강한 몬순의 두가지 type에 관한 연구
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 김정은 | - |
dc.contributor.author | 홍성유 | - |
dc.contributor.author | 예상욱 | - |
dc.date.accessioned | 2020-07-17T02:51:03Z | - |
dc.date.available | 2020-07-17T02:51:03Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2007-10-27 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/30271 | - |
dc.description.abstract | A question regarding how a basin-wide warming in the Indian Ocean is associated with the subsystem of Asian summer monsoon is unanswered. We examine the characteristics of strong northeast Asian summer monsoon (NEASM) with (i.e., A-type) and without (i.e., B-type) a basin-wide warming in the Indian Ocean during the preceding winter. In case of the A-type strong El Nino-like sea surface temperature (SST) decay very rapidly from the preceding winter to the following summer, which may be due to a feedback process of warm Indian Ocean. In contrast, an El Nino-like SST during the preceding winter persistently influences into the following summer as in the B-type. Furthermore, the striking difference can be found in the atmospheric teleconnection pattern from the tropics to the midlatitude over the Indo-Pacific region, i.e., the Pacific-Japan-like pattern versus a pronounced Rossby wave train pattern. Such processes may result in somewhat different spatial structure and rainfall intensity in the two types of strong NEASM. | - |
dc.description.uri | 2 | - |
dc.language | English | - |
dc.publisher | 한국기상학회지 | - |
dc.relation.isPartOf | 한국기상학회 | - |
dc.title | 강한 몬순의 두가지 type에 관한 연구 | - |
dc.title.alternative | Two Types of strong Northeast Asian Summer Monsoon | - |
dc.type | Conference | - |
dc.citation.conferencePlace | KO | - |
dc.citation.endPage | 495 | - |
dc.citation.startPage | 494 | - |
dc.citation.title | 한국기상학회 | - |
dc.contributor.alternativeName | 예상욱 | - |
dc.identifier.bibliographicCitation | 한국기상학회, pp.494 - 495 | - |
dc.description.journalClass | 2 | - |