Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report
Physics|Updated:2023-05-19
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Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report
Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report
海洋湖沼学报(英文)2018年36卷第3期 页码:601-611
Affiliations:
Physical Oceanography Laboratory/CIMST, Ocean University of China, and Qingdao National Laboratory for Marine Science and Technology, Qingdao 266003, China
Author bio:
CHEN Zheng, chenzhengouc@163.com
Funds:
the China National Global Change Major Research Project(2013CB956201);the National Science Foundation of China (NSFC) Key Project(41130859);the NSFC(41506009);the National Natural Science Foundation of China(41521091);the National Natural Science Foundation of China(41490643)
陈峥, 甘波澜, 吴立新. Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report[J]. 海洋湖沼学报(英文), 2018,36(3):601-611.
Zheng CHEN, Bolan GAN, Lixin WU. Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 601-611.
陈峥, 甘波澜, 吴立新. Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report[J]. 海洋湖沼学报(英文), 2018,36(3):601-611. DOI: 10.1007/s00343-018-7022-z.
Zheng CHEN, Bolan GAN, Lixin WU. Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report[J]. Chinese Journal of Oceanology and Limnology, 2018, 36(3): 601-611. DOI: 10.1007/s00343-018-7022-z.
Response of the North Pacific Oscillation to global warming in the models of the Intergovernmental Panel on Climate Change Fourth Assessment Report
摘要
Abstract
Based on 22 of the climate models from phase 3 of the Coupled Model Intercomparison Project
we investigate the ability of the models to reproduce the spatiotemporal features of the wintertime North Pacific Oscillation (NPO)
which is the second most important factor determining the wintertime sea level pressure field in simulations of the pre-industrial control climate
and evaluate the NPO response to the future most reasonable global warming scenario (the A1B scenario). We reveal that while most models simulate the geographic distribution and amplitude of the NPO pattern satisfactorily
only 13 models capture both features well. However
the temporal variability of the simulated NPO could not be significantly correlated with the observations. Further analysis indicates the weakened NPO intensity for a scenario of strong global warming is attributable to the reduced lower-tropospheric baroclinicity at mid-latitudes
which is anticipated to disrupt large-scale and low-frequency atmospheric variability
resulting in the diminished transfer of energy to the NPO
together with its northward shift.
关键词
Keywords
references
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