Northern hemisphere storm tracks in strong AO anomaly winters
Northern Hemisphere winter 300 hPa storm tracks/baroclinic waves and their energetics during strong Arctic Oscillation (AO) anomaly events are investigated. It is shown that during strong positive AO anomaly winters, the Atlantic storm track intensifies significantly and shifts northward and far dow...
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Online Access: | https://hdl.handle.net/20.500.11897/148978 https://doi.org/10.1002/asl.186 |
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ftpekinguniv:oai:localhost:20.500.11897/148978 2023-05-15T14:53:59+02:00 Northern hemisphere storm tracks in strong AO anomaly winters Nie, Ji Wang, Peng Yang, Wenchang Tan, Benkui Nie, J (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Lab Severe Storm & Flood Disaster, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher Sci, Lab Severe Storm & Flood Disaster, Beijing 100871, Peoples R China. 2008 https://hdl.handle.net/20.500.11897/148978 https://doi.org/10.1002/asl.186 en eng atmospheric science letters ATMOSPHERIC SCIENCE LETTERS.2008,9,(3),153-159. 959315 1530-261X http://hdl.handle.net/20.500.11897/148978 doi:10.1002/asl.186 WOS:000263860700008 SCI storm tracks baroclinic wave guide Arctic Oscillation ATLANTIC OSCILLATION MIDWINTER SUPPRESSION WAVE DYNAMICS VARIABILITY ATMOSPHERE PACIFIC Journal 2008 ftpekinguniv https://doi.org/20.500.11897/148978 https://doi.org/10.1002/asl.186 2021-08-01T07:58:44Z Northern Hemisphere winter 300 hPa storm tracks/baroclinic waves and their energetics during strong Arctic Oscillation (AO) anomaly events are investigated. It is shown that during strong positive AO anomaly winters, the Atlantic storm track intensifies significantly and shifts northward and far downstream while Pacific storm track extends westward. Baroclinic waves over the Atlantic propagate along central North Atlantic during strong negative AO anomaly winters while during strong positive AO anomaly winters, waves over the Atlantic split into two branches. Distributions of the kinetic energy and energy conversions of different spatial scale over the storm track regions assume different characteristics for different AO phases. Copyright (c) 2008 Royal Meteorological Society http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000263860700008&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Geochemistry & Geophysics Meteorology & Atmospheric Sciences SCI(E) 9 ARTICLE 3 153-159 9 Journal/Newspaper Arctic North Atlantic Peking University Institutional Repository (PKU IR) Arctic Midwinter ENVELOPE(139.931,139.931,-66.690,-66.690) Pacific Atmospheric Science Letters 9 3 153 159 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
storm tracks baroclinic wave guide Arctic Oscillation ATLANTIC OSCILLATION MIDWINTER SUPPRESSION WAVE DYNAMICS VARIABILITY ATMOSPHERE PACIFIC |
spellingShingle |
storm tracks baroclinic wave guide Arctic Oscillation ATLANTIC OSCILLATION MIDWINTER SUPPRESSION WAVE DYNAMICS VARIABILITY ATMOSPHERE PACIFIC Nie, Ji Wang, Peng Yang, Wenchang Tan, Benkui Northern hemisphere storm tracks in strong AO anomaly winters |
topic_facet |
storm tracks baroclinic wave guide Arctic Oscillation ATLANTIC OSCILLATION MIDWINTER SUPPRESSION WAVE DYNAMICS VARIABILITY ATMOSPHERE PACIFIC |
description |
Northern Hemisphere winter 300 hPa storm tracks/baroclinic waves and their energetics during strong Arctic Oscillation (AO) anomaly events are investigated. It is shown that during strong positive AO anomaly winters, the Atlantic storm track intensifies significantly and shifts northward and far downstream while Pacific storm track extends westward. Baroclinic waves over the Atlantic propagate along central North Atlantic during strong negative AO anomaly winters while during strong positive AO anomaly winters, waves over the Atlantic split into two branches. Distributions of the kinetic energy and energy conversions of different spatial scale over the storm track regions assume different characteristics for different AO phases. Copyright (c) 2008 Royal Meteorological Society http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000263860700008&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Geochemistry & Geophysics Meteorology & Atmospheric Sciences SCI(E) 9 ARTICLE 3 153-159 9 |
author2 |
Nie, J (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Lab Severe Storm & Flood Disaster, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher Sci, Lab Severe Storm & Flood Disaster, Beijing 100871, Peoples R China. |
format |
Journal/Newspaper |
author |
Nie, Ji Wang, Peng Yang, Wenchang Tan, Benkui |
author_facet |
Nie, Ji Wang, Peng Yang, Wenchang Tan, Benkui |
author_sort |
Nie, Ji |
title |
Northern hemisphere storm tracks in strong AO anomaly winters |
title_short |
Northern hemisphere storm tracks in strong AO anomaly winters |
title_full |
Northern hemisphere storm tracks in strong AO anomaly winters |
title_fullStr |
Northern hemisphere storm tracks in strong AO anomaly winters |
title_full_unstemmed |
Northern hemisphere storm tracks in strong AO anomaly winters |
title_sort |
northern hemisphere storm tracks in strong ao anomaly winters |
publisher |
atmospheric science letters |
publishDate |
2008 |
url |
https://hdl.handle.net/20.500.11897/148978 https://doi.org/10.1002/asl.186 |
long_lat |
ENVELOPE(139.931,139.931,-66.690,-66.690) |
geographic |
Arctic Midwinter Pacific |
geographic_facet |
Arctic Midwinter Pacific |
genre |
Arctic North Atlantic |
genre_facet |
Arctic North Atlantic |
op_source |
SCI |
op_relation |
ATMOSPHERIC SCIENCE LETTERS.2008,9,(3),153-159. 959315 1530-261X http://hdl.handle.net/20.500.11897/148978 doi:10.1002/asl.186 WOS:000263860700008 |
op_doi |
https://doi.org/20.500.11897/148978 https://doi.org/10.1002/asl.186 |
container_title |
Atmospheric Science Letters |
container_volume |
9 |
container_issue |
3 |
container_start_page |
153 |
op_container_end_page |
159 |
_version_ |
1766325686378692608 |