Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
Bo Pang
State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
Viewed
Total article views: 3,824 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,792
960
72
3,824
95
147
HTML: 2,792
PDF: 960
XML: 72
Total: 3,824
BibTeX: 95
EndNote: 147
Views and downloads (calculated since 21 Jul 2022)
Cumulative views and downloads
(calculated since 21 Jul 2022)
Total article views: 2,806 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,275
474
57
2,806
87
137
HTML: 2,275
PDF: 474
XML: 57
Total: 2,806
BibTeX: 87
EndNote: 137
Views and downloads (calculated since 23 Feb 2023)
Cumulative views and downloads
(calculated since 23 Feb 2023)
Total article views: 1,018 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
517
486
15
1,018
8
10
HTML: 517
PDF: 486
XML: 15
Total: 1,018
BibTeX: 8
EndNote: 10
Views and downloads (calculated since 21 Jul 2022)
Cumulative views and downloads
(calculated since 21 Jul 2022)
Viewed (geographical distribution)
Total article views: 3,824 (including HTML, PDF, and XML)
Thereof 3,642 with geography defined
and 182 with unknown origin.
Total article views: 2,806 (including HTML, PDF, and XML)
Thereof 2,656 with geography defined
and 150 with unknown origin.
Total article views: 1,018 (including HTML, PDF, and XML)
Thereof 986 with geography defined
and 32 with unknown origin.
Sudden-stratospheric-warming (SSW) events can severely affect the subsequent weather at the surface. We use a large ensemble of climate model hindcasts to investigate features of the climate that make strong impacts more likely through negative NAO conditions. This allows a more robust assessment than using observations alone. Air pressure over the Arctic prior to an SSW and the zonal-mean zonal wind in the lower stratosphere have the strongest relationship with the subsequent NAO response.
Sudden-stratospheric-warming (SSW) events can severely affect the subsequent weather at the...