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...
Published in: | The Cryosphere |
---|---|
Main Authors: | , , , |
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 |
id |
ftdoajarticles:oai:doaj.org/article:ed1ff3836d4b47c28d35ead45b80d8f3 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1774292480027525120 |