스톰 피드백에 대한 왼손의 법칙
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | 국종성 | - |
| dc.contributor.author | F.-F. Jin | - |
| dc.contributor.author | 박주현 | - |
| dc.contributor.author | H.-L. Ren | - |
| dc.date.accessioned | 2020-07-16T23:30:45Z | - |
| dc.date.available | 2020-07-16T23:30:45Z | - |
| dc.date.created | 2020-02-11 | - |
| dc.date.issued | 2009-04-24 | - |
| dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/29551 | - |
| dc.description.abstract | This left-hand rule of eddy-vorticity fluxes relative to low-frequency flow indicates positive feedback of synoptic eddy forcing on the low-frequency flow. If the low-frequency flow is cyclonic (anticyclonic), the eddy vorticity fluxeswill converge (diverge) to the center of the cyclonic (anticyclonic) flow based on the left-hand rule, indicating that the vorticity fields of low-frequency flow are reinforced. This relation confirms the results of the pioneer work by Lau [1988]. Note that the eddy feedback will be maximized when the eddy vorticity flux is perpendicular to the left-hand side of low-frequency flow. Therefore, this positive feedback plays an important role in the dominance of climatic modes, such NAO (North Atlantic Oscillation) and PNA (Pacific -North America) patterns. | - |
| dc.description.uri | 2 | - |
| dc.language | English | - |
| dc.publisher | 한국기상학회 | - |
| dc.relation.isPartOf | 봄철 한국기상학회 | - |
| dc.title | 스톰 피드백에 대한 왼손의 법칙 | - |
| dc.title.alternative | Left-hand Rule for Synoptic Eddy Feedback on Low-frequency Flow | - |
| dc.type | Conference | - |
| dc.citation.conferencePlace | KO | - |
| dc.citation.endPage | 151 | - |
| dc.citation.startPage | 150 | - |
| dc.citation.title | 봄철 한국기상학회 | - |
| dc.contributor.alternativeName | 국종성 | - |
| dc.identifier.bibliographicCitation | 봄철 한국기상학회, pp.150 - 151 | - |
| dc.description.journalClass | 2 | - |
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