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Mi-Kyung Sung

Researcher at Yonsei University

Publications -  29
Citations -  712

Mi-Kyung Sung is an academic researcher from Yonsei University. The author has contributed to research in topics: Teleconnection & North Atlantic oscillation. The author has an hindex of 15, co-authored 25 publications receiving 532 citations. Previous affiliations of Mi-Kyung Sung include Ewha Womans University & Seoul National University.

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A possible impact of the North Atlantic Oscillation on the east Asian summer monsoon precipitation

TL;DR: In this paper, a possible delayed impact of the winter North Atlantic Oscillation (NAO) on the following east Asian summer monsoon precipitation was reported. But, the correlation may be related to a wave train pattern which originates from the North Atlantic and can affect large-scale circulation and the precipitation over east Asia in early summer.
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Connection between weak stratospheric vortex events and the Pacific Decadal Oscillation

TL;DR: In this article, the authors investigate the possible impacts of the Pacific Decadal Oscillation (PDO) on the occurrence of weak stratospheric polar vortex (WSV) events in the Northern Hemisphere winter.
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Statistical relationship between two types of El Niño events and climate variation over the Korean Peninsula

TL;DR: In this article, the authors focus on statistical relationship between climate variation in Korea and the two types of El Nino, and they focus on the statistical relation between climate variables and the El-Nino events.
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Tropical influence on the North Pacific Oscillation drives winter extremes in North America

TL;DR: The authors showed that an eastward shift of the North Pacific Oscillation (NPO) in recent decades has caused its flip in phases to have more influence in causing abnormal warming and cooling over North America.
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How does the SST variability over the western North Atlantic Ocean control Arctic warming over the Barents-Kara Seas?

TL;DR: In this article, a possible cause of regional Arctic warming over the Barents-Kara Seas during early winter (October-December) is suggested, where the authors found that warmer sea surface temperature anomalies over the western North Atlantic Ocean (WNAO) modulate the transient eddies overlying the oceanic frontal region.