A general rule for synoptic-eddy feedback onto 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.contributor.author | Park, Juhyun | - |
dc.contributor.author | Ren, Hong-Li | - |
dc.contributor.author | Kang, In-Sik | - |
dc.date.accessioned | 2020-04-20T08:25:27Z | - |
dc.date.available | 2020-04-20T08:25:27Z | - |
dc.date.created | 2020-01-28 | - |
dc.date.issued | 2010-11 | - |
dc.identifier.issn | 0930-7575 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/4019 | - |
dc.description.abstract | In this study, scale interaction between synoptic eddies and low-frequency flow is investigated. It is demonstrated here that there is a general rule, the "left-hand rule", that describes synoptic eddy feedback onto low-frequency flow. The rule is that low-frequency anomalies systematically stir and deform the transient eddies in such a way that the irrotational eddy-vorticity fluxes are directed preferentially about 90A degrees toward the left-hand side of the low-frequency flow; thus this eddy feedback plays a positive role in maintaining and prolonging low-frequency flow under the stormy atmosphere. Similarly, we show that the irrotational eddy-temperature and moisture fluxes are also directed preferentially about 90A degrees toward the left-hand side of the low-frequency flow in the northern hemisphere. The eddy-temperature fluxes and their vertical structure play a positive role in reinforcing the low-frequency flow in the low levels. The moisture fluxes play a role in enhancing low-frequency flow by providing eddy-induced moisture convergence and divergence. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | SPRINGER | - |
dc.subject | NORTH-ATLANTIC OSCILLATION | - |
dc.subject | MIDLATITUDE STORM TRACKS | - |
dc.subject | GEOPOTENTIAL HEIGHT | - |
dc.subject | ZONAL INDEX | - |
dc.subject | TELECONNECTION PATTERN | - |
dc.subject | CIRCULATION ANOMALIES | - |
dc.subject | TEMPERATURE-FIELDS | - |
dc.subject | ARCTIC OSCILLATION | - |
dc.subject | HEMISPHERE WINTER | - |
dc.subject | ANNULAR MODES | - |
dc.title | A general rule for synoptic-eddy feedback onto low-frequency flow | - |
dc.type | Article | - |
dc.citation.endPage | 1026 | - |
dc.citation.startPage | 1011 | - |
dc.citation.title | CLIMATE DYNAMICS | - |
dc.citation.volume | 35 | - |
dc.citation.number | 6 | - |
dc.contributor.alternativeName | 국종성 | - |
dc.identifier.bibliographicCitation | CLIMATE DYNAMICS, v.35, no.6, pp.1011 - 1026 | - |
dc.identifier.doi | 10.1007/s00382-009-0606-8 | - |
dc.identifier.scopusid | 2-s2.0-77955295071 | - |
dc.identifier.wosid | 000283298900007 | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.subject.keywordPlus | NORTH-ATLANTIC OSCILLATION | - |
dc.subject.keywordPlus | MIDLATITUDE STORM TRACKS | - |
dc.subject.keywordPlus | GEOPOTENTIAL HEIGHT | - |
dc.subject.keywordPlus | ZONAL INDEX | - |
dc.subject.keywordPlus | TELECONNECTION PATTERN | - |
dc.subject.keywordPlus | CIRCULATION ANOMALIES | - |
dc.subject.keywordPlus | TEMPERATURE-FIELDS | - |
dc.subject.keywordPlus | ARCTIC OSCILLATION | - |
dc.subject.keywordPlus | HEMISPHERE WINTER | - |
dc.subject.keywordPlus | ANNULAR MODES | - |
dc.relation.journalWebOfScienceCategory | Meteorology & Atmospheric Sciences | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Meteorology & Atmospheric Sciences | - |