Monthly changes in the influence of the Arctic oscillation on surface air temperature over China
Partial Least Squares Regression (PLSR) is used to study monthly changes in the influence of the Arctic Oscillation (AO) on spring, summer and autumn air temperature over China with the January 500 hPa geopotential height data from 1951 to 2004 and monthly temperature data from January to November a...
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Online Access: | https://hdl.handle.net/20.500.11897/149037 https://doi.org/10.1007/s00376-007-0799-x |
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ftpekinguniv:oai:localhost:20.500.11897/149037 2023-05-15T14:51:37+02:00 Monthly changes in the influence of the Arctic oscillation on surface air temperature over China Huang, Jiayou Tan, Benkui Suo, Lingling Hu, Yongyun Huang, JY (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. 2007 https://hdl.handle.net/20.500.11897/149037 https://doi.org/10.1007/s00376-007-0799-x en eng 大气科学进展英文版 ADVANCES IN ATMOSPHERIC SCIENCES.2007,24,(5),799-807. 965642 0256-1530 http://hdl.handle.net/20.500.11897/149037 doi:10.1007/s00376-007-0799-x WOS:000249569100005 SCI arctic oscillation temperature field monthly changes partial least squares regression ASIAN WINTER MONSOON NORTH-ATLANTIC OSCILLATION POSSIBLE IMPACTS CLIMATE-CHANGE EAST-ASIA VARIABILITY PREDICTION REGRESSION Journal 2007 ftpekinguniv https://doi.org/20.500.11897/149037 https://doi.org/10.1007/s00376-007-0799-x 2021-08-01T07:58:47Z Partial Least Squares Regression (PLSR) is used to study monthly changes in the influence of the Arctic Oscillation (AO) on spring, summer and autumn air temperature over China with the January 500 hPa geopotential height data from 1951 to 2004 and monthly temperature data from January to November at 160 stations in China. Several AO indices have been defined with the 500-hPa geopotential data and the index defined as the first principal component of the normalized geopotential data is best to be used to study the influence of the AO on SAT (surface air temperature) in China. There are three modes through which the AO in winter influences SAT in China. The influence of the AO on SAT in China changes monthly and is stronger in spring and summer than in autumn. The main influenced regions are Northeast China and the Changjiang River drainage area. Meteorology & Atmospheric Sciences SCI(E) 中国科学引文数据库(CSCD) 0 ARTICLE 5 799-807 24 Journal/Newspaper Arctic Climate change North Atlantic North Atlantic oscillation Peking University Institutional Repository (PKU IR) Arctic Advances in Atmospheric Sciences 24 5 799 807 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
arctic oscillation temperature field monthly changes partial least squares regression ASIAN WINTER MONSOON NORTH-ATLANTIC OSCILLATION POSSIBLE IMPACTS CLIMATE-CHANGE EAST-ASIA VARIABILITY PREDICTION REGRESSION |
spellingShingle |
arctic oscillation temperature field monthly changes partial least squares regression ASIAN WINTER MONSOON NORTH-ATLANTIC OSCILLATION POSSIBLE IMPACTS CLIMATE-CHANGE EAST-ASIA VARIABILITY PREDICTION REGRESSION Huang, Jiayou Tan, Benkui Suo, Lingling Hu, Yongyun Monthly changes in the influence of the Arctic oscillation on surface air temperature over China |
topic_facet |
arctic oscillation temperature field monthly changes partial least squares regression ASIAN WINTER MONSOON NORTH-ATLANTIC OSCILLATION POSSIBLE IMPACTS CLIMATE-CHANGE EAST-ASIA VARIABILITY PREDICTION REGRESSION |
description |
Partial Least Squares Regression (PLSR) is used to study monthly changes in the influence of the Arctic Oscillation (AO) on spring, summer and autumn air temperature over China with the January 500 hPa geopotential height data from 1951 to 2004 and monthly temperature data from January to November at 160 stations in China. Several AO indices have been defined with the 500-hPa geopotential data and the index defined as the first principal component of the normalized geopotential data is best to be used to study the influence of the AO on SAT (surface air temperature) in China. There are three modes through which the AO in winter influences SAT in China. The influence of the AO on SAT in China changes monthly and is stronger in spring and summer than in autumn. The main influenced regions are Northeast China and the Changjiang River drainage area. Meteorology & Atmospheric Sciences SCI(E) 中国科学引文数据库(CSCD) 0 ARTICLE 5 799-807 24 |
author2 |
Huang, JY (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. |
format |
Journal/Newspaper |
author |
Huang, Jiayou Tan, Benkui Suo, Lingling Hu, Yongyun |
author_facet |
Huang, Jiayou Tan, Benkui Suo, Lingling Hu, Yongyun |
author_sort |
Huang, Jiayou |
title |
Monthly changes in the influence of the Arctic oscillation on surface air temperature over China |
title_short |
Monthly changes in the influence of the Arctic oscillation on surface air temperature over China |
title_full |
Monthly changes in the influence of the Arctic oscillation on surface air temperature over China |
title_fullStr |
Monthly changes in the influence of the Arctic oscillation on surface air temperature over China |
title_full_unstemmed |
Monthly changes in the influence of the Arctic oscillation on surface air temperature over China |
title_sort |
monthly changes in the influence of the arctic oscillation on surface air temperature over china |
publisher |
大气科学进展英文版 |
publishDate |
2007 |
url |
https://hdl.handle.net/20.500.11897/149037 https://doi.org/10.1007/s00376-007-0799-x |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change North Atlantic North Atlantic oscillation |
genre_facet |
Arctic Climate change North Atlantic North Atlantic oscillation |
op_source |
SCI |
op_relation |
ADVANCES IN ATMOSPHERIC SCIENCES.2007,24,(5),799-807. 965642 0256-1530 http://hdl.handle.net/20.500.11897/149037 doi:10.1007/s00376-007-0799-x WOS:000249569100005 |
op_doi |
https://doi.org/20.500.11897/149037 https://doi.org/10.1007/s00376-007-0799-x |
container_title |
Advances in Atmospheric Sciences |
container_volume |
24 |
container_issue |
5 |
container_start_page |
799 |
op_container_end_page |
807 |
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1766322753785298944 |