Historical glacier change on Svalbard predicts doubling of mass loss by 2100

The melting of glaciers and ice caps accounts for about one-third of current sea-level rise , exceeding the mass loss from the more voluminous Greenland or Antarctic Ice Sheets. The Arctic archipelago of Svalbard, which hosts spatial climate gradients that are larger than the expected temporal clima...

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Main Authors: Geyman, Emily C., van Pelt, J. J. Ward, Maloof, Adam C., Aas, Harald Faste, Kohler, Jack
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 2022
Subjects:
Online Access:https://doi.org/10.1038/s41586-021-04314-4
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spelling ftcaltechauth:oai:authors.library.caltech.edu:rym9y-eqx76 2024-10-13T14:01:48+00:00 Historical glacier change on Svalbard predicts doubling of mass loss by 2100 Geyman, Emily C. van Pelt, J. J. Ward Maloof, Adam C. Aas, Harald Faste Kohler, Jack 2022-01-20 https://doi.org/10.1038/s41586-021-04314-4 unknown Nature Publishing Group https://www.doi.org/10.21334/npolar.2021.f6afca5c https://doi.org/10.5281/zenodo.5806388 https://toposvalbard.npolar.no/ https://publicdatasets.data.npolar.no/kartdata/S0_Terrengmodell/Delmodell/ https://geodata.npolar.no/#basemap-data https://doi.org/10.5281/zenodo.5643856 https://doi.org/10.5281/zenodo.5644415 eprintid:112998 info:eu-repo/semantics/openAccess Other Nature, 601(7893), 374-379, (2022-01-20) Cryospheric science Projection and prediction Multidisciplinary info:eu-repo/semantics/article 2022 ftcaltechauth https://doi.org/10.1038/s41586-021-04314-410.21334/npolar.2021.f6afca5c10.5281/zenodo.580638810.5281/zenodo.564385610.5281/zenodo.5644415 2024-09-25T18:46:45Z The melting of glaciers and ice caps accounts for about one-third of current sea-level rise , exceeding the mass loss from the more voluminous Greenland or Antarctic Ice Sheets. The Arctic archipelago of Svalbard, which hosts spatial climate gradients that are larger than the expected temporal climate shifts over the next century, is a natural laboratory to constrain the climate sensitivity of glaciers and predict their response to future warming. Here we link historical and modern glacier observations to predict that twenty-first century glacier thinning rates will more than double those from 1936 to 2010. Making use of an archive of historical aerial imagery7 from 1936 and 1938, we use structure-from-motion photogrammetry to reconstruct the three-dimensional geometry of 1,594 glaciers across Svalbard. We compare these reconstructions to modern ice elevation data to derive the spatial pattern of mass balance over a more than 70-year timespan, enabling us to see through the noise of annual and decadal variability to quantify how variables such as temperature and precipitation control ice loss. We find a robust temperature dependence of melt rates, whereby a 1 °C rise in mean summer temperature corresponds to a decrease in area-normalized mass balance of −0.28 m yr−1 of water equivalent. Finally, we design a space-for-time substitution8 to combine our historical glacier observations with climate projections and make first-order predictions of twenty-first century glacier change across Svalbard. © 2022 Nature Publishing Group. Received 17 June 2021; Accepted 07 December 2021; Published 19 January 2022. We thank F. Simons, C.-Y. Lai, P. Wennberg, P. Moore, B. Dyer, G. Moholdt, R.A. Morris, E. Isaksson, A. Schomacker, C. Nuth, E. Schytt Holmlund and B. Geyman for conversations that improved the manuscript. W.J.J.v.P. acknowledges funding from the Swedish National Space Agency (project 189/18). E.C.G. was supported by a Daniel M. Sachs Class of 1960 Global Scholarship at Princeton University, a Svalbard ... Article in Journal/Newspaper Antarc* Antarctic Arctic Archipelago Arctic glacier glacier Greenland Svalbard Caltech Authors (California Institute of Technology) Arctic Antarctic Svalbard Greenland Dyer ENVELOPE(-81.366,-81.366,50.550,50.550)
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
topic Cryospheric science
Projection and prediction
Multidisciplinary
spellingShingle Cryospheric science
Projection and prediction
Multidisciplinary
Geyman, Emily C.
van Pelt, J. J. Ward
Maloof, Adam C.
