Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations
Journal homepage: http://journals.ametsoc.org/loi/clim Hydrologic cycle intensification is an expected manifestation of a warming climate. Although positive trends in several global average quantities have been reported, no previous studies have documented broad intensification across elements of th...
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Online Access: | http://hdl.handle.net/11250/109001 https://doi.org/10.1175/2010JCLI3421.1 |
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ftimr:oai:imr.brage.unit.no:11250/109001 2024-09-15T17:53:24+00:00 Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations Rawlins, Michael A. Steele, Michael Holland, Marika H. Adam, Jennifer C. Cherry, Jessica E. Francis, Jennifer A. Groisman, Pavel Ya Hinzman, Larry D. Huntington, Thomas G. Kane, Douglas L. Kimball, John S. Kwok, Ron Lammers, Richard B. Lee, Craig M. Lettenmaier, Dennis P. McDonald, Kyle C. Podest, Erika Pundsack, Jonathan W. Rudels, Bert Serreze, Mark C. Shiklomanov, Alexander Skagseth, Øystein Troy, Tara J. Vörösmarty, Charles J. Wensnahan, Mark Wood, Eric F. Woodgate, Rebecca Yang, Daqing Zhang, Ke Zhang, Tingjun 2010 application/pdf http://hdl.handle.net/11250/109001 https://doi.org/10.1175/2010JCLI3421.1 eng eng American Meteorological Society urn:issn:0894-8755 urn:issn:1520-0442 http://hdl.handle.net/11250/109001 http://dx.doi.org/10.1175/2010JCLI3421.1 5715-5737 23 Journal of Climate 21 climate change klimaendringer temperature changes temperaturendringer artic freshwater cycle arktisk ferskvanns syklus VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488 Journal article Peer reviewed 2010 ftimr https://doi.org/10.1175/2010JCLI3421.1 2024-07-31T03:37:25Z Journal homepage: http://journals.ametsoc.org/loi/clim Hydrologic cycle intensification is an expected manifestation of a warming climate. Although positive trends in several global average quantities have been reported, no previous studies have documented broad intensification across elements of the Arctic freshwater cycle (FWC). In this study we examine the character and quantitative significance of changes in annual precipitation, evapotranspiration, and river discharge across the terrestrial pan-Arctic over the past several decades from observations and a suite of coupled general circulation models (GCMs). Trends in freshwater flux and storage derived from observations across the Arctic Ocean and surrounding seas are also described. With few exceptions, precipitation, evapotranspiration, and river discharge fluxes from observations and the GCMs exhibit positive trends. Significant positive trends above the 90% confidence level, however, are not present for all of the observations. Greater confidence in the GCM trends arises through lower inter-annual variability relative to trend magnitude. Put another way, intrinsic variability in the observations limits our confidence in the robustness of their increases. Ocean fluxes are less certain, due primarily to the lack of long-term observations. Where available, salinity and volume flux data suggest some decrease in salt-water inflow to the Barents Sea (i.e., a decrease in freshwater outflow) in recent decades. A decline in freshwater storage across the central Arctic Ocean and suggestions that large-scale circulation plays a dominant role in freshwater trends raise questions as to whether Arctic Ocean freshwater flows are intensifying. Although oceanic fluxes of freshwater are highly variable and consistent trends are difficult to verify, the other components of the Arctic FWC do show consistent positive trends over recent decades. The broad-scale increases provide evidence that the Arctic FWC is experiencing intensification. Efforts which aim to develop an ... Article in Journal/Newspaper Arctic Ocean Arktis* Barents Sea Climate change Institute for Marine Research: Brage IMR Journal of Climate 23 21 5715 5737 |
institution |
Open Polar |
collection |
Institute for Marine Research: Brage IMR |
op_collection_id |
ftimr |
language |
English |
topic |
climate change klimaendringer temperature changes temperaturendringer artic freshwater cycle arktisk ferskvanns syklus VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488 |
spellingShingle |
climate change klimaendringer temperature changes temperaturendringer artic freshwater cycle arktisk ferskvanns syklus VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488 Rawlins, Michael A. Steele, Michael Holland, Marika H. Adam, Jennifer C. Cherry, Jessica E. Francis, Jennifer A. Groisman, Pavel Ya Hinzman, Larry D. Huntington, Thomas G. Kane, Douglas L. Kimball, John S. Kwok, Ron Lammers, Richard B. Lee, Craig M. Lettenmaier, Dennis P. McDonald, Kyle C. Podest, Erika Pundsack, Jonathan W. Rudels, Bert Serreze, Mark C. Shiklomanov, Alexander Skagseth, Øystein Troy, Tara J. Vörösmarty, Charles J. Wensnahan, Mark Wood, Eric F. Woodgate, Rebecca Yang, Daqing Zhang, Ke Zhang, Tingjun Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations |
