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DC Field | Value | Language |
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dc.citation.endPage | 1499 | - |
dc.citation.number | 7-8 | - |
dc.citation.startPage | 1483 | - |
dc.citation.title | CLIMATE DYNAMICS | - |
dc.citation.volume | 37 | - |
dc.contributor.author | Park, Myung-Sook | - |
dc.contributor.author | Ho, Chang-Hoi | - |
dc.contributor.author | Kim, Jinwon | - |
dc.contributor.author | Elsberry, Russell L. | - |
dc.date.accessioned | 2023-12-22T05:43:07Z | - |
dc.date.available | 2023-12-22T05:43:07Z | - |
dc.date.created | 2015-11-19 | - |
dc.date.issued | 2011-10 | - |
dc.description.abstract | The morning diurnal precipitation maximum over the coastal sea upstream of the Philippines during intraseasonal westerly wind bursts is examined from observations and numerical model simulations. A well-defined case of precipitation and large-scale circulation over the coastal sea west of the Philippines during 17-27 June 2004 is selected as a representative case. The hypothesis is that the mesoscale diurnal circulation over the Philippines and a large-scale diurnal circulation that is induced by large-scale differential heating over Asian continent and the surrounding ocean interact to produce the offshore precipitation maximum during the morning. Three-hourly combined satellite microwave and infrared rainfall retrievals define the morning rainfall peak during this period, and then later the stratiform rain area extends toward the open sea. A control numerical simulation in which a grid-nudging four-dimensional data assimilation (FDDA) is applied to force the large-scale diurnal circulation represents reasonably well the morning rainfall maximum. An enhanced low-level convergence similar to observations is simulated due to the interaction of the local- and large-scale diurnal circulations. The essential role of the local-scale diurnal circulation is illustrated in a sensitivity test in which the solar zenith angle is fixed at 7 am to suppress this diurnal circulation. The implication for climate diagnosis or modeling of such upstream coastal sea precipitation maxima is that the diurnal variations of both the local- and the large-scale circulations must be taken into consideration | - |
dc.identifier.bibliographicCitation | CLIMATE DYNAMICS, v.37, no.7-8, pp.1483 - 1499 | - |
dc.identifier.doi | 10.1007/s00382-010-0922-z | - |
dc.identifier.issn | 0930-7575 | - |
dc.identifier.scopusid | 2-s2.0-80053305665 | - |
dc.identifier.uri | https://scholarworks.unist.ac.kr/handle/201301/17815 | - |
dc.identifier.url | http://link.springer.com/article/10.1007%2Fs00382-010-0922-z | - |
dc.identifier.wosid | 000295522600012 | - |
dc.language | 영어 | - |
dc.publisher | SPRINGER | - |
dc.title | Diurnal circulations and their multi-scale interaction leading to rainfall over the South China Sea upstream of the Philippines during intraseasonal monsoon westerly wind bursts | - |
dc.type | Article | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.subject.keywordAuthor | Diurnal rainfall | - |
dc.subject.keywordAuthor | Westerly wind bursts | - |
dc.subject.keywordAuthor | Intra-seasonal rainfall variability | - |
dc.subject.keywordAuthor | South China Sea | - |
dc.subject.keywordPlus | ASIAN SUMMER MONSOON | - |
dc.subject.keywordPlus | MESOSCALE CONVECTIVE SYSTEMS | - |
dc.subject.keywordPlus | TRMM-PR | - |
dc.subject.keywordPlus | PRECIPITATION | - |
dc.subject.keywordPlus | CYCLE | - |
dc.subject.keywordPlus | TROPICS | - |
dc.subject.keywordPlus | MODEL | - |
dc.subject.keywordPlus | VICINITY | - |
dc.subject.keywordPlus | PACIFIC | - |
dc.subject.keywordPlus | VARIABILITY | - |
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