Aas, Harald Faste
Kohler, Jack
Historical glacier change on Svalbard predicts doubling of mass loss by 2100
topic_facet Cryospheric science
Projection and prediction
Multidisciplinary
description The melting of glaciers and ice caps accounts for about one-third of current sea-level rise , exceeding the mass loss from the more voluminous Greenland or Antarctic Ice Sheets. The Arctic archipelago of Svalbard, which hosts spatial climate gradients that are larger than the expected temporal climate shifts over the next century, is a natural laboratory to constrain the climate sensitivity of glaciers and predict their response to future warming. Here we link historical and modern glacier observations to predict that twenty-first century glacier thinning rates will more than double those from 1936 to 2010. Making use of an archive of historical aerial imagery7 from 1936 and 1938, we use structure-from-motion photogrammetry to reconstruct the three-dimensional geometry of 1,594 glaciers across Svalbard. We compare these reconstructions to modern ice elevation data to derive the spatial pattern of mass balance over a more than 70-year timespan, enabling us to see through the noise of annual and decadal variability to quantify how variables such as temperature and precipitation control ice loss. We find a robust temperature dependence of melt rates, whereby a 1 °C rise in mean summer temperature corresponds to a decrease in area-normalized mass balance of −0.28 m yr−1 of water equivalent. Finally, we design a space-for-time substitution8 to combine our historical glacier observations with climate projections and make first-order predictions of twenty-first century glacier change across Svalbard. © 2022 Nature Publishing Group. Received 17 June 2021; Accepted 07 December 2021; Published 19 January 2022. We thank F. Simons, C.-Y. Lai, P. Wennberg, P. Moore, B. Dyer, G. Moholdt, R.A. Morris, E. Isaksson, A. Schomacker, C. Nuth, E. Schytt Holmlund and B. Geyman for conversations that improved the manuscript. W.J.J.v.P. acknowledges funding from the Swedish National Space Agency (project 189/18). E.C.G. was supported by a Daniel M. Sachs Class of 1960 Global Scholarship at Princeton University, a Svalbard ...
format Article in Journal/Newspaper
author Geyman, Emily C.
van Pelt, J. J. Ward
Maloof, Adam C.
Aas, Harald Faste
Kohler, Jack
author_facet Geyman, Emily C.
van Pelt, J. J. Ward
Maloof, Adam C.
Aas, Harald Faste
Kohler, Jack
author_sort Geyman, Emily C.
title Historical glacier change on Svalbard predicts doubling of mass loss by 2100
title_short Historical glacier change on Svalbard predicts doubling of mass loss by 2100
title_full Historical glacier change on Svalbard predicts doubling of mass loss by 2100
title_fullStr Historical glacier change on Svalbard predicts doubling of mass loss by 2100
title_full_unstemmed Historical glacier change on Svalbard predicts doubling of mass loss by 2100
title_sort historical glacier change on svalbard predicts doubling of mass loss by 2100
publisher Nature Publishing Group
publishDate 2022
url https://doi.org/10.1038/s41586-021-04314-4
long_lat ENVELOPE(-81.366,-81.366,50.550,50.550)
geographic Arctic
Antarctic
Svalbard
Greenland
Dyer
geographic_facet Arctic
Antarctic
Svalbard
Greenland
Dyer
genre Antarc*
Antarctic
Arctic Archipelago
Arctic
glacier
glacier
Greenland
Svalbard
genre_facet Antarc*
Antarctic
Arctic Archipelago
Arctic
glacier
glacier
Greenland
Svalbard
op_source Nature, 601(7893), 374-379, (2022-01-20)
op_relation https://www.doi.org/10.21334/npolar.2021.f6afca5c
https://doi.org/10.5281/zenodo.5806388
https://toposvalbard.npolar.no/
https://publicdatasets.data.npolar.no/kartdata/S0_Terrengmodell/Delmodell/
https://geodata.npolar.no/#basemap-data
https://doi.org/10.5281/zenodo.5643856
https://doi.org/10.5281/zenodo.5644415
eprintid:112998
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1038/s41586-021-04314-410.21334/npolar.2021.f6afca5c10.5281/zenodo.580638810.5281/zenodo.564385610.5281/zenodo.5644415
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