| Co-Investigator(Kenkyū-buntansha) |
KAWAMOTO Kazuaki 長崎大学, 大学院水産・環境科学総合研究科, 教授 (10353450)
MURAYAMA Toshiyuki 東京海洋大学, 大学院海洋科学技術研究科, 教授 (50200308)
EGUCHI Nawo 九州大学, 応用力学研究所, 助教 (50378907)
IWASAKI Toshiki 東北大学, 大学院理学研究科, 教授 (80302074)
TSUBOKI Kazuhisa 名古屋大学, 地球水循環研究センター, 教授 (90222140)
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| Budget Amount *help |
¥100,373,000 (Direct Cost: ¥77,210,000、Indirect Cost: ¥23,163,000)
Fiscal Year 2014: ¥13,338,000 (Direct Cost: ¥10,260,000、Indirect Cost: ¥3,078,000)
Fiscal Year 2013: ¥21,905,000 (Direct Cost: ¥16,850,000、Indirect Cost: ¥5,055,000)
Fiscal Year 2012: ¥21,060,000 (Direct Cost: ¥16,200,000、Indirect Cost: ¥4,860,000)
Fiscal Year 2011: ¥24,960,000 (Direct Cost: ¥19,200,000、Indirect Cost: ¥5,760,000)
Fiscal Year 2010: ¥19,110,000 (Direct Cost: ¥14,700,000、Indirect Cost: ¥4,410,000)
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| Outline of Final Research Achievements |
A relationship between micro and macro physical properties of cloud and heat flux at the sea surface was studied by using satellite observation data, ship-borne observation data, surface observation data, and numerical simulation with a cloud-resolving model. The results show that condensation process is dominant in the growth of cloud droplet over the area where heat flux at the sea surface is large, while collision process is important for the droplet growth in the other area. It was shown from the space-borne lidar and cloud-radar that overlapping clouds suppress the underlying low level cloud development.
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