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: 1,929 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,363
529
37
1,929
30
37
HTML: 1,363
PDF: 529
XML: 37
Total: 1,929
BibTeX: 30
EndNote: 37
Views and downloads (calculated since 21 Jul 2022)
Cumulative views and downloads
(calculated since 21 Jul 2022)
Total article views: 1,151 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
925
201
25
1,151
26
32
HTML: 925
PDF: 201
XML: 25
Total: 1,151
BibTeX: 26
EndNote: 32
Views and downloads (calculated since 23 Feb 2023)
Cumulative views and downloads
(calculated since 23 Feb 2023)
Total article views: 778 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
438
328
12
778
4
5
HTML: 438
PDF: 328
XML: 12
Total: 778
BibTeX: 4
EndNote: 5
Views and downloads (calculated since 21 Jul 2022)
Cumulative views and downloads
(calculated since 21 Jul 2022)
Viewed (geographical distribution)
Total article views: 1,929 (including HTML, PDF, and XML)
Thereof 1,801 with geography defined
and 128 with unknown origin.
Total article views: 1,151 (including HTML, PDF, and XML)
Thereof 1,046 with geography defined
and 105 with unknown origin.
Total article views: 778 (including HTML, PDF, and XML)
Thereof 755 with geography defined
and 23 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...