A kinematic mechanism for positive feedback between synoptic eddies
[1] A kinematic mechanism for the positive feedback between the North Atlantic Oscillation (NAO) and synoptic eddies are depicted based on observational data analyses. Using three-point rescaled covariance statistics of bandpass-filtered (2–8 days) synoptic eddy fields, we examined observed eddy str...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.367.4134 2023-05-15T17:31:25+02:00 A kinematic mechanism for positive feedback between synoptic eddies Nao Hong-li Ren Fei-fei Jin Jong-seong Kug Jing-xia Zhao Juhyun Park The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.367.4134 http://www.soest.hawaii.edu/met/Faculty/jff/2009_02 A Kinematic Mechanism for Positive Feedback between Synoptic Eddies and NAO.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.367.4134 http://www.soest.hawaii.edu/met/Faculty/jff/2009_02 A Kinematic Mechanism for Positive Feedback between Synoptic Eddies and NAO.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.soest.hawaii.edu/met/Faculty/jff/2009_02 A Kinematic Mechanism for Positive Feedback between Synoptic Eddies and NAO.pdf text ftciteseerx 2016-01-08T01:06:38Z [1] A kinematic mechanism for the positive feedback between the North Atlantic Oscillation (NAO) and synoptic eddies are depicted based on observational data analyses. Using three-point rescaled covariance statistics of bandpass-filtered (2–8 days) synoptic eddy fields, we examined observed eddy structure changes associated with wintermean NAO anomalous flow. It is demonstrated that the NAO flow anomalies systematically deform the structures of recurring synoptic eddies to generate seasonal-mean eddyvorticity flux anomalies predominately directed to the lefthand side of the NAO flow anomalies. These anomalous eddy-vorticity fluxes converge into the cyclonic center and diverge from the anticyclonic center of the anomalous NAO flow, and thus enhance the NAO flow. Citation: Ren, H.-L. Text North Atlantic North Atlantic oscillation ren Unknown |
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English |
description |
[1] A kinematic mechanism for the positive feedback between the North Atlantic Oscillation (NAO) and synoptic eddies are depicted based on observational data analyses. Using three-point rescaled covariance statistics of bandpass-filtered (2–8 days) synoptic eddy fields, we examined observed eddy structure changes associated with wintermean NAO anomalous flow. It is demonstrated that the NAO flow anomalies systematically deform the structures of recurring synoptic eddies to generate seasonal-mean eddyvorticity flux anomalies predominately directed to the lefthand side of the NAO flow anomalies. These anomalous eddy-vorticity fluxes converge into the cyclonic center and diverge from the anticyclonic center of the anomalous NAO flow, and thus enhance the NAO flow. Citation: Ren, H.-L. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Nao Hong-li Ren Fei-fei Jin Jong-seong Kug Jing-xia Zhao Juhyun Park |
spellingShingle |
Nao Hong-li Ren Fei-fei Jin Jong-seong Kug Jing-xia Zhao Juhyun Park A kinematic mechanism for positive feedback between synoptic eddies |
author_facet |
Nao Hong-li Ren Fei-fei Jin Jong-seong Kug Jing-xia Zhao Juhyun Park |
author_sort |
Nao |
title |
A kinematic mechanism for positive feedback between synoptic eddies |
title_short |
A kinematic mechanism for positive feedback between synoptic eddies |
title_full |
A kinematic mechanism for positive feedback between synoptic eddies |
title_fullStr |
A kinematic mechanism for positive feedback between synoptic eddies |
title_full_unstemmed |
A kinematic mechanism for positive feedback between synoptic eddies |
title_sort |
kinematic mechanism for positive feedback between synoptic eddies |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.367.4134 http://www.soest.hawaii.edu/met/Faculty/jff/2009_02 A Kinematic Mechanism for Positive Feedback between Synoptic Eddies and NAO.pdf |
genre |
North Atlantic North Atlantic oscillation ren |
genre_facet |
North Atlantic North Atlantic oscillation ren |
op_source |
http://www.soest.hawaii.edu/met/Faculty/jff/2009_02 A Kinematic Mechanism for Positive Feedback between Synoptic Eddies and NAO.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.367.4134 http://www.soest.hawaii.edu/met/Faculty/jff/2009_02 A Kinematic Mechanism for Positive Feedback between Synoptic Eddies and NAO.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766128967272628224 |