Formation mechanism of Asian Monsoon and its variation

亚洲季风的形成机制及其变化

• 批准号: 09041198
• 负责人: FUKUSHIMA Yoshihiro
• 金额: --
• 依托单位: Nagoya University
• 依托单位国家: 日本
• 项目类别: Grant-in-Aid for international Scientific Research
• 财政年份: 1997
• 资助国家: 日本
• 起止时间: 1997 至 无数据
• 项目状态: 已结题
• 来源: https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-09041198/
• 关键词: GEWEX; GAME; Asian Monsoon; Energy and water cycle; Continental-scale; Intensive observation; Tropics; Tibetan Plateau; Siberia; 植生フラックス観測; 広域土壌水分分布観測; チベット; アエロゾンデ観測; 冬期集中観測

The project team of this rsearch fund was organized for the promotion of regional experiments relevant to GEWEX/GAME activities. GEWEX/GAME is an international project to clarify the formation mechanism of Asian Monsoon, that is the biggest monsoon of the world, and to forecast the variation of water resources, during five years from 1996 to 2000.Thailand and Malaysia as Tropics, Tibetan Plateau and Siberia are included for field experimental area.Particularly, the studies in 1997 fiscal year were carried out for completing the preparation of the intensive observation to be implemented in the spring to summer season of 1998, in Tropics and Tibetan Plateau, and for flux observation in a cold winter, in Tundra and plain Taiga of Siberia.As research results, a monsoon march from diurnal -to seasonal- scale by the interaction between atmosphere and land surface was clarified in Thailand.In tibetan Plateau, local circulation of evaporated water due to strong convection was detected in summer season. Therefore, aero-sonde observation was planned in 1998, in order to investigate the structure of boundary layer.In Siberia, thawing and freezing processes of active layer in the top horizon of permafrost was intensivery observed and explained by using a one-dimensional model.

该RSEarch基金的项目团队是为了促进与GEWEX/GAME活动相关的区域实验而组织的。 Gewex/Game是一个国际项目，旨在阐明亚洲季风的形成机制，这是世界上最大的季风，并预测从1996年至2000年的五年中，水资源的变化。将于1998年的春季至夏季在热带和藏族高原上实施，以及在寒冷的冬天，在西伯利亚的苔原和平原的塔加（Taiga of Shiberia）中进行的通量观察。随着研究结果，季风从昼夜 - 季节性到季节性到季节性的互动，在泰比尔（Thailand）的境地中，在泰比特（Thailand）的境地中，在泰比尔（Thailand）的境地中阐明了季节性的季节性，以季节性地散布。因此，为了研究边界层的结构，在1998年进行了空调观察。在西伯利亚，在长期冻土顶部的有效层的融化和冻结过程是通过使用一维模型观察到的。

项目成果

Herath, S., Jha, R. and Musiake, K.: "Application of IISDHM to Predict the Flood in the Chiang Mai and Phraya cities, Thailand"The Third International Study Conference on GEWEX in Asia and GAME. 14-2. 430-440 (1997)

Herath, S.、Jha, R. 和 Musiake, K.：“应用 IISDHM 预测泰国清迈和披耶市的洪水”第三届亚洲 GEWEX 和 GAME 国际研究会议。

Matsumoto, J.: "Seasonal transition of summer rainy season over Indochina and adjacent monsoon region" Advance in Atmospheric Science. 14(2). 231-245 (1997)

Matsumoto, J.：“印度支那和邻近季风地区夏季雨季的季节转变”大气科学进展。

Ma, X., Hiyama, T., Fukushima, Y., and Hashimoto, T: "A numerical model of the heat transfer for permafrost regions"J. Jpn. Soc. Hydro. & Water Resource. 11-4. 346-359 (1998)

Ma, X.、Hiyama, T.、Fukushima, Y. 和 Hashimoto, T：“永久冻土地区传热的数值模型”J。

Yang, D., Herath, S. and Musiake, K.: "Analysis of Stability of River Network Geomorphologic Parameters Using DEM Data of Japanese Catchments"Proc. of the 27th Congress of the Intl. Association for Hydraulic Research. Vol.2. 973-978 (1997)

Yang, D.、Herath, S. 和 Musiake, K.：“使用日本流域 DEM 数据分析河网地貌参数的稳定性”Proc。