---
_id: '12603'
abstract:
- lang: eng
text: We present a field-data rich modelling analysis to reconstruct the climatic
forcing, glacier response, and runoff generation from a high-elevation catchment
in central Chile over the period 2000–2015 to provide insights into the differing
contributions of debris-covered and debris-free glaciers under current and future
changing climatic conditions. Model simulations with the physically based glacio-hydrological
model TOPKAPI-ETH reveal a period of neutral or slightly positive mass balance
between 2000 and 2010, followed by a transition to increasingly large annual mass
losses, associated with a recent mega drought. Mass losses commence earlier, and
are more severe, for a heavily debris-covered glacier, most likely due to its
strong dependence on snow avalanche accumulation, which has declined in recent
years. Catchment runoff shows a marked decreasing trend over the study period,
but with high interannual variability directly linked to winter snow accumulation,
and high contribution from ice melt in dry periods and drought conditions. The
study demonstrates the importance of incorporating local-scale processes such
as snow avalanche accumulation and spatially variable debris thickness, in understanding
the responses of different glacier types to climate change. We highlight the increased
dependency of runoff from high Andean catchments on the diminishing resource of
glacier ice during dry years.
article_processing_charge: No
article_type: original
author:
- first_name: Flavia
full_name: Burger, Flavia
last_name: Burger
- first_name: Alvaro
full_name: Ayala, Alvaro
last_name: Ayala
- first_name: David
full_name: Farias, David
last_name: Farias
- first_name: Thomas E.
full_name: Shaw, Thomas E.
last_name: Shaw
- first_name: Shelley
full_name: MacDonell, Shelley
last_name: MacDonell
- first_name: Ben
full_name: Brock, Ben
last_name: Brock
- first_name: James
full_name: McPhee, James
last_name: McPhee
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: 'Burger F, Ayala A, Farias D, et al. Interannual variability in glacier contribution
to runoff from a high‐elevation Andean catchment: Understanding the role of debris
cover in glacier hydrology. Hydrological Processes. 2018;33(2):214-229.
doi:10.1002/hyp.13354'
apa: 'Burger, F., Ayala, A., Farias, D., Shaw, T. E., MacDonell, S., Brock, B.,
… Pellicciotti, F. (2018). Interannual variability in glacier contribution to
runoff from a high‐elevation Andean catchment: Understanding the role of debris
cover in glacier hydrology. Hydrological Processes. Wiley. https://doi.org/10.1002/hyp.13354'
chicago: 'Burger, Flavia, Alvaro Ayala, David Farias, Thomas E. Shaw, Shelley MacDonell,
Ben Brock, James McPhee, and Francesca Pellicciotti. “Interannual Variability
in Glacier Contribution to Runoff from a High‐elevation Andean Catchment: Understanding
the Role of Debris Cover in Glacier Hydrology.” Hydrological Processes.
Wiley, 2018. https://doi.org/10.1002/hyp.13354.'
ieee: 'F. Burger et al., “Interannual variability in glacier contribution
to runoff from a high‐elevation Andean catchment: Understanding the role of debris
cover in glacier hydrology,” Hydrological Processes, vol. 33, no. 2. Wiley,
pp. 214–229, 2018.'
ista: 'Burger F, Ayala A, Farias D, Shaw TE, MacDonell S, Brock B, McPhee J, Pellicciotti
F. 2018. Interannual variability in glacier contribution to runoff from a high‐elevation
Andean catchment: Understanding the role of debris cover in glacier hydrology.
Hydrological Processes. 33(2), 214–229.'
mla: 'Burger, Flavia, et al. “Interannual Variability in Glacier Contribution to
Runoff from a High‐elevation Andean Catchment: Understanding the Role of Debris
Cover in Glacier Hydrology.” Hydrological Processes, vol. 33, no. 2, Wiley,
2018, pp. 214–29, doi:10.1002/hyp.13354.'
short: F. Burger, A. Ayala, D. Farias, T.E. Shaw, S. MacDonell, B. Brock, J. McPhee,
F. Pellicciotti, Hydrological Processes 33 (2018) 214–229.
date_created: 2023-02-20T08:13:14Z
date_published: 2018-11-26T00:00:00Z
date_updated: 2023-02-28T11:49:36Z
day: '26'
doi: 10.1002/hyp.13354
extern: '1'
intvolume: ' 33'
issue: '2'
keyword:
- Water Science and Technology
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1002/hyp.13354
month: '11'
oa: 1
oa_version: Published Version
page: 214-229
publication: Hydrological Processes
publication_identifier:
eissn:
- 1099-1085
issn:
- 0885-6087
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: 'Interannual variability in glacier contribution to runoff from a high‐elevation
Andean catchment: Understanding the role of debris cover in glacier hydrology'
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 33
year: '2018'
...
