Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon
Here we present a study of the relationship between July-August (JA) mean climate over China, which is strongly linked to the East Asian summer monsoon (EASM), and the summer (JA) North Atlantic Oscillation (SNAO). The variations of temperature, precipitation, and cloud cover related to the SNAO wer...
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Language: | English |
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Online Access: | http://ir.ieecas.cn/handle/361006/10348 https://doi.org/10.1029/2010JD015235 |
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ftchinacascieeca:oai:ir.ieecas.cn:361006/10348 2023-06-11T04:14:20+02:00 Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon Linderholm, HW (Linderholm, Hans W.)1 Ou, TH (Ou, Tinghai)1,2 Jeong, JH (Jeong, Jee-Hoon)1 Folland, CK (Folland, Chris K.)3 Gong, DY (Gong, Daoyi)4 Liu, HB (Liu, Hongbin)5 Liu, Y (Liu, Yu)6 Chen, DL (Chen, Deliang)1 2011-07-13 http://ir.ieecas.cn/handle/361006/10348 https://doi.org/10.1029/2010JD015235 英语 eng JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES http://ir.ieecas.cn/handle/361006/10348 doi:10.1029/2010JD015235 null 期刊论文 2011 ftchinacascieeca https://doi.org/10.1029/2010JD015235 2023-05-08T13:23:37Z Here we present a study of the relationship between July-August (JA) mean climate over China, which is strongly linked to the East Asian summer monsoon (EASM), and the summer (JA) North Atlantic Oscillation (SNAO). The variations of temperature, precipitation, and cloud cover related to the SNAO were analyzed for the period 1951-2002 using gridded data sets as well as instrumental data from 160 stations in China. It was shown that the major patterns of summer climate over China are highly connected with the interannual variation of the SNAO, supporting a teleconnection between the North Atlantic region and East Asia. Based on the analyses of the daily and monthly reanalysis data sets, we propose possible mechanisms of this teleconnection. Changes in the position of the North Atlantic storm tracks and transient eddy activity associated with the positive (negative) SNAO phase contribute downstream to negative (positive) sea level pressure anomalies in northeastern East Asia. In negative SNAO years, a stationary wave pattern is excited from the southern SNAO center over northwestern Europe to northeastern East Asia. However, during positive SNAO years, a stationary wave pattern is excited extending from the SNAO center across the central Eurasian continent at around 40 degrees N and downstream to the southeast. This may explain a connection between the positive SNAO and atmospheric circulation in middle and southeastern China. Report North Atlantic North Atlantic oscillation Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) Journal of Geophysical Research 116 D13 |
institution |
Open Polar |
collection |
Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchinacascieeca |
language |
English |
description |
Here we present a study of the relationship between July-August (JA) mean climate over China, which is strongly linked to the East Asian summer monsoon (EASM), and the summer (JA) North Atlantic Oscillation (SNAO). The variations of temperature, precipitation, and cloud cover related to the SNAO were analyzed for the period 1951-2002 using gridded data sets as well as instrumental data from 160 stations in China. It was shown that the major patterns of summer climate over China are highly connected with the interannual variation of the SNAO, supporting a teleconnection between the North Atlantic region and East Asia. Based on the analyses of the daily and monthly reanalysis data sets, we propose possible mechanisms of this teleconnection. Changes in the position of the North Atlantic storm tracks and transient eddy activity associated with the positive (negative) SNAO phase contribute downstream to negative (positive) sea level pressure anomalies in northeastern East Asia. In negative SNAO years, a stationary wave pattern is excited from the southern SNAO center over northwestern Europe to northeastern East Asia. However, during positive SNAO years, a stationary wave pattern is excited extending from the SNAO center across the central Eurasian continent at around 40 degrees N and downstream to the southeast. This may explain a connection between the positive SNAO and atmospheric circulation in middle and southeastern China. |
format |
Report |
author |
Linderholm, HW (Linderholm, Hans W.)1 Ou, TH (Ou, Tinghai)1,2 Jeong, JH (Jeong, Jee-Hoon)1 Folland, CK (Folland, Chris K.)3 Gong, DY (Gong, Daoyi)4 Liu, HB (Liu, Hongbin)5 Liu, Y (Liu, Yu)6 Chen, DL (Chen, Deliang)1 |
spellingShingle |
Linderholm, HW (Linderholm, Hans W.)1 Ou, TH (Ou, Tinghai)1,2 Jeong, JH (Jeong, Jee-Hoon)1 Folland, CK (Folland, Chris K.)3 Gong, DY (Gong, Daoyi)4 Liu, HB (Liu, Hongbin)5 Liu, Y (Liu, Yu)6 Chen, DL (Chen, Deliang)1 Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon |
author_facet |
Linderholm, HW (Linderholm, Hans W.)1 Ou, TH (Ou, Tinghai)1,2 Jeong, JH (Jeong, Jee-Hoon)1 Folland, CK (Folland, Chris K.)3 Gong, DY (Gong, Daoyi)4 Liu, HB (Liu, Hongbin)5 Liu, Y (Liu, Yu)6 Chen, DL (Chen, Deliang)1 |
author_sort |
Linderholm, HW (Linderholm, Hans W.)1 |
title |
Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon |
title_short |
Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon |
title_full |
Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon |
title_fullStr |
Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon |
title_full_unstemmed |
Interannual teleconnections between the summer North Atlantic Oscillation and the East Asian summer monsoon |
title_sort |
interannual teleconnections between the summer north atlantic oscillation and the east asian summer monsoon |
publishDate |
2011 |
url |
http://ir.ieecas.cn/handle/361006/10348 https://doi.org/10.1029/2010JD015235 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES http://ir.ieecas.cn/handle/361006/10348 doi:10.1029/2010JD015235 |
op_rights |
null |
op_doi |
https://doi.org/10.1029/2010JD015235 |
container_title |
Journal of Geophysical Research |
container_volume |
116 |
container_issue |
D13 |
_version_ |
1768392278340009984 |