Left-hand rule for synoptic eddy feedback on low-frequency flow SCIE SCOPUS
DC Field | Value | Language |
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dc.contributor.author | Kug, Jong-Seong | - |
dc.contributor.author | Jin, Fei-Fei | - |
dc.date.accessioned | 2020-04-20T09:55:09Z | - |
dc.date.available | 2020-04-20T09:55:09Z | - |
dc.date.created | 2020-01-28 | - |
dc.date.issued | 2009-03-13 | - |
dc.identifier.issn | 0094-8276 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/4316 | - |
dc.description.abstract | In this study, scale interaction between synoptic eddies and low-frequency flow is investigated. The synoptic eddy feedback is a key process in sustaining the low-frequency flow. We show clear evidence using NCEP reanalysis data that there is a general underlying rule-the "left-hand rule'', governing the synoptic eddy feedback onto low-frequency flow. This rule states that eddy-vorticity fluxes are directed preferentially about 90 degrees toward their left-hand side, so that they converge into cyclonic flow and diverge from anticyclonic flow. Therefore, the eddy vorticity flux plays a positive role in reinforcing low-frequency flow. Citation: Kug, J.-S., and F.-F. Jin (2009), Left-hand rule for synoptic eddy feedback on low-frequency flow, Geophys. Res. Lett., 36, L05709, doi:10.1029/2008GL036435. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | AMER GEOPHYSICAL UNION | - |
dc.subject | MIDLATITUDE STORM TRACKS | - |
dc.subject | ZONAL INDEX | - |
dc.subject | TELECONNECTION PATTERN | - |
dc.subject | CIRCULATION ANOMALIES | - |
dc.subject | SIMPLE-MODEL | - |
dc.subject | DYNAMICS | - |
dc.subject | VARIABILITY | - |
dc.subject | ORGANIZATION | - |
dc.subject | HEMISPHERE | - |
dc.subject | ATMOSPHERE | - |
dc.title | Left-hand rule for synoptic eddy feedback on low-frequency flow | - |
dc.type | Article | - |
dc.citation.title | GEOPHYSICAL RESEARCH LETTERS | - |
dc.citation.volume | 36 | - |
dc.contributor.alternativeName | 국종성 | - |
dc.identifier.bibliographicCitation | GEOPHYSICAL RESEARCH LETTERS, v.36 | - |
dc.identifier.doi | 10.1029/2008GL036435 | - |
dc.identifier.scopusid | 2-s2.0-65649113603 | - |
dc.identifier.wosid | 000264222300002 | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.subject.keywordPlus | MIDLATITUDE STORM TRACKS | - |
dc.subject.keywordPlus | ZONAL INDEX | - |
dc.subject.keywordPlus | TELECONNECTION PATTERN | - |
dc.subject.keywordPlus | CIRCULATION ANOMALIES | - |
dc.subject.keywordPlus | SIMPLE-MODEL | - |
dc.subject.keywordPlus | DYNAMICS | - |
dc.subject.keywordPlus | VARIABILITY | - |
dc.subject.keywordPlus | ORGANIZATION | - |
dc.subject.keywordPlus | HEMISPHERE | - |
dc.subject.keywordPlus | ATMOSPHERE | - |
dc.relation.journalWebOfScienceCategory | Geosciences, Multidisciplinary | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Geology | - |