2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts
The North Pacific Oscillation (NPO) in sea level pressure and its upper-air geopotential height signature, the west Pacific (WP) teleconnection pattern, constitute a prominent mode of winter midlatitude variability, the NPO/WP. Its mature-phase expression is identified from principal component analy...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.362.5264 2023-05-15T15:00:52+02:00 2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts Megan E. Linkin Sumant Nigam The Pennsylvania State University CiteSeerX Archives 1979 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.5264 http://www.atmos.umd.edu/~nigam/Linkin-Nigam.JCLIM.May.2008.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.5264 http://www.atmos.umd.edu/~nigam/Linkin-Nigam.JCLIM.May.2008.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmos.umd.edu/~nigam/Linkin-Nigam.JCLIM.May.2008.pdf text 1979 ftciteseerx 2016-01-08T00:53:58Z The North Pacific Oscillation (NPO) in sea level pressure and its upper-air geopotential height signature, the west Pacific (WP) teleconnection pattern, constitute a prominent mode of winter midlatitude variability, the NPO/WP. Its mature-phase expression is identified from principal component analysis of monthly sea level pressure variability as the second leading mode just behind the Pacific–North American variability pattern. NPO/WP variability, primarily on subseasonal time scales, is characterized by a large-scale meridional dipole in SLP and geopotential height over the Pacific and is linked to meridional movements of the Asian–Pacific jet and Pacific storm track modulation. The hemispheric height anomalies at upper levels resemble the climatological stationary wave pattern attributed to transient eddy forcing. The NPO/WP divergent circulation is thermal wind restoring, pointing to independent forcing of jet fluctuations. Intercomparison of sea level pressure, geopotential height, and zonal wind anomaly structure reveals that NPO/WP is a basin analog of the NAO, which is not surprising given strong links to storm track variability in both cases. The NPO/WP variability is influential: its impact on Alaskan, Pacific Northwest, Canadian, and U.S. winter surface air temperatures is substantial—more than that of PNA or ENSO. It is likewise more influential on the Pacific Northwest, western Mexico, and south-central Great Plains winter precipitation. Finally, and perhaps, most importantly, NPO/WP is strongly linked to marginal ice zone variability of the Arctic seas with an influence that surpasses that of other Pacific modes. Although NPO/WP variability and impacts have not been as extensively analyzed as its Pacific cousins (PNA, ENSO), it is shown to be more consequential for Arctic sea ice and North American winter hydroclimate. 1. Text Arctic Sea ice Unknown Arctic Pacific |
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Unknown |
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ftciteseerx |
language |
English |
description |
The North Pacific Oscillation (NPO) in sea level pressure and its upper-air geopotential height signature, the west Pacific (WP) teleconnection pattern, constitute a prominent mode of winter midlatitude variability, the NPO/WP. Its mature-phase expression is identified from principal component analysis of monthly sea level pressure variability as the second leading mode just behind the Pacific–North American variability pattern. NPO/WP variability, primarily on subseasonal time scales, is characterized by a large-scale meridional dipole in SLP and geopotential height over the Pacific and is linked to meridional movements of the Asian–Pacific jet and Pacific storm track modulation. The hemispheric height anomalies at upper levels resemble the climatological stationary wave pattern attributed to transient eddy forcing. The NPO/WP divergent circulation is thermal wind restoring, pointing to independent forcing of jet fluctuations. Intercomparison of sea level pressure, geopotential height, and zonal wind anomaly structure reveals that NPO/WP is a basin analog of the NAO, which is not surprising given strong links to storm track variability in both cases. The NPO/WP variability is influential: its impact on Alaskan, Pacific Northwest, Canadian, and U.S. winter surface air temperatures is substantial—more than that of PNA or ENSO. It is likewise more influential on the Pacific Northwest, western Mexico, and south-central Great Plains winter precipitation. Finally, and perhaps, most importantly, NPO/WP is strongly linked to marginal ice zone variability of the Arctic seas with an influence that surpasses that of other Pacific modes. Although NPO/WP variability and impacts have not been as extensively analyzed as its Pacific cousins (PNA, ENSO), it is shown to be more consequential for Arctic sea ice and North American winter hydroclimate. 1. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Megan E. Linkin Sumant Nigam |
spellingShingle |
Megan E. Linkin Sumant Nigam 2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts |
author_facet |
Megan E. Linkin Sumant Nigam |
author_sort |
Megan E. Linkin |
title |
2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts |
title_short |
2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts |
title_full |
2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts |
title_fullStr |
2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts |
title_full_unstemmed |
2008), The North Pacific Oscillation-West Pacific teleconnections pattern: Mature-phase structure and winter impacts |
title_sort |
2008), the north pacific oscillation-west pacific teleconnections pattern: mature-phase structure and winter impacts |
publishDate |
1979 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.5264 http://www.atmos.umd.edu/~nigam/Linkin-Nigam.JCLIM.May.2008.pdf |
geographic |
Arctic Pacific |
geographic_facet |
Arctic Pacific |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_source |
http://www.atmos.umd.edu/~nigam/Linkin-Nigam.JCLIM.May.2008.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.5264 http://www.atmos.umd.edu/~nigam/Linkin-Nigam.JCLIM.May.2008.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766332911449014272 |