역학규모축소법을 이용한 북태평양 기후변화전망

DC Field Value Language
dc.contributor.author 장찬주 -
dc.contributor.author 정춘용 -
dc.contributor.author 고철민 -
dc.date.accessioned 2020-07-16T03:51:42Z -
dc.date.available 2020-07-16T03:51:42Z -
dc.date.created 2020-02-11 -
dc.date.issued 2014-09-21 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/26028 -
dc.description.abstract This study presents preliminary results of regional climate model (RCM) development and its application to future climate change projection for the western North Pacific. The RCM consists of the Regional Ocean Modeling System (ROMS) as an oceanic component and the Weather Research Forecast (WRF) as an atmospheric component. The ocean model has horizontal resolution of 1/12 degrees, while the atmospheric model, covering the East Asia region, has horizontal resolution of 50km. As a first step for future climate projection with the RCM, we used future climate changes by CanESM2 that well reproduces the East Asian monsoon. Both ocean and atmospheric RCM projections with a pseudo global warming method show some prominent features including ocean surface warming concentrated near the Kuroshio-Oyashio front, a dipole pattern in mixed layer depth change, and an opposite trend in precipitation changes between the southern and northern region over the Korean Peninsula. We will also present detailed regional patterns in future changes compared with global model projections.ceanic component and the Weather Research Forecast (WRF) as an atmospheric component. The ocean model has horizontal resolution of 1/12 degrees, while the atmospheric model, covering the East Asia region, has horizontal resolution of 50km. As a first step for future climate projection with the RCM, we used future climate changes by CanESM2 that well reproduces the East Asian monsoon. Both ocean and atmospheric RCM projections with a pseudo global warming method show some prominent features including ocean surface warming concentrated near the Kuroshio-Oyashio front, a dipole pattern in mixed layer depth change, and an opposite trend in precipitation changes between the southern and northern region over the Korean Peninsula. We will also present detailed regional patterns in future changes compared with global model projections. -
dc.description.uri 1 -
dc.language English -
dc.publisher PICES FUTURE OSM -
dc.relation.isPartOf 2014 PICES FUTURE OPEN SCIENCE MEETING -
dc.title 역학규모축소법을 이용한 북태평양 기후변화전망 -
dc.title.alternative Climate Change Projection for the western North Pacific: Dynamical Downscaling -
dc.type Conference -
dc.citation.endPage 52 -
dc.citation.startPage 52 -
dc.citation.title 2014 PICES FUTURE OPEN SCIENCE MEETING -
dc.contributor.alternativeName 장찬주 -
dc.contributor.alternativeName 정춘용 -
dc.contributor.alternativeName 고철민 -
dc.identifier.bibliographicCitation 2014 PICES FUTURE OPEN SCIENCE MEETING, pp.52 -
dc.description.journalClass 1 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
Files in This Item:
There are no files associated with this item.

qrcode

Items in ScienceWatch@KIOST are protected by copyright, with all rights reserved, unless otherwise indicated.

Browse