Soil moisture–atmosphere coupling accelerates global warming
Abstract Soil moisture–atmosphere coupling (SA) amplifies greenhouse gas-driven global warming via changes in surface heat balance. The Scenario Model Intercomparison Project projects an acceleration in SA-driven warming due to the ‘warmer climate – drier soil’ feedback, which continuously warms the...
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ftdoajarticles:oai:doaj.org/article:f67ee12a2c1f46a9ab839e0bbc3d94b1 2023-09-26T15:11:37+02:00 Soil moisture–atmosphere coupling accelerates global warming Liang Qiao Zhiyan Zuo Renhe Zhang Shilong Piao Dong Xiao Kaiwen Zhang 2023-08-01T00:00:00Z https://doi.org/10.1038/s41467-023-40641-y https://doaj.org/article/f67ee12a2c1f46a9ab839e0bbc3d94b1 EN eng Nature Portfolio https://doi.org/10.1038/s41467-023-40641-y https://doaj.org/toc/2041-1723 doi:10.1038/s41467-023-40641-y 2041-1723 https://doaj.org/article/f67ee12a2c1f46a9ab839e0bbc3d94b1 Nature Communications, Vol 14, Iss 1, Pp 1-10 (2023) Science Q article 2023 ftdoajarticles https://doi.org/10.1038/s41467-023-40641-y 2023-08-27T00:39:18Z Abstract Soil moisture–atmosphere coupling (SA) amplifies greenhouse gas-driven global warming via changes in surface heat balance. The Scenario Model Intercomparison Project projects an acceleration in SA-driven warming due to the ‘warmer climate – drier soil’ feedback, which continuously warms the globe and thereby exerts an acceleration effect on global warming. The projection shows that SA-driven warming exceeds 0.5 °C over extratropical landmasses by the end of the 21st Century. The likelihood of extreme high temperatures will additionally increase by about 10% over the entire globe (excluding Antarctica) and more than 30% over large parts of North America and Europe under the high-emission scenario. This demonstrates the high sensitivity of SA to climate change, in which SA can exceed the natural range of climate variability and play a non-linear warming component role on the globe. Article in Journal/Newspaper Antarc* Antarctica Directory of Open Access Journals: DOAJ Articles Nature Communications 14 1 |
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Science Q Liang Qiao Zhiyan Zuo Renhe Zhang Shilong Piao Dong Xiao Kaiwen Zhang Soil moisture–atmosphere coupling accelerates global warming |
topic_facet |
Science Q |
description |
Abstract Soil moisture–atmosphere coupling (SA) amplifies greenhouse gas-driven global warming via changes in surface heat balance. The Scenario Model Intercomparison Project projects an acceleration in SA-driven warming due to the ‘warmer climate – drier soil’ feedback, which continuously warms the globe and thereby exerts an acceleration effect on global warming. The projection shows that SA-driven warming exceeds 0.5 °C over extratropical landmasses by the end of the 21st Century. The likelihood of extreme high temperatures will additionally increase by about 10% over the entire globe (excluding Antarctica) and more than 30% over large parts of North America and Europe under the high-emission scenario. This demonstrates the high sensitivity of SA to climate change, in which SA can exceed the natural range of climate variability and play a non-linear warming component role on the globe. |
format |
Article in Journal/Newspaper |
author |
Liang Qiao Zhiyan Zuo Renhe Zhang Shilong Piao Dong Xiao Kaiwen Zhang |
author_facet |
Liang Qiao Zhiyan Zuo Renhe Zhang Shilong Piao Dong Xiao Kaiwen Zhang |
author_sort |
Liang Qiao |
title |
Soil moisture–atmosphere coupling accelerates global warming |
title_short |
Soil moisture–atmosphere coupling accelerates global warming |
title_full |
Soil moisture–atmosphere coupling accelerates global warming |
title_fullStr |
Soil moisture–atmosphere coupling accelerates global warming |
title_full_unstemmed |
Soil moisture–atmosphere coupling accelerates global warming |
title_sort |
soil moisture–atmosphere coupling accelerates global warming |
publisher |
Nature Portfolio |
publishDate |
2023 |
url |
https://doi.org/10.1038/s41467-023-40641-y https://doaj.org/article/f67ee12a2c1f46a9ab839e0bbc3d94b1 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Nature Communications, Vol 14, Iss 1, Pp 1-10 (2023) |
op_relation |
https://doi.org/10.1038/s41467-023-40641-y https://doaj.org/toc/2041-1723 doi:10.1038/s41467-023-40641-y 2041-1723 https://doaj.org/article/f67ee12a2c1f46a9ab839e0bbc3d94b1 |
op_doi |
https://doi.org/10.1038/s41467-023-40641-y |
container_title |
Nature Communications |
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14 |
container_issue |
1 |
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1778131856917528576 |