Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard

The Arctic is undergoing increased warming compared to the global mean, which has major implications for freshwater runoff into the oceans from seasonal snow and glaciers. Here, we present high-resolution (2.5 km) simulations of glacier mass balance, runoff, and snow conditions on Svalbard from 1991...

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Published in:The Cryosphere
Main Authors: L. S. Schmidt, T. V. Schuler, E. E. Thomas, S. Westermann
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-2941-2023
https://doaj.org/article/ed1ff3836d4b47c28d35ead45b80d8f3
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spelling ftdoajarticles:oai:doaj.org/article:ed1ff3836d4b47c28d35ead45b80d8f3 2023-08-15T12:39:48+02:00 Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard L. S. Schmidt T. V. Schuler E. E. Thomas S. Westermann 2023-07-01T00:00:00Z https://doi.org/10.5194/tc-17-2941-2023 https://doaj.org/article/ed1ff3836d4b47c28d35ead45b80d8f3 EN eng Copernicus Publications https://tc.copernicus.org/articles/17/2941/2023/tc-17-2941-2023.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-17-2941-2023 1994-0416 1994-0424 https://doaj.org/article/ed1ff3836d4b47c28d35ead45b80d8f3 The Cryosphere, Vol 17, Pp 2941-2963 (2023) Environmental sciences GE1-350 Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.5194/tc-17-2941-2023 2023-07-23T00:35:22Z The Arctic is undergoing increased warming compared to the global mean, which has major implications for freshwater runoff into the oceans from seasonal snow and glaciers. Here, we present high-resolution (2.5 km) simulations of glacier mass balance, runoff, and snow conditions on Svalbard from 1991–2022, one of the fastest warming regions in the world. The simulations are created using the CryoGrid community model forced by Copernicus Arctic Regional ReAnalysis (CARRA) (1991–2021) and AROME-ARCTIC forecasts (2016–2022). Updates to the water percolation and runoff schemes are implemented in the CryoGrid model for the simulations. In situ observations available for Svalbard, including automatic weather station data, stake measurements, and discharge observations, are used to carefully evaluate the quality of the simulations and model forcing. We find a slightly negative climatic mass balance (CMB) over the simulation period of − 0.08 m w . e . yr - 1 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="8d84a44e8dceadc876a4f5187e80e616"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-17-2941-2023-ie00001.svg" width="52pt" height="15pt" src="tc-17-2941-2023-ie00001.png"/></svg:svg> but with no statistically significant trend. The most negative annual CMB is found for Nordenskiöldland ( − 0.73 m w . e . yr - 1 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="79c2734b54b21dfe576cdb9add09f447"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-17-2941-2023-ie00002.svg" width="52pt" height="15pt" src="tc-17-2941-2023-ie00002.png"/></svg:svg> ), with a significant negative trend of − 0.27 m w . e . <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="8pt" class="svg-formula" dspmath="mathimg" md5hash="53a7260869c21d86416d281790c9f913"><svg:image ... Article in Journal/Newspaper Arctic glacier Svalbard The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic Svalbard The Cryosphere 17 7 2941 2963
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
L. S. Schmidt
T. V. Schuler
E. E. Thomas
S. Westermann
Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description The Arctic is undergoing increased warming compared to the global mean, which has major implications for freshwater runoff into the oceans from seasonal snow and glaciers. Here, we present high-resolution (2.5 km) simulations of glacier mass balance, runoff, and snow conditions on Svalbard from 1991–2022, one of the fastest warming regions in the world. The simulations are created using the CryoGrid community model forced by Copernicus Arctic Regional ReAnalysis (CARRA) (1991–2021) and AROME-ARCTIC forecasts (2016–2022). Updates to the water percolation and runoff schemes are implemented in the CryoGrid model for the simulations. In situ observations available for Svalbard, including automatic weather station data, stake measurements, and discharge observations, are used to carefully evaluate the quality of the simulations and model forcing. We find a slightly negative climatic mass balance (CMB) over the simulation period of − 0.08 m w . e . yr - 1 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="8d84a44e8dceadc876a4f5187e80e616"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-17-2941-2023-ie00001.svg" width="52pt" height="15pt" src="tc-17-2941-2023-ie00001.png"/></svg:svg> but with no statistically significant trend. The most negative annual CMB is found for Nordenskiöldland ( − 0.73 m w . e . yr - 1 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="79c2734b54b21dfe576cdb9add09f447"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-17-2941-2023-ie00002.svg" width="52pt" height="15pt" src="tc-17-2941-2023-ie00002.png"/></svg:svg> ), with a significant negative trend of − 0.27 m w . e . <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="8pt" class="svg-formula" dspmath="mathimg" md5hash="53a7260869c21d86416d281790c9f913"><svg:image ...
format Article in Journal/Newspaper
author L. S. Schmidt
T. V. Schuler
E. E. Thomas
S. Westermann
author_facet L. S. Schmidt
T. V. Schuler
E. E. Thomas
S. Westermann
author_sort L. S. Schmidt
title Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard
title_short Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard
title_full Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard
title_fullStr Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard
title_full_unstemmed Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulations for Svalbard
title_sort meltwater runoff and glacier mass balance in the high arctic: 1991–2022 simulations for svalbard
publisher Copernicus Publications
publishDate 2023
url https://doi.org/10.5194/tc-17-2941-2023
https://doaj.org/article/ed1ff3836d4b47c28d35ead45b80d8f3
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
glacier
Svalbard
The Cryosphere
genre_facet Arctic
glacier
Svalbard
The Cryosphere
op_source The Cryosphere, Vol 17, Pp 2941-2963 (2023)
op_relation https://tc.copernicus.org/articles/17/2941/2023/tc-17-2941-2023.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-17-2941-2023
1994-0416
1994-0424
https://doaj.org/article/ed1ff3836d4b47c28d35ead45b80d8f3
op_doi https://doi.org/10.5194/tc-17-2941-2023
container_title The Cryosphere
container_volume 17
container_issue 7
container_start_page 2941
op_container_end_page 2963
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