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South-north dipolar pattern around mid-1990s in Korean summer rainfall variability
Institution:1. National Institute of Meteorological Research, Jeju, Republic of Korea;2. Department of Global Environment, Keimyung University, Daegu, Republic of Korea;1. National Center for Agro-Meteorology, 1, Gwanak-ro, Gwanak-gu, Seoul 08826, South Korea;2. School of Informatics, Computing, and Cyber Systems, Northern Arizona University, S San Francisco St, Flagstaff, AZ 86011, USA;3. National Institute of Meteorological Research, 33, Seohobuk-ro, Seogwipo-si, Jeju 63568, South Korea;4. Department of Forest Conservation, National Institute of Forest Science, 57, Hoegi-ro, Dongdaemun-gu, Seoul 02455, South Korea;5. Interdisciplinary Program in Agricultural & Forest Meteorology/Department of Landscape Architecture & Rural Systems Engineering, Seoul National University, 1, Gwanak-ro, Gwanak-gu, Seoul 08826, South Korea;6. Institute of Green Bio Science and Technology, Seoul National University Pyeongchang Campus, 1447, Pyeongchang-daero, Deahwa-myeon, Pyeongchang 25354, South Korea;1. Earth System Research Division, National Institute of Meteorological Sciences, Korea;2. Department of Earth and Marine Science, College of Ocean Sciences, Jeju National University, Korea;1. National Institute of Meteorological Research, 16-Gil, Yeouidaebang-ro, Dongjak-gu, Seoul 156-720, Republic of Korea;2. Center for Marine Environmental Studies, Ehime University, Bunkyo-cho 2-5, Matsuyama, Ehime 790-8577, Japan;3. National Typhoon Center, 810 Seosung-ro, Seogwipo, Jeju 699-942, Republic of Korea;4. Suwon Weather Station, 149 Seoho-ro, Gwonseon-gu, Suwon, Gyeonggi-do 441-856, Republic of Korea;1. Indian Institute of Astrophysics, Bangalore, India;2. National Institute of Meteorological Sciences, Seogwipo, Jeju, South Korea;1. Washera Geospace and Radar Science Laboratory, Department of Physics, Science College, Bahir Dar University, Bahir Dar, Ethiopia;2. Department of Physics, Science College, Debre Markos University, Debre Markos, Ethiopia;3. Climate Research Division, National Institute of Meteorological Sciences (NIMS), Jeju-do, Republic of Korea;1. Applied Meteorology Research Division, National Institute of Meteorological Sciences, Jeju-do, Republic of Korea;2. Department of Civil,Environmental and Architectural Enginering, Korea University, Seoul, Republic of Korea
Abstract:From the time series of rainfall in summer (June, July and August) in South and North Koreas for recent 28 years (1981–2008), rainfall has significantly increased in South Korea while it has significantly decreased in North Korea since 1996. In particular, the decreasing trend of summer rainfall in North Korea was more conspicuous during the second Changma (late August – mid-September). This characteristic was also found in the south-north dipolar pattern based on 1996 by empirical orthogonal function analysis using summer rainfall observed in all weather observation stations in South and North Korea.The decreasing rainfall trend in North Korea was found to be associated with the weakening of convection by anomalous northeasterlies from anomalous anticyclone centered on around Baikal Lake during summer. On the other hand, the increasing rainfall trend of South Korea was associated with the strengthened anomalous cyclone in the southern region of China, which in turn strengthened anomalous southwesterlies.
Keywords:South Korea  North Korea  Summer rainfall  Second changma
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