• Sorted by Date • Sorted by Last Name of First Author •
Sherpa, Sonam Futi and Werth, Susanna, 2025. Investigating the Influence of Climate Seasonality on Glacier Mass Changes in High Mountain Asia via GRACE Observations. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 18:20545–20562, doi:10.1109/JSTARS.2025.3595165.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025IJSTA..1820545S,
author = {{Sherpa}, Sonam Futi and {Werth}, Susanna},
title = "{Investigating the Influence of Climate Seasonality on Glacier Mass Changes in High Mountain Asia via GRACE Observations}",
journal = {IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing},
keywords = {Gravimetry, gravity recovery and climate experiment/follow-on (GRACE/FO) mass change, precipitation seasonality, time-series analysis, wavelet signal processing},
year = 2025,
month = jan,
volume = {18},
pages = {20545-20562},
abstract = "{Recent global warming has caused a rapid melting of high mountain Asia
(HMA) glaciers. The impact of warming on glacier mass decline is
undisputed. However, the influence of precipitation changes and
their seasonal distribution on glacier mass remains uncertain.
Here, using observations from satellite gravimetry complemented
by hydrological data for seven glacier regions, we investigate
the relationship between net glacier mass budget changes and
seasonal precipitation patterns by applying time series and
wavelet-based signal decomposition approaches. For a total HMA
glacier mass loss of 22.23 8.61 Gt/yr during 20022016, the
highest portions are contributed by the glacier regions Central
Himalaya, Eastern Himalaya, and Tien Shan with 11.99 1.24 Gt/yr,
8.62 0.99 Gt/yr, and 6.93 0.97 Gt/yr, respectively. We found a
high association between glacier mass loss and increased
rainfall during Western Himalayas monsoon season, decreased
snowfall during postmonsoon months in Eastern Himalaya, and
increased rainfall during the premonsoon season for Central
Himalaya. These associations partly derive from frequency bands
at 34.5-year and 58-year periods, which conform with typical
repeat patterns of the South Asian Monsoon (SAM). Since
precipitation seasonality of several HMA regions is strongly
influenced by SAM, this raises the question of which role a
climate change-induced SAM alteration would play in glacier
melting. We conclude that especially summer-fed and SAM-
dominated HMA glacier regions are vulnerable to accelerated
melting from changes in precipitation seasonality driven by SAM
alterations. We call for denser and more accurate spatial
monitoring of meteorological variables to accurately predict the
impact of monsoon alterations on future melting rates.}",
doi = {10.1109/JSTARS.2025.3595165},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025IJSTA..1820545S},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
Generated by
bib2html_grace.pl
(written by Patrick Riley
modified for this page by Volker Klemann) on
Mon Dec 15, 2025 18:11:59
GRACE-FO
Mon Dec 15, F. Flechtner![]()