---
_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'
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'
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: '12633'
abstract:
- lang: eng
text: We use two hydrological models of varying complexity to study the Juncal River
Basin in the Central Andes of Chile with the aim to understand the degree of conceptualization
and the spatial structure that are needed to model present and future streamflows.
We use a conceptual semi-distributed model based on elevation bands [Water Evaluation
and Planning (WEAP)], frequently used for water management, and a physically oriented,
fully distributed model [Topographic Kinematic Wave Approximation and Integration
ETH Zurich (TOPKAPI-ETH)] developed for research purposes mainly. We evaluate
the ability of the two models to reproduce the key hydrological processes in the
basin with emphasis on snow accumulation and melt, streamflow and the relationships
between internal processes. Both models are capable of reproducing observed runoff
and the evolution of Moderate-resolution Imaging Spectroradiometer snow cover
adequately. In spite of WEAP's simple and conceptual approach for modelling snowmelt
and its lack of glacier representation and snow gravitational redistribution as
well as a proper routing algorithm, this model can reproduce historical data with
a similar goodness of fit as the more complex TOPKAPI-ETH. We show that the performance
of both models can be improved by using measured precipitation gradients of higher
temporal resolution. In contrast to the good performance of the conceptual model
for the present climate, however, we demonstrate that the simplifications in WEAP
lead to error compensation, which results in different predictions in simulated
melt and runoff for a potentially warmer future climate. TOPKAPI-ETH, using a
more physical representation of processes, depends less on calibration and thus
is less subject to a compensation of errors through different model components.
Our results show that data obtained locally in ad hoc short-term field campaigns
are needed to complement data extrapolated from long-term records for simulating
changes in the water cycle of high-elevation catchments but that these data can
only be efficiently used by a model applying a spatially distributed physical
representation of hydrological processes.
article_processing_charge: No
article_type: original
author:
- first_name: S.
full_name: Ragettli, S.
last_name: Ragettli
- first_name: G.
full_name: Cortés, G.
last_name: Cortés
- first_name: J.
full_name: McPhee, J.
last_name: McPhee
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
citation:
ama: Ragettli S, Cortés G, McPhee J, Pellicciotti F. An evaluation of approaches
for modelling hydrological processes in high-elevation, glacierized Andean watersheds.
Hydrological Processes. 2013;28(23):5674-5695. doi:10.1002/hyp.10055
apa: Ragettli, S., Cortés, G., McPhee, J., & Pellicciotti, F. (2013). An evaluation
of approaches for modelling hydrological processes in high-elevation, glacierized
Andean watersheds. Hydrological Processes. Wiley. https://doi.org/10.1002/hyp.10055
chicago: Ragettli, S., G. Cortés, J. McPhee, and Francesca Pellicciotti. “An Evaluation
of Approaches for Modelling Hydrological Processes in High-Elevation, Glacierized
Andean Watersheds.” Hydrological Processes. Wiley, 2013. https://doi.org/10.1002/hyp.10055.
ieee: S. Ragettli, G. Cortés, J. McPhee, and F. Pellicciotti, “An evaluation of
approaches for modelling hydrological processes in high-elevation, glacierized
Andean watersheds,” Hydrological Processes, vol. 28, no. 23. Wiley, pp.
5674–5695, 2013.
ista: Ragettli S, Cortés G, McPhee J, Pellicciotti F. 2013. An evaluation of approaches
for modelling hydrological processes in high-elevation, glacierized Andean watersheds.
Hydrological Processes. 28(23), 5674–5695.
mla: Ragettli, S., et al. “An Evaluation of Approaches for Modelling Hydrological
Processes in High-Elevation, Glacierized Andean Watersheds.” Hydrological Processes,
vol. 28, no. 23, Wiley, 2013, pp. 5674–95, doi:10.1002/hyp.10055.
short: S. Ragettli, G. Cortés, J. McPhee, F. Pellicciotti, Hydrological Processes
28 (2013) 5674–5695.
date_created: 2023-02-20T08:16:39Z
date_published: 2013-09-06T00:00:00Z
date_updated: 2023-02-24T08:48:40Z
day: '06'
doi: 10.1002/hyp.10055
extern: '1'
intvolume: ' 28'
issue: '23'
keyword:
- Water Science and Technology
language:
- iso: eng
month: '09'
oa_version: None
page: 5674-5695
publication: Hydrological Processes
publication_identifier:
issn:
- 0885-6087
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: An evaluation of approaches for modelling hydrological processes in high-elevation,
glacierized Andean watersheds
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 28
year: '2013'
...
---
_id: '12656'
abstract:
- lang: eng
text: We use meteorological data from two automatic weather stations (AWS) on Juncal
Norte Glacier, central Chile, to investigate the glacier–climate interaction and
to test ablation models of different complexity. The semi-arid Central Andes are
characterized by dry summers, with precipitation close to zero, low relative humidity
and intense solar radiation. We show that katabatic forcing is dominant both on
the glacier tongue and in the fore field, and that low humidity and absence of
clouds cause strong radiative cooling of the glacier surface. Surface albedo is
basically constant for snow and ice, because of the scarcity of solid precipitation.
