A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century

Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 33 (2006): L06715, doi:10.1029/2006GL025753. Several recent publi...

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Published in:Geophysical Research Letters
Main Authors: McClelland, James W., Dery, Stephen J., Peterson, Bruce J., Holmes, Robert M., Wood, Eric F.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2006
Subjects:
Online Access:https://hdl.handle.net/1912/924
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/924 2023-05-15T14:36:03+02:00 A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century McClelland, James W. Dery, Stephen J. Peterson, Bruce J. Holmes, Robert M. Wood, Eric F. 2006-03-30 text/plain application/pdf https://hdl.handle.net/1912/924 en_US eng American Geophysical Union https://doi.org/10.1029/2006GL025753 Geophysical Research Letters 33 (2006): L06715 https://hdl.handle.net/1912/924 doi:10.1029/2006GL025753 Geophysical Research Letters 33 (2006): L06715 doi:10.1029/2006GL025753 Article 2006 ftwhoas https://doi.org/10.1029/2006GL025753 2022-05-28T22:57:03Z Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 33 (2006): L06715, doi:10.1029/2006GL025753. Several recent publications have documented changes in river discharge from arctic and subarctic watersheds. Comparison of these findings, however, has been hampered by differences in time periods and methods of analysis. Here we compare changes in discharge from different regions of the pan-arctic watershed using identical time periods and analytical methods. Discharge to the Arctic Ocean increased by 5.6 km3/y/y during 1964-2000, the net result of a large increase from Eurasia moderated by a small decrease from North America. In contrast, discharge to Hudson/James/Ungava Bays decreased by 2.5 km3/y/y during 1964-2000. While this evaluation identifies an overall increase in discharge (~120 km3/y greater discharge at the end of the time period as compared to the beginning for Hudson/James/Unvaga Bays and the Arctic Ocean combined), the contrasting regional trends also highlight the need to understand the consequences of adding/removing freshwater from particular regions of the arctic and subarctic oceans. This work was supported by the Arctic System Science Program of the National Science Foundation (NSF-OPP-0229302, NSF-OPP-0230211, NSF-OPP-0519840) and by the National Oceanic and Atmospheric Administration (NA17RJ2612). Article in Journal/Newspaper Arctic Arctic Ocean Subarctic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Arctic Arctic Ocean Hudson Geophysical Research Letters 33 6
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language English
description Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 33 (2006): L06715, doi:10.1029/2006GL025753. Several recent publications have documented changes in river discharge from arctic and subarctic watersheds. Comparison of these findings, however, has been hampered by differences in time periods and methods of analysis. Here we compare changes in discharge from different regions of the pan-arctic watershed using identical time periods and analytical methods. Discharge to the Arctic Ocean increased by 5.6 km3/y/y during 1964-2000, the net result of a large increase from Eurasia moderated by a small decrease from North America. In contrast, discharge to Hudson/James/Ungava Bays decreased by 2.5 km3/y/y during 1964-2000. While this evaluation identifies an overall increase in discharge (~120 km3/y greater discharge at the end of the time period as compared to the beginning for Hudson/James/Unvaga Bays and the Arctic Ocean combined), the contrasting regional trends also highlight the need to understand the consequences of adding/removing freshwater from particular regions of the arctic and subarctic oceans. This work was supported by the Arctic System Science Program of the National Science Foundation (NSF-OPP-0229302, NSF-OPP-0230211, NSF-OPP-0519840) and by the National Oceanic and Atmospheric Administration (NA17RJ2612).
format Article in Journal/Newspaper
author McClelland, James W.
Dery, Stephen J.
Peterson, Bruce J.
Holmes, Robert M.
Wood, Eric F.
spellingShingle McClelland, James W.
Dery, Stephen J.
Peterson, Bruce J.
Holmes, Robert M.
Wood, Eric F.
A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century
author_facet McClelland, James W.
Dery, Stephen J.
Peterson, Bruce J.
Holmes, Robert M.
Wood, Eric F.
author_sort McClelland, James W.
title A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century
title_short A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century
title_full A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century
title_fullStr A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century
title_full_unstemmed A pan-arctic evaluation of changes in river discharge during the latter half of the 20th century
title_sort pan-arctic evaluation of changes in river discharge during the latter half of the 20th century
publisher American Geophysical Union
publishDate 2006
url https://hdl.handle.net/1912/924
geographic Arctic
Arctic Ocean
Hudson
geographic_facet Arctic
Arctic Ocean
Hudson
genre Arctic
Arctic Ocean
Subarctic
genre_facet Arctic
Arctic Ocean
Subarctic
op_source Geophysical Research Letters 33 (2006): L06715
doi:10.1029/2006GL025753
op_relation https://doi.org/10.1029/2006GL025753
Geophysical Research Letters 33 (2006): L06715
https://hdl.handle.net/1912/924
doi:10.1029/2006GL025753
op_doi https://doi.org/10.1029/2006GL025753
container_title Geophysical Research Letters
container_volume 33
container_issue 6
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