Optica, vol. 3, no. 6. Optica Publishing
Group, pp. 597–604, 2016.'
ista: 'Rueda A, Sedlmeir F, Collodo M, Vogl U, Stiller B, Schunk G, Strekalov D,
Marquardt C, Fink JM, Painter O, Leuchs G, Schwefel H. 2016. Efficient microwave
to optical photon conversion: An electro-optical realization. Optica. 3(6), 597–604.'
mla: 'Rueda, Alfredo, et al. “Efficient Microwave to Optical Photon Conversion:
An Electro-Optical Realization.” Optica, vol. 3, no. 6, Optica Publishing
Group, 2016, pp. 597–604, doi:10.1364/OPTICA.3.000597.'
short: A. Rueda, F. Sedlmeir, M. Collodo, U. Vogl, B. Stiller, G. Schunk, D. Strekalov,
C. Marquardt, J.M. Fink, O. Painter, G. Leuchs, H. Schwefel, Optica 3 (2016) 597–604.
date_created: 2018-12-11T11:51:01Z
date_published: 2016-06-20T00:00:00Z
date_updated: 2026-06-18T17:28:15Z
day: '20'
ddc:
- '580'
department:
- _id: JoFi
doi: 10.1364/OPTICA.3.000597
external_id:
isi:
- '000378847400007'
fulldoi: https://doi.org/10.1364/OPTICA.3.000597
intvolume: ' 3'
isi: 1
issue: '6'
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1364/OPTICA.3.000597
month: '06'
oa: 1
oa_version: Published Version
page: 597 - 604
publication: Optica
publication_status: published
publisher: Optica Publishing Group
publist_id: '6061'
quality_controlled: '1'
scopus_import: '1'
status: public
title: 'Efficient microwave to optical photon conversion: An electro-optical realization'
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 3
year: '2016'
...
---
_id: '1264'
abstract:
- lang: eng
text: n contrast with the wealth of recent reports about the function of μ-adaptins
and clathrin adaptor protein (AP) complexes, there is very little information
about the motifs that determine the sorting of membrane proteins within clathrin-coated
vesicles in plants. Here, we investigated putative sorting signals in the large
cytosolic loop of the Arabidopsis (Arabidopsis thaliana) PIN-FORMED1 (PIN1) auxin
transporter, which are involved in binding μ-adaptins and thus in PIN1 trafficking
and localization. We found that Phe-165 and Tyr-280, Tyr-328, and Tyr-394 are
involved in the binding of different μ-adaptins in vitro. However, only Phe-165,
which binds μA(μ2)- and μD(μ3)-adaptin, was found to be essential for PIN1 trafficking
and localization in vivo. The PIN1:GFP-F165A mutant showed reduced endocytosis
but also localized to intracellular structures containing several layers of membranes
and endoplasmic reticulum (ER) markers, suggesting that they correspond to ER
or ER-derived membranes. While PIN1:GFP localized normally in a μA (μ2)-adaptin
mutant, it accumulated in big intracellular structures containing LysoTracker
in a μD (μ3)-adaptin mutant, consistent with previous results obtained with mutants
of other subunits of the AP-3 complex. Our data suggest that Phe-165, through
the binding of μA (μ2)- and μD (μ3)-adaptin, is important for PIN1 endocytosis
and for PIN1 trafficking along the secretory pathway, respectively.
acknowledgement: "We thank Dr. R. Offringa (Leiden University) for providing the GST-\r\nPIN-CL
construct; Sandra Richter and Gerd Jurgens (University of Tübin-\r\ngen) for providing
the estradiol-inducible PIN1-RFP construct and the\r\ngnl1 mutant expressing BFA-sensitive
GNL1; F.J. Santonja (University of Valencia)\r\nfor help with the statistical analysis;
Jurgen Kleine-Vehn, Elke Barbez, and\r\nEva Benkova for helpful discussions; the
Salk Institute Genomic Analysis\r\nLaboratory for providing the sequence-indexed
Arabidopsis T-DNA in-\r\nsertion mutants; and the greenhouse section and the microscopy
section\r\nof SCSIE (University of Valencia) and Pilar Selvi for excellent technical\r\nassistance."