The energy balance of the glacier is simulated for a 2-month period in austral
summer using two models of different complexity, which differ in the inclusion
of the heat conduction flux into the snowpack and in the parameterization of the
incoming longwave radiation. Net shortwave radiation is the dominant component
of the energy balance. The sensible heat flux is always positive, while both the
net longwave radiation and latent heat flux are negative. Neglecting the subsurface
heat flux and corresponding variations in surface temperature leads to an overestimation
of ablation of 2% over a total of 3695 mm water equivalent (w.e.) at the end of
the season. Correct modelling of incoming longwave radiation is crucial, and we
suggest that parameterizations based on vapour pressure and air temperature should
be used rather than on computed cloud amount. We also used an enhanced temperature-index
model incorporating the shortwave radiation flux, which has two empirical parameters.
We apply it both with values of parameters obtained for Alpine glaciers and recalibrated
on Juncal Norte. The model recalibrated against the correct energy balance simulations
performs very well. The model parameters respond to the meteorological conditions
typical of this climatic setting.
article_processing_charge: No
article_type: original
author:
- first_name: Francesca
full_name: Pellicciotti, Francesca
id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
last_name: Pellicciotti
orcid: 0000-0002-5554-8087
- first_name: Jakob
full_name: Helbing, Jakob
last_name: Helbing
- first_name: Andrés
full_name: Rivera, Andrés
last_name: Rivera
- first_name: Vincent
full_name: Favier, Vincent
last_name: Favier
- first_name: Javier
full_name: Corripio, Javier
last_name: Corripio
- first_name: José
full_name: Araos, José
last_name: Araos
- first_name: Jean-Emmanuel
full_name: Sicart, Jean-Emmanuel
last_name: Sicart
- first_name: Marco
full_name: Carenzo, Marco
last_name: Carenzo
citation:
ama: Pellicciotti F, Helbing J, Rivera A, et al. A study of the energy balance and
melt regime on Juncal Norte Glacier, semi-arid Andes of central Chile, using melt
models of different complexity. Hydrological Processes. 2008;22(19):3980-3997.
doi:10.1002/hyp.7085
apa: Pellicciotti, F., Helbing, J., Rivera, A., Favier, V., Corripio, J., Araos,
J., … Carenzo, M. (2008). A study of the energy balance and melt regime on Juncal
Norte Glacier, semi-arid Andes of central Chile, using melt models of different
complexity. Hydrological Processes. Wiley. https://doi.org/10.1002/hyp.7085
chicago: Pellicciotti, Francesca, Jakob Helbing, Andrés Rivera, Vincent Favier,
Javier Corripio, José Araos, Jean-Emmanuel Sicart, and Marco Carenzo. “A Study
of the Energy Balance and Melt Regime on Juncal Norte Glacier, Semi-Arid Andes
of Central Chile, Using Melt Models of Different Complexity.” Hydrological
Processes. Wiley, 2008. https://doi.org/10.1002/hyp.7085.
ieee: F. Pellicciotti et al., “A study of the energy balance and melt regime
on Juncal Norte Glacier, semi-arid Andes of central Chile, using melt models of
different complexity,” Hydrological Processes, vol. 22, no. 19. Wiley,
pp. 3980–3997, 2008.
ista: Pellicciotti F, Helbing J, Rivera A, Favier V, Corripio J, Araos J, Sicart
J-E, Carenzo M. 2008. A study of the energy balance and melt regime on Juncal
Norte Glacier, semi-arid Andes of central Chile, using melt models of different
complexity. Hydrological Processes. 22(19), 3980–3997.
mla: Pellicciotti, Francesca, et al. “A Study of the Energy Balance and Melt Regime
on Juncal Norte Glacier, Semi-Arid Andes of Central Chile, Using Melt Models of
Different Complexity.” Hydrological Processes, vol. 22, no. 19, Wiley,
2008, pp. 3980–97, doi:10.1002/hyp.7085.
short: F. Pellicciotti, J. Helbing, A. Rivera, V. Favier, J. Corripio, J. Araos,
J.-E. Sicart, M. Carenzo, Hydrological Processes 22 (2008) 3980–3997.
date_created: 2023-02-20T08:18:45Z
date_published: 2008-09-15T00:00:00Z
date_updated: 2024-10-14T12:00:17Z
day: '15'
doi: 10.1002/hyp.7085
extern: '1'
intvolume: ' 22'
issue: '19'
keyword:
- Water Science and Technology
language:
- iso: eng
month: '09'
oa_version: None
page: 3980-3997
publication: Hydrological Processes
publication_identifier:
eissn:
- 1099-1085
issn:
- 0885-6087
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: A study of the energy balance and melt regime on Juncal Norte Glacier, semi-arid
Andes of central Chile, using melt models of different complexity
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 22
year: '2008'
...