Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate
Solar irradiance has been universally acknowledged to be dominant by quasi-decadal variability, which has been adopted frequently to investigate its effect on climate decadal variability. As one major terrestrial energy source, solar-wind energy flux into Earth's magnetosphere (E-in) exhibits d...
Published in: | National Science Review |
---|---|
Main Authors: | , , , , |
Format: | Report |
Language: | English |
Published: |
2020
|
Subjects: | |
Online Access: | http://ir.nssc.ac.cn/handle/122/7718 https://doi.org/10.1093/nsr/nwz082 |
id |
ftchinacadscnssc:oai:ir.nssc.ac.cn:122/7718 |
---|---|
record_format |
openpolar |
spelling |
ftchinacadscnssc:oai:ir.nssc.ac.cn:122/7718 2023-05-15T14:57:10+02:00 Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate WOS:000519816200024;20201408365767 He, Shengping Wang, Huijun Li, Fei Li, Hui Wang, Chi 2020 http://ir.nssc.ac.cn/handle/122/7718 https://doi.org/10.1093/nsr/nwz082 英语 eng NATIONAL SCIENCE REVIEW http://ir.nssc.ac.cn/handle/122/7718 doi:10.1093/nsr/nwz082 null solar wind winter climate interannual variability stratosphere JANUARY TEMPERATURE ARCTIC OSCILLATION CYCLE OZONE IRRADIANCE MODULATION TROPOSPHERE IMPACTS SIGNAL LINKS 期刊论文 2020 ftchinacadscnssc https://doi.org/10.1093/nsr/nwz082 2021-01-08T01:07:10Z Solar irradiance has been universally acknowledged to be dominant by quasi-decadal variability, which has been adopted frequently to investigate its effect on climate decadal variability. As one major terrestrial energy source, solar-wind energy flux into Earth's magnetosphere (E-in) exhibits dramatic interannual variation, the effect of which on Earth's climate, however, has not drawn much attention. Based on the Ein estimated by 3D magnetohydrodynamic simulations, we demonstrate a novelty that the annual mean Ein can explain up to 25% total interannual variance of the northern-hemispheric temperature in the subsequent boreal winter. The concurrent anomalous atmospheric circulation resembles the positive phase of Arctic Oscillation/North Atlantic Oscillation. The warm anomalies in the tropic stratopause and tropopause induced by increased solar-wind-magnetosphere energy persist into the subsequent winter. Due to the dominant change in the polar vortex and mid-latitude westerly in boreal winter, a 'top-down' propagation of the stationary planetary wave emerges in the Northern Hemisphere and further influences the atmospheric circulation and climate. Report Arctic North Atlantic North Atlantic oscillation National Space Science Center: NSSC OpenIR (Chinese Academy of Sciences) Arctic National Science Review 7 1 141 148 |
institution |
Open Polar |
collection |
National Space Science Center: NSSC OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchinacadscnssc |
language |
English |
topic |
solar wind winter climate interannual variability stratosphere JANUARY TEMPERATURE ARCTIC OSCILLATION CYCLE OZONE IRRADIANCE MODULATION TROPOSPHERE IMPACTS SIGNAL LINKS |
spellingShingle |
solar wind winter climate interannual variability stratosphere JANUARY TEMPERATURE ARCTIC OSCILLATION CYCLE OZONE IRRADIANCE MODULATION TROPOSPHERE IMPACTS SIGNAL LINKS He, Shengping Wang, Huijun Li, Fei Li, Hui Wang, Chi Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate |
topic_facet |
solar wind winter climate interannual variability stratosphere JANUARY TEMPERATURE ARCTIC OSCILLATION CYCLE OZONE IRRADIANCE MODULATION TROPOSPHERE IMPACTS SIGNAL LINKS |
description |
Solar irradiance has been universally acknowledged to be dominant by quasi-decadal variability, which has been adopted frequently to investigate its effect on climate decadal variability. As one major terrestrial energy source, solar-wind energy flux into Earth's magnetosphere (E-in) exhibits dramatic interannual variation, the effect of which on Earth's climate, however, has not drawn much attention. Based on the Ein estimated by 3D magnetohydrodynamic simulations, we demonstrate a novelty that the annual mean Ein can explain up to 25% total interannual variance of the northern-hemispheric temperature in the subsequent boreal winter. The concurrent anomalous atmospheric circulation resembles the positive phase of Arctic Oscillation/North Atlantic Oscillation. The warm anomalies in the tropic stratopause and tropopause induced by increased solar-wind-magnetosphere energy persist into the subsequent winter. Due to the dominant change in the polar vortex and mid-latitude westerly in boreal winter, a 'top-down' propagation of the stationary planetary wave emerges in the Northern Hemisphere and further influences the atmospheric circulation and climate. |
format |
Report |
author |
He, Shengping Wang, Huijun Li, Fei Li, Hui Wang, Chi |
author_facet |
He, Shengping Wang, Huijun Li, Fei Li, Hui Wang, Chi |
author_sort |
He, Shengping |
title |
Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate |
title_short |
Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate |
title_full |
Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate |
title_fullStr |
Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate |
title_full_unstemmed |
Solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate |
title_sort |
solar-wind-magnetosphere energy influences the interannual variability of the northern-hemispheric winter climate |
publishDate |
2020 |
url |
http://ir.nssc.ac.cn/handle/122/7718 https://doi.org/10.1093/nsr/nwz082 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic North Atlantic North Atlantic oscillation |
genre_facet |
Arctic North Atlantic North Atlantic oscillation |
op_relation |
NATIONAL SCIENCE REVIEW http://ir.nssc.ac.cn/handle/122/7718 doi:10.1093/nsr/nwz082 |
op_rights |
null |
op_doi |
https://doi.org/10.1093/nsr/nwz082 |
container_title |
National Science Review |
container_volume |
7 |
container_issue |
1 |
container_start_page |
141 |
op_container_end_page |
148 |
_version_ |
1766329257479372800 |