globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-15-0406.1
Scopus记录号: 2-s2.0-84957824067
论文题名:
Impact of two distinct teleconnection patterns induced by western central Pacific SST anomalies on Korean temperature variability during the early boreal summer
作者: Ham Y.-G.; Kug J.-S.; Yeh S.-W.; Kwon M.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2016
卷: 29, 期:2
起始页码: 743
结束页码: 759
语种: 英语
Scopus关键词: Atmospheric pressure ; Atmospheric temperature ; Atmospheric thermodynamics ; Climate change ; Climatology ; Surface waters ; Atmosphere-ocean interactions ; Climate variability ; Interannual variability ; Intraseasonal variability ; Southern oscillation ; Tropical variability ; Variability ; Oceanography ; air-sea interaction ; annual variation ; atmosphere-ocean system ; atmospheric circulation ; sea surface temperature ; summer ; teleconnection ; temperature profile ; Korea ; Pacific Ocean ; Pacific Ocean (Central) ; Citrus maxima
英文摘要: This study investigates the impact of western central Pacific sea surface temperatures (SSTs) on the temperature variability over the Korea Peninsula during the early boreal summer season. The authors found a significant positive correlation between June temperature anomalies across the Korea Peninsula and a horseshoe pattern of ENSO-related SST anomalies in the western central Pacific during May. While this SST pattern is relatively stationary throughout the boreal summer, the SST-driven atmospheric teleconnection exhibits dramatic subseasonal changes. During May, positive precipitation anomalies caused by SST warming in the northern central Pacific (NCP; 20°-30°N, 160°E-160°W) induce a wave train extending in a northwest-southeast direction.During June, while this wave train pattern is weakened, a Pacific-Japan (PJ) pattern is formed by positive precipitation anomalies over the off-equatorial western Pacific (off-WP). Even though dramatic subseasonal changes exist in the teleconnection patterns, both patterns contribute to temperature warming over Korea. It is shown that the subseasonal change in the atmospheric teleconnection is caused by changes in climatological precipitation. During May, significant climatological precipitation related to the pre-mei-yu and pre-baiu fronts occurs over the NCP. These wet background conditions provide a favorable environment for anomalous convection over the NCP but not over the off-equatorial western Pacific. On the other hand, during June, convective activities over the off-WP result in the formation of a PJ pattern, enhanced by an increase in climatological precipitation associated with the activation of thewestern North Pacific (WNP)monsoon. These results indicate that climatological conditions play an important role in the formation of atmospheric teleconnection linking Pacific and East Asian climates. © 2016 American Meteorological Society.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/50144
Appears in Collections:气候变化事实与影响

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作者单位: Faculty of Earth Systems and Environmental Sciences, Chonnam Natio.nal University, Gwangju, South Korea; School of Earth Science and Engineering, Pohang University of Science and Technology, Pohang, South Korea; Department of Marine Science and Convergent Technology, Hanyang University, Education Research Industry Cluster at Ansan, Ansan, South Korea; Korea Institute of Ocean Science and Technology, Ansan, South Korea

Recommended Citation:
Ham Y.-G.,Kug J.-S.,Yeh S.-W.,et al. Impact of two distinct teleconnection patterns induced by western central Pacific SST anomalies on Korean temperature variability during the early boreal summer[J]. Journal of Climate,2016-01-01,29(2)
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