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전임교원이 최근 5년간 출판한 논문 중, 연도별 카테고리별 피인용 상위 1%에 달성된 논문
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SCIE Article [Excluded] Combined effect of El Nino-Southern Oscillation and Pacific Decadal Oscillation on the East Asian winter monsoon
Author	Kim, Ji-Won; Yeh, Sang-Wook; Chang, Eun-Chul
Corresponding Author Info	Prof. Yeh, Sang-Wook (해양융합공학과 예상욱 교수)
Professor
E-mail	swyeh@hanyang.ac.kr
Document Type
Source	CLIMATE DYNAMICS 2014, 42, 3-4, 957-971
Times Cited	Excluded
External Information	https://link.springer.com/article/10.1007%2Fs00382-013-1730-z
Abstract	[History] - 7월/8월 2019부로, 이 인용 빈도가 높은 논문의 인용 횟수가 분야와 출판 연도에 대해 인용 빈도가 높은 임계값을 기반으로 Geosciences 관련 학술 분야에서 상위 1%에 올랐습니다. [Abstract] Using long-term observational data and numerical model experiments, the combined effect of the El Nio-Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) on the variability of the East Asian winter monsoon is examined. In the observations, it is found that when the ENSO and PDO are in-phase combinations (i.e., El Nio/positive PDO phase and La Nia/negative PDO phase), a negative relationship between ENSO and East Asian winter monsoon is significantly intensified. In other words, when El Nio (La Nia) occurs with positive (negative) PDO phase, anomalous warm (cold) temperatures are dominant over the East Asian winter continent. On the other hand, there are no significant temperature anomalies when the ENSO and PDO are out-of-phase combinations (i.e., El Nio/negative PDO phase and La Nia/positive PDO phase). Further analyses indicate that the anticyclone over the western North Pacific including the East Asian marginal seas plays an essential role in modulating the intensity of the East Asian winter monsoon under the changes of ENSO-PDO phase relationship. Long-lasting high pressure and warm sea surface temperature anomalies during the late fall/winter and following spring over the western North Pacific, which appear as the El Nio occurs with positive PDO phase, can lead to a weakened East Asian winter monsoon by transporting warm and wet conditions into the East Asian continent through the southerly wind anomalies along the western flank of the anomalous high pressure, and vice versa as the La Nia occurs with negative PDO phase. In contrast, the anomalous high pressure over the western North Pacific does not show a prominent change under the out-of-phase combinations of ENSO and PDO. Numerical model experiments confirm the observational results, accompanying dominant warm temperature anomalies over East Asia via strong anticyclonic circulation anomalies near the Philippine Sea as the El Nio occurs with positive PDO phase, whereas such warming is weakened as the El Nio occurs with negative PDO phase. This result supports the argument that the changes in the East Asian winter monsoon intensity with ENSO are largely affected by the strength of the anticyclone over the western North Pacific, which significantly changes according to the ENSO-PDO phase relationship.
Web of Science Categories	Meteorology & Atmospheric Sciences
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