---
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '22502'
abstract:
- lang: eng
  text: "The Indian and East Asian summer monsoons shape the melt and accumulation
    patterns of glaciers in High Mountain Asia in complex ways due to the interaction
    of persistent cloud cover, large temperature ranges, high atmospheric water content
    and high precipitation rates. Glacier energy- and mass-balance modelling using
    in situ measurements offers insights into the ways in which surface processes
    are shaped by climatic regimes. In this study, we use a full energy- and mass-balance
    model and seven on-glacier automatic weather station datasets from different parts
    of the Central and Eastern Himalaya to investigate how monsoon conditions influence
    the glacier surface energy and mass balance. In particular, we look at how debris-covered
    and debris-free glaciers respond differently to monsoonal conditions. The radiation
    budget primarily controls the melt of clean-ice glaciers, but turbulent fluxes
    play an important role in modulating the melt energy on debris-covered glaciers.
    The sensible heat flux decreases during core monsoon, but the latent heat flux
    cools the surface due to evaporation of liquid water. This interplay of radiative
    and turbulent fluxes causes debris-covered glacier melt rates to stay almost constant
    through the different phases of the monsoon. Ice melt under thin debris, on the
    other hand, is amplified by both the dark surface and the turbulent fluxes, which
    intensify melt during monsoon through surface heating and condensation. Pre-monsoon
    snow cover can considerably delay melt onset and have a strong impact on the seasonal
    mass balance. Intermittent monsoon snow cover lowers the melt rates at high elevation.
    This work is fundamental to the understanding of the present and future Himalayan
    cryosphere and water budget, while informing and motivating further glacier- and
    catchment-scale research using process-based models.The radiation budget primarily
    controls the melt of clean-ice glaciers, but turbulent fluxes play an important
    role in modulating the melt energy on debris-covered glaciers. The sensible heat
    flux decreases during core monsoon, but the latent heat flux cools the surface
    due to evaporation of liquid water. This interplay of radiative and turbulent
    fluxes causes debris-covered glacier melt rates to stay almost constant through
    the different phases of the monsoon. Ice melt under thin debris, on the other
    hand, is amplified by both the dark surface and the turbulent fluxes, which intensify
    melt during monsoon through surface heating and condensation.\r\nPre-monsoon snow
    cover can considerably delay melt onset and have a strong impact on the seasonal
    mass balance. Intermittent monsoon snow cover lowers the melt rates at high elevation.
    This work is fundamental to the understanding of the present and future Himalayan
    cryosphere and water budget, while informing and motivating further glacier- and
    catchment-scale research using process-based models.</jats:p>"
article_processing_charge: No
article_type: original
author:
- first_name: Stefan
  full_name: Fugger, Stefan
  last_name: Fugger
- first_name: Catriona L.
  full_name: Fyffe, Catriona L.
  last_name: Fyffe
- first_name: Simone
  full_name: Fatichi, Simone
  id: cf8e546b-a9b0-11f0-a43b-aa89ed1b56d6
  last_name: Fatichi
- first_name: Evan
  full_name: Miles, Evan
  last_name: Miles
- first_name: Michael
  full_name: McCarthy, Michael
  last_name: McCarthy
- first_name: Thomas E.
  full_name: Shaw, Thomas E.
  last_name: Shaw
- first_name: Baohong
  full_name: Ding, Baohong
  last_name: Ding
- first_name: Wei
  full_name: Yang, Wei
  last_name: Yang
- first_name: Patrick
  full_name: Wagnon, Patrick
  last_name: Wagnon
- first_name: Walter
  full_name: Immerzeel, Walter
  last_name: Immerzeel
- first_name: Qiao
  full_name: Liu, Qiao
  last_name: Liu
- first_name: Francesca
  full_name: Pellicciotti, Francesca
  last_name: Pellicciotti
citation:
  ama: Fugger S, Fyffe CL, Fatichi S, et al. Understanding monsoon controls on the
    energy and mass balance of glaciers in the Central and Eastern Himalaya. <i>The
    Cryosphere</i>. 2022;16(5):1631-1652. doi:<a href="https://doi.org/10.5194/tc-16-1631-2022">10.5194/tc-16-1631-2022</a>
  apa: Fugger, S., Fyffe, C. L., Fatichi, S., Miles, E., McCarthy, M., Shaw, T. E.,
    … Pellicciotti, F. (2022). Understanding monsoon controls on the energy and mass
    balance of glaciers in the Central and Eastern Himalaya. <i>The Cryosphere</i>.
    Copernicus Publications. <a href="https://doi.org/10.5194/tc-16-1631-2022">https://doi.org/10.5194/tc-16-1631-2022</a>
  chicago: Fugger, Stefan, Catriona L. Fyffe, Simone Fatichi, Evan Miles, Michael
    McCarthy, Thomas E. Shaw, Baohong Ding, et al. “Understanding Monsoon Controls
    on the Energy and Mass Balance of Glaciers in the Central and Eastern Himalaya.”
    <i>The Cryosphere</i>. Copernicus Publications, 2022. <a href="https://doi.org/10.5194/tc-16-1631-2022">https://doi.org/10.5194/tc-16-1631-2022</a>.
  ieee: S. Fugger <i>et al.</i>, “Understanding monsoon controls on the energy and
    mass balance of glaciers in the Central and Eastern Himalaya,” <i>The Cryosphere</i>,
    vol. 16, no. 5. Copernicus Publications, pp. 1631–1652, 2022.
  ista: Fugger S, Fyffe CL, Fatichi S, Miles E, McCarthy M, Shaw TE, Ding B, Yang
    W, Wagnon P, Immerzeel W, Liu Q, Pellicciotti F. 2022. Understanding monsoon controls
    on the energy and mass balance of glaciers in the Central and Eastern Himalaya.
    The Cryosphere. 16(5), 1631–1652.
  mla: Fugger, Stefan, et al. “Understanding Monsoon Controls on the Energy and Mass
    Balance of Glaciers in the Central and Eastern Himalaya.” <i>The Cryosphere</i>,
    vol. 16, no. 5, Copernicus Publications, 2022, pp. 1631–52, doi:<a href="https://doi.org/10.5194/tc-16-1631-2022">10.5194/tc-16-1631-2022</a>.
  short: S. Fugger, C.L. Fyffe, S. Fatichi, E. Miles, M. McCarthy, T.E. Shaw, B. Ding,
    W. Yang, P. Wagnon, W. Immerzeel, Q. Liu, F. Pellicciotti, The Cryosphere 16 (2022)
    1631–1652.
das_tickbox: '1'
date_created: 2026-07-27T12:30:24Z
date_published: 2022-05-05T00:00:00Z
date_updated: 2026-08-06T11:17:17Z
day: '05'
doi: 10.5194/tc-16-1631-2022
extern: '1'
intvolume: '        16'
issue: '5'
language:
- iso: eng
main_file_link:
- open_access: '1'
  url: https://doi.org/10.5194/tc-16-1631-2022
month: '05'
oa: 1
oa_version: Published Version
page: 1631-1652
publication: The Cryosphere
publication_identifier:
  eissn:
  - 1994-0424
publication_status: published
publisher: Copernicus Publications
quality_controlled: '1'
scopus_import: '1'
status: public
title: Understanding monsoon controls on the energy and mass balance of glaciers in
  the Central and Eastern Himalaya
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: ba8df636-2132-11f1-aed0-ed93e2281fdd
volume: 16
year: '2022'
...
