Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century

Quantifying the spatial and temporal patterns of the water lost to the atmosphere through land surface evapotranspiration (ET) is essential for understanding the global hydrological cycle, but remains much uncertain. In this study, we use the Dynamic Land Ecosystem Model to estimate the global terre...

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Main Authors: Pan, Shufen, Tian, Hanqin, Dangal, Shree, Yang, Qichun, Yang, Jia, Lu, Chaoqun, Tao, Bo, Ren, Wei, Ouyang, Zhiyun
Other Authors: Hanqin Tian, tianhan@auburn.edu
Format: Text
Language:unknown
Published: American Geophysical Union 2015
Subjects:
Online Access:https://doi.org/10.1002/2014EF000263
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014EF000263
https://aurora.auburn.edu/handle/11200/50535
https://doi.org/10.35099/aurora-603
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spelling ftunivauburn:oai:aurora.auburn.edu:11200/50535 2023-09-26T15:15:12+02:00 Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century Pan, Shufen Tian, Hanqin Dangal, Shree Yang, Qichun Yang, Jia Lu, Chaoqun Tao, Bo Ren, Wei Ouyang, Zhiyun Hanqin Tian, tianhan@auburn.edu 2015 PDF application/pdf https://doi.org/10.1002/2014EF000263 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014EF000263 https://aurora.auburn.edu/handle/11200/50535 https://doi.org/10.35099/aurora-603 unknown American Geophysical Union Earth's Future 2328-4277 doi:10.1002/2014EF000263 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014EF000263 https://aurora.auburn.edu/handle/11200/50535 http://dx.doi.org/10.35099/aurora-603 ©American Geophysical Union 2015. This is this the version of record co-published by the American Geophysical Union and John Wiley & Sons, Inc. It is made available under the CC-BY-NC-ND 4.0 license. Item should be cited as: Pan, Shufen, et al. (2015). "Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century." Earth's Future 3(1): 15-35. climate change evapotranspiration terrestrial ecosystem modeling terrestrial ecosystems Text Journal Article, Academic Journal 2015 ftunivauburn https://doi.org/10.1002/2014EF00026310.35099/aurora-603 2023-08-29T09:37:55Z Quantifying the spatial and temporal patterns of the water lost to the atmosphere through land surface evapotranspiration (ET) is essential for understanding the global hydrological cycle, but remains much uncertain. In this study, we use the Dynamic Land Ecosystem Model to estimate the global terrestrial ET during 2000-2009 and project its changes in response to climate change and increasing atmospheric CO2 under two IPCC SRES scenarios (A2 and B1) during 2010-2099. Modeled results show a mean annual global terrestrial ET of about 549 (545-552) mm yr(-1) during 2000-2009. Relative to the 2000s, global terrestrial ET for the 2090s would increase by 30.7 mm yr(-1) (5.6%) and 13.2 mm yr(-1) (2.4%) under the A2 and B1 scenarios, respectively. About 60% of global land area would experience increasing ET at rates of over 9.5 mm decade(-1) over the study period under the A2 scenario. The Arctic region would have the largest ET increase (16% compared with the 2000s level) due to larger increase in temperature than other regions. Decreased ET would mainly take place in regions like central and western Asia, northern Africa, Australia, eastern South America, and Greenland due to declines in soil moisture and changing rainfall patterns. Our results indicate that warming temperature and increasing precipitation would result in large increase in ET by the end of the 21st century, while increasing atmospheric CO2 would be responsible for decrease in ET, given the reduction of stomatal conductance under elevated CO2. Published Yes Text Arctic Climate change Greenland AUrora - Auburn University Scholarly Repository Arctic Greenland
institution Open Polar
collection AUrora - Auburn University Scholarly Repository
op_collection_id ftunivauburn
language unknown
topic climate change
evapotranspiration
terrestrial ecosystem modeling
terrestrial ecosystems
spellingShingle climate change
evapotranspiration
terrestrial ecosystem modeling
terrestrial ecosystems
Pan, Shufen
Tian, Hanqin
Dangal, Shree
Yang, Qichun
Yang, Jia
Lu, Chaoqun
Tao, Bo
Ren, Wei
Ouyang, Zhiyun
Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century
topic_facet climate change
evapotranspiration
terrestrial ecosystem modeling
terrestrial ecosystems
description Quantifying the spatial and temporal patterns of the water lost to the atmosphere through land surface evapotranspiration (ET) is essential for understanding the global hydrological cycle, but remains much uncertain. In this study, we use the Dynamic Land Ecosystem Model to estimate the global terrestrial ET during 2000-2009 and project its changes in response to climate change and increasing atmospheric CO2 under two IPCC SRES scenarios (A2 and B1) during 2010-2099. Modeled results show a mean annual global terrestrial ET of about 549 (545-552) mm yr(-1) during 2000-2009. Relative to the 2000s, global terrestrial ET for the 2090s would increase by 30.7 mm yr(-1) (5.6%) and 13.2 mm yr(-1) (2.4%) under the A2 and B1 scenarios, respectively. About 60% of global land area would experience increasing ET at rates of over 9.5 mm decade(-1) over the study period under the A2 scenario. The Arctic region would have the largest ET increase (16% compared with the 2000s level) due to larger increase in temperature than other regions. Decreased ET would mainly take place in regions like central and western Asia, northern Africa, Australia, eastern South America, and Greenland due to declines in soil moisture and changing rainfall patterns. Our results indicate that warming temperature and increasing precipitation would result in large increase in ET by the end of the 21st century, while increasing atmospheric CO2 would be responsible for decrease in ET, given the reduction of stomatal conductance under elevated CO2. Published Yes
author2 Hanqin Tian, tianhan@auburn.edu
format Text
author Pan, Shufen
Tian, Hanqin
Dangal, Shree
Yang, Qichun
Yang, Jia
Lu, Chaoqun
Tao, Bo
Ren, Wei
Ouyang, Zhiyun
author_facet Pan, Shufen
Tian, Hanqin
Dangal, Shree
Yang, Qichun
Yang, Jia
Lu, Chaoqun
Tao, Bo
Ren, Wei
Ouyang, Zhiyun
author_sort Pan, Shufen
title Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century
title_short Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century
title_full Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century
title_fullStr Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century
title_full_unstemmed Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century
title_sort responses of global terrestrial evapotranspiration to climate change and increasing atmospheric co2 in the 21st century
publisher American Geophysical Union
publishDate 2015
url https://doi.org/10.1002/2014EF000263
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014EF000263
https://aurora.auburn.edu/handle/11200/50535
https://doi.org/10.35099/aurora-603
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Climate change
Greenland
genre_facet Arctic
Climate change
Greenland
op_relation Earth's Future
2328-4277
doi:10.1002/2014EF000263
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014EF000263
https://aurora.auburn.edu/handle/11200/50535
http://dx.doi.org/10.35099/aurora-603
op_rights ©American Geophysical Union 2015. This is this the version of record co-published by the American Geophysical Union and John Wiley & Sons, Inc. It is made available under the CC-BY-NC-ND 4.0 license. Item should be cited as: Pan, Shufen, et al. (2015). "Responses of global terrestrial evapotranspiration to climate change and increasing atmospheric CO2 in the 21st century." Earth's Future 3(1): 15-35.
op_doi https://doi.org/10.1002/2014EF00026310.35099/aurora-603
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