극지역 온도 상승 및 강수 증가에 대한 스톰의 역할
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | 국종성 | - |
| dc.contributor.author | 최다희 | - |
| dc.contributor.author | F.-F. Jin | - |
| dc.contributor.author | 권원태 | - |
| dc.contributor.author | H.-L Ren | - |
| dc.date.accessioned | 2020-07-16T22:50:08Z | - |
| dc.date.available | 2020-07-16T22:50:08Z | - |
| dc.date.created | 2020-02-11 | - |
| dc.date.issued | 2009-06-15 | - |
| dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/29421 | - |
| dc.description.abstract | The climate responses to the anthropogenic greenhouse gas forcing are spatially non-uniform and the underlying dynamics of these responses remain unclear. We find that poleward shift of jet streams and associated weather storm feedback play a critical role in enhancing polar warming and moistening. Storm feedback in this case tends to follow a simple rule: providing anomalous heat and moisture fluxes to the left of anomalous jet stream flow. This rule can be used for understanding dynamical climate responses to the anthropogenic forcing. | - |
| dc.description.uri | 1 | - |
| dc.language | English | - |
| dc.publisher | KORDI | - |
| dc.relation.isPartOf | International Workshop on Global Climate Monitoring and Modeling | - |
| dc.title | 극지역 온도 상승 및 강수 증가에 대한 스톰의 역할 | - |
| dc.title.alternative | Storm-induced polar warming and moistening under anthropogenic forcing | - |
| dc.type | Conference | - |
| dc.citation.conferencePlace | KO | - |
| dc.citation.endPage | 48 | - |
| dc.citation.startPage | 48 | - |
| dc.citation.title | International Workshop on Global Climate Monitoring and Modeling | - |
| dc.contributor.alternativeName | 국종성 | - |
| dc.identifier.bibliographicCitation | International Workshop on Global Climate Monitoring and Modeling, pp.48 | - |
| dc.description.journalClass | 1 | - |
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