KOPRI Repository

Reproduction of climate for the mid-Holocene over the Korean Peninsula using a high-resolution numerical model

Cited 0 time in wos
Cited 0 time in scopus

Full metadata record

DC Field Value Language
dc.contributor.authorKim, Seong-Joong-
dc.contributor.authorKim, Ji-Won-
dc.date.accessioned2018-03-29T06:02:26Z-
dc.date.available2018-03-29T06:02:26Z-
dc.date.issued2014-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/7289-
dc.description.abstractThe climate response over Korea to the change in orbital parameters for the mid-Holocene at 6000 BP is reproduced using a relatively high-resolution (about 75 km) climate model of National Center for Atmosphere Research (NCAR) Community Climate Model version 3 (CCM3). In response to the mid- Holocene orbital conditions, the surface temperature over Korea increased over the northern part and decreased over the southern part by up to about 0.5 C. The increase in surface temperature is mainly due to the increase in summer surface temperature as the earth receives more energy. Despite the reduced insolation in winter, surface temperature increased in North Korea, associated with the increase in downward long wave and turbulent heat fluxes. The cooler climate in the southern part is due to the reduced surface temperature in winter, spring, and autumn. In the mid-Holocene, precipitation decreased overall in most of Korea, except for the southern part, where it slightly increased. Associated with the reduced precipitation, the climate was overall drier in most of Korea, especially the northern part, though climate was slightly wetter in southernmost Korea, including Jeju Island. In comparison to some proxy records, the increase in surface temperature in the mid-Holocene is overall consistent. In terms of precipitation and hydrological budget, the southern part agrees with proxy evidence, but in central Korea there exists a disagreement. However, there are only limited numbers of proxy records throughout Korea. A greater number and lines of proxy evidence are required before we draw any clear conclusions regarding climate change for the mid-Holocene over Korea.-
dc.languageKorean-
dc.titleReproduction of climate for the mid-Holocene over the Korean Peninsula using a high-resolution numerical model-
dc.title.alternative고해상도 수치모형을 이용한 홀로세중기 한반도 기후복원-
dc.typeArticle-
dc.identifier.bibliographicCitationKim, Seong-Joong, Kim, Ji-Won. 2014. "Reproduction of climate for the mid-Holocene over the Korean Peninsula using a high-resolution numerical model". <em>QUATERNARY INTERNATIONAL</em>, 344(1): 86-96.-
dc.citation.titleQUATERNARY INTERNATIONAL-
dc.citation.volume344-
dc.citation.number1-
dc.identifier.doi10.1016/j.quaint.2014.04.052-
dc.citation.startPage86-
dc.citation.endPage96-
dc.description.articleClassificationSCI-
dc.description.jcrRateJCR 2012:33.72-
dc.subject.keyword기후변화-
dc.subject.keyword수치모델-
dc.subject.keyword홀로세 중기-
dc.identifier.localId2014-0157-
dc.identifier.scopusid2-s2.0-84923223552-
dc.identifier.wosid000342361800010-
Appears in Collections  
2014-2016, Investigation of Climate Change Mechanism by Observation and Simulation of Polar Climate for The Past and Present (14-16) / Kim, Seong-Joong (PE14010; PE15010; PE16010)
Files in This Item

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

Browse