The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum
Abstract Proxy reconstructions and model simulations of precipitation during Earth's glacial periods suggest that the locations and mechanisms of atmospheric moisture transport have changed considerably during Earth's past. We investigate the hydroclimate of the Last Glacial Maximum (LGM)...
Published in: | Geophysical Research Letters |
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ftdoajarticles:oai:doaj.org/article:ce6ae8efec3d40c1975b0799f27a4157 2024-09-09T19:55:35+00:00 The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum J. M. Lora C. B. Skinner W. D. Rush S. H. Baek 2023-09-01T00:00:00Z https://doi.org/10.1029/2023GL104805 https://doaj.org/article/ce6ae8efec3d40c1975b0799f27a4157 EN eng Wiley https://doi.org/10.1029/2023GL104805 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL104805 https://doaj.org/article/ce6ae8efec3d40c1975b0799f27a4157 Geophysical Research Letters, Vol 50, Iss 18, Pp n/a-n/a (2023) atmospheric rivers hydroclimate Last Glacial Maximum paleoclimate Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL104805 2024-08-05T17:49:23Z Abstract Proxy reconstructions and model simulations of precipitation during Earth's glacial periods suggest that the locations and mechanisms of atmospheric moisture transport have changed considerably during Earth's past. We investigate the hydroclimate of the Last Glacial Maximum (LGM) using simulations with the Community Earth System Model, with a focus on the extratropics and the influence of atmospheric rivers (ARs), a key driver of modern‐day moisture transport globally. Mean and extreme precipitation increase significantly over southwestern Patagonia, Iberia, and southwestern North America—mid‐latitude regions affected by ARs in the modern climate—despite overall decreases elsewhere. In each, the associated moisture transport changes are different, with increased transport and AR activity mainly occurring in the North Atlantic. The overall LGM response is dominated by the response to ice sheets, with other forcings causing additional cooling and drying over the extratropics and a strong decrease of moisture transport over the subpolar North Atlantic. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Patagonia Geophysical Research Letters 50 18 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
atmospheric rivers hydroclimate Last Glacial Maximum paleoclimate Geophysics. Cosmic physics QC801-809 |
spellingShingle |
atmospheric rivers hydroclimate Last Glacial Maximum paleoclimate Geophysics. Cosmic physics QC801-809 J. M. Lora C. B. Skinner W. D. Rush S. H. Baek The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum |
topic_facet |
atmospheric rivers hydroclimate Last Glacial Maximum paleoclimate Geophysics. Cosmic physics QC801-809 |
description |
Abstract Proxy reconstructions and model simulations of precipitation during Earth's glacial periods suggest that the locations and mechanisms of atmospheric moisture transport have changed considerably during Earth's past. We investigate the hydroclimate of the Last Glacial Maximum (LGM) using simulations with the Community Earth System Model, with a focus on the extratropics and the influence of atmospheric rivers (ARs), a key driver of modern‐day moisture transport globally. Mean and extreme precipitation increase significantly over southwestern Patagonia, Iberia, and southwestern North America—mid‐latitude regions affected by ARs in the modern climate—despite overall decreases elsewhere. In each, the associated moisture transport changes are different, with increased transport and AR activity mainly occurring in the North Atlantic. The overall LGM response is dominated by the response to ice sheets, with other forcings causing additional cooling and drying over the extratropics and a strong decrease of moisture transport over the subpolar North Atlantic. |
format |
Article in Journal/Newspaper |
author |
J. M. Lora C. B. Skinner W. D. Rush S. H. Baek |
author_facet |
J. M. Lora C. B. Skinner W. D. Rush S. H. Baek |
author_sort |
J. M. Lora |
title |
The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum |
title_short |
The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum |
title_full |
The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum |
title_fullStr |
The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum |
title_full_unstemmed |
The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum |
title_sort |
hydrologic cycle and atmospheric rivers in cesm2 simulations of the last glacial maximum |
publisher |
Wiley |
publishDate |
2023 |
url |
https://doi.org/10.1029/2023GL104805 https://doaj.org/article/ce6ae8efec3d40c1975b0799f27a4157 |
geographic |
Patagonia |
geographic_facet |
Patagonia |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Geophysical Research Letters, Vol 50, Iss 18, Pp n/a-n/a (2023) |
op_relation |
https://doi.org/10.1029/2023GL104805 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL104805 https://doaj.org/article/ce6ae8efec3d40c1975b0799f27a4157 |
op_doi |
https://doi.org/10.1029/2023GL104805 |
container_title |
Geophysical Research Letters |
container_volume |
50 |
container_issue |
18 |
_version_ |
1809925476699865088 |