[E] Poster
A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment
Tue. May 28, 2019 10:45 AM - 12:15 PM Poster Hall (International Exhibition Hall8, Makuhari Messe)
convener:Hiroaki Miura(The University of Tokyo), Atsushi Hamada(University of Toyama), Satoru Yokoi(Japan Agency for Marine-Earth Science and Technology), Masaki Satoh(Atmosphere and Ocean Research Institute, The University of Tokyo)
Water vapor plays a significant role in regulating the global atmospheric circulation, especially in the troposphere. The overturning circulation is directly driven by the longwave radiative cooling of water vapor and the latent heating/cooling through microphysical processes to balance it. This global circulation is composed of diverse atmospheric phenomena with various spatial and temporal scales. Developments of some significant turbulent motions such as 3D isotropic turbulence in clouds, stratocumulus and cumulus convection, squall lines and tropical cyclones, and the Madden-Julian oscillation, are essentially associated with moisture anomaly in each scale. Moisture is accumulated relatively slowly in larger horizontal scales, but is consumed relatively quickly in smaller ones. This significant scale gaps between the accumulation and consumption may be one of the causes of the long-lasting difficulty in developing the theory of the moist atmosphere. The aim of this session is to share the recent researches about the relationships between moisture and organized cloud systems in wider spatial and temporal scales to enhance collaborations between modeling, observational, and theoretical approaches in tackling this challenging task. Research results relating to the Years of the Maritime Continent (YMC) and Radiative-Convective Equilibrium Model Intercomparison Project (RCEMPI) are welcome.
*Ong Chia Rui1, Hiroaki Miura1 (1.The University of Tokyo)
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*Jing LiU1, Yushu Zhou2, Lianmei Yang1 (1.Institute of Desert Meteorology,CMA, 2.Institute of Atmospheric Physics,CAS)
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*Jou Ping Hou1, Bo-Shiou Wei1, Li-Zhen Su1 (1.Chung Cheng Institute of Technology)
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*Yong Liu1 (1.Institute of Atmospheric Physics, Beijing , China)
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*Xinyue Wang1, Hironobu Iwabuchi1 (1.Tohoku Univ.)
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*Madam Taqiyya Maulana1, Takeshi Yamazaki1 (1.Tohoku University)
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*Lianmei Yang1, Xuefeng Guan1 (1.Institute of Desert Meteorology, China Meteorological Administration,)
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*Kanta Nakae1, Masaki Satoh1, Daisuke Takasuka1 (1.Atmosphere and Ocean Research Institute, The University of Tokyo)
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*Takuya Jinno1 (1.Graduate School of Science, The University of Tokyo)
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*Noriyuki Nishi1, Atsushi Hamada4, Yohei Yamada2, Tomoe Nasuno2, Reona Satoh5, Masaki Satoh3 (1.Faculty of Science, Fukuoka Universtiy, 2.JAMSTEC, 3.AORI, University of Tokyo, 4.Graduate School of Science and Engineering for Education, University of Toyama, 5.Graduate School of Science, Fukuoka University)
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*Woosub Roh1, Tatsuya Seiki2, Masaki Satoh1, Tempei Hashino3 (1.AORI, the university of Tokyo, 2.JAMSTEC, 3.Kochi university of technology )
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*Tomoki Ohno1, Masaki Satoh2 (1.Japan Agency for Marine-Earth Science and Technology, 2.Atmosphere and Ocean Research Institute, The University of Tokyo)
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*bo hai Wang1, hua Zhang2 (1.Institute of Atmospheric Physics, Chinese Academy of Sciences, 2.State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences)
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