article_processing_charge: No
author:
- first_name: Gloria
full_name: Sancho Andrés, Gloria
last_name: Sancho Andrés
- first_name: Esther
full_name: Soriano Ortega, Esther
last_name: Soriano Ortega
- first_name: Caiji
full_name: Gao, Caiji
last_name: Gao
- first_name: Joan
full_name: Bernabé Orts, Joan
last_name: Bernabé Orts
- first_name: Madhumitha
full_name: Narasimhan, Madhumitha
id: 44BF24D0-F248-11E8-B48F-1D18A9856A87
last_name: Narasimhan
orcid: 0000-0002-8600-0671
- first_name: Anna
full_name: Müller, Anna
id: 420AB15A-F248-11E8-B48F-1D18A9856A87
last_name: Müller
- first_name: Ricardo
full_name: Tejos, Ricardo
last_name: Tejos
- first_name: Liwen
full_name: Jiang, Liwen
last_name: Jiang
- first_name: Jirí
full_name: Friml, Jirí
id: 4159519E-F248-11E8-B48F-1D18A9856A87
last_name: Friml
orcid: 0000-0002-8302-7596
- first_name: Fernando
full_name: Aniento, Fernando
last_name: Aniento
- first_name: Maria
full_name: Marcote, Maria
last_name: Marcote
citation:
ama: Sancho Andrés G, Soriano Ortega E, Gao C, et al. Sorting motifs involved in
the trafficking and localization of the PIN1 auxin efflux carrier. Plant Physiology.
2016;171(3):1965-1982. doi:10.1104/pp.16.00373
apa: Sancho Andrés, G., Soriano Ortega, E., Gao, C., Bernabé Orts, J., Narasimhan,
M., Müller, A., … Marcote, M. (2016). Sorting motifs involved in the trafficking
and localization of the PIN1 auxin efflux carrier. Plant Physiology. American
Society of Plant Biologists. https://doi.org/10.1104/pp.16.00373
chicago: Sancho Andrés, Gloria, Esther Soriano Ortega, Caiji Gao, Joan Bernabé Orts,
Madhumitha Narasimhan, Anna Müller, Ricardo Tejos, et al. “Sorting Motifs Involved
in the Trafficking and Localization of the PIN1 Auxin Efflux Carrier.” Plant
Physiology. American Society of Plant Biologists, 2016. https://doi.org/10.1104/pp.16.00373.
ieee: G. Sancho Andrés et al., “Sorting motifs involved in the trafficking
and localization of the PIN1 auxin efflux carrier,” Plant Physiology, vol.
171, no. 3. American Society of Plant Biologists, pp. 1965–1982, 2016.
ista: Sancho Andrés G, Soriano Ortega E, Gao C, Bernabé Orts J, Narasimhan M, Müller
A, Tejos R, Jiang L, Friml J, Aniento F, Marcote M. 2016. Sorting motifs involved
in the trafficking and localization of the PIN1 auxin efflux carrier. Plant Physiology.
171(3), 1965–1982.
mla: Sancho Andrés, Gloria, et al. “Sorting Motifs Involved in the Trafficking and
Localization of the PIN1 Auxin Efflux Carrier.” Plant Physiology, vol.
171, no. 3, American Society of Plant Biologists, 2016, pp. 1965–82, doi:10.1104/pp.16.00373.
short: G. Sancho Andrés, E. Soriano Ortega, C. Gao, J. Bernabé Orts, M. Narasimhan,
A. Müller, R. Tejos, L. Jiang, J. Friml, F. Aniento, M. Marcote, Plant Physiology
171 (2016) 1965–1982.
date_created: 2018-12-11T11:51:01Z
date_published: 2016-07-01T00:00:00Z
date_updated: 2025-09-22T08:58:52Z
day: '01'
department:
- _id: JiFr
- _id: EvBe
doi: 10.1104/pp.16.00373
ec_funded: 1
external_id:
isi:
- '000381303300037'
fulldoi: https://doi.org/10.1104/pp.16.00373
intvolume: ' 171'
isi: 1
issue: '3'
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4936568/
month: '07'
oa: 1
oa_version: Submitted Version
page: 1965 - 1982
project:
- _id: 25716A02-B435-11E9-9278-68D0E5697425
call_identifier: FP7
grant_number: '282300'
name: Polarity and subcellular dynamics in plants
publication: Plant Physiology
publication_status: published
publisher: American Society of Plant Biologists
publist_id: '6059'
quality_controlled: '1'
scopus_import: '1'
status: public
title: Sorting motifs involved in the trafficking and localization of the PIN1 auxin
efflux carrier
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 171
year: '2016'
...