topic_facet |
climate change klimaendringer temperature changes temperaturendringer artic freshwater cycle arktisk ferskvanns syklus VDP::Mathematics and natural science: 400::Zoology and botany: 480::Ecology: 488 |
description |
Journal homepage: http://journals.ametsoc.org/loi/clim Hydrologic cycle intensification is an expected manifestation of a warming climate. Although positive trends in several global average quantities have been reported, no previous studies have documented broad intensification across elements of the Arctic freshwater cycle (FWC). In this study we examine the character and quantitative significance of changes in annual precipitation, evapotranspiration, and river discharge across the terrestrial pan-Arctic over the past several decades from observations and a suite of coupled general circulation models (GCMs). Trends in freshwater flux and storage derived from observations across the Arctic Ocean and surrounding seas are also described. With few exceptions, precipitation, evapotranspiration, and river discharge fluxes from observations and the GCMs exhibit positive trends. Significant positive trends above the 90% confidence level, however, are not present for all of the observations. Greater confidence in the GCM trends arises through lower inter-annual variability relative to trend magnitude. Put another way, intrinsic variability in the observations limits our confidence in the robustness of their increases. Ocean fluxes are less certain, due primarily to the lack of long-term observations. Where available, salinity and volume flux data suggest some decrease in salt-water inflow to the Barents Sea (i.e., a decrease in freshwater outflow) in recent decades. A decline in freshwater storage across the central Arctic Ocean and suggestions that large-scale circulation plays a dominant role in freshwater trends raise questions as to whether Arctic Ocean freshwater flows are intensifying. Although oceanic fluxes of freshwater are highly variable and consistent trends are difficult to verify, the other components of the Arctic FWC do show consistent positive trends over recent decades. The broad-scale increases provide evidence that the Arctic FWC is experiencing intensification. Efforts which aim to develop an ... |
format |
Article in Journal/Newspaper |
author |
Rawlins, Michael A. Steele, Michael Holland, Marika H. Adam, Jennifer C. Cherry, Jessica E. Francis, Jennifer A. Groisman, Pavel Ya Hinzman, Larry D. Huntington, Thomas G. Kane, Douglas L. Kimball, John S. Kwok, Ron Lammers, Richard B. Lee, Craig M. Lettenmaier, Dennis P. McDonald, Kyle C. Podest, Erika Pundsack, Jonathan W. Rudels, Bert Serreze, Mark C. Shiklomanov, Alexander Skagseth, Øystein Troy, Tara J. Vörösmarty, Charles J. Wensnahan, Mark Wood, Eric F. Woodgate, Rebecca Yang, Daqing Zhang, Ke Zhang, Tingjun |
author_facet |
Rawlins, Michael A. Steele, Michael Holland, Marika H. Adam, Jennifer C. Cherry, Jessica E. Francis, Jennifer A. Groisman, Pavel Ya Hinzman, Larry D. Huntington, Thomas G. Kane, Douglas L. Kimball, John S. Kwok, Ron Lammers, Richard B. Lee, Craig M. Lettenmaier, Dennis P. McDonald, Kyle C. Podest, Erika Pundsack, Jonathan W. Rudels, Bert Serreze, Mark C. Shiklomanov, Alexander Skagseth, Øystein Troy, Tara J. Vörösmarty, Charles J. Wensnahan, Mark Wood, Eric F. Woodgate, Rebecca Yang, Daqing Zhang, Ke Zhang, Tingjun |
author_sort |
Rawlins, Michael A. |
title |
Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations |
title_short |
Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations |
title_full |
Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations |
title_fullStr |
Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations |
title_full_unstemmed |
Analysis of the Arctic System for Freshwater Cycle Intensification: Observations and Expectations |
title_sort |
analysis of the arctic system for freshwater cycle intensification: observations and expectations |
publisher |
American Meteorological Society |
publishDate |
2010 |
url |
http://hdl.handle.net/11250/109001 https://doi.org/10.1175/2010JCLI3421.1 |
genre |
Arctic Ocean Arktis* Barents Sea Climate change |
genre_facet |
Arctic Ocean Arktis* Barents Sea Climate change |
op_source |
5715-5737 23 Journal of Climate 21 |
op_relation |
urn:issn:0894-8755 urn:issn:1520-0442 http://hdl.handle.net/11250/109001 http://dx.doi.org/10.1175/2010JCLI3421.1 |
op_doi |
https://doi.org/10.1175/2010JCLI3421.1 |
container_title |
Journal of Climate |
container_volume |
23 |
container_issue |
21 |
container_start_page |
5715 |
op_container_end_page |
5737 |
_version_ |
1810295477640364032 |