| Project/Area Number |
10305037
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| Research Category |
Grant-in-Aid for Scientific Research (A)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
水工水理学
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| Research Institution | KYOTO UNIVERSITY |
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Principal Investigator |
NAKAKITA Eiichi KYOTO UNIVERSITY, Graduate of Engineering, Associate Professor, 工学研究科, 助教授 (70183506)
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| Co-Investigator(Kenkyū-buntansha) |
TANAKA Kenji KYOTO UNIVERSITY, Disaster Prevention Research Inst., Research Associate, 防災研究所, 助手 (30283625)
KONDOH Akihiko Chiba Univ., CERes, Associate Professor, 環境リモートセンシング研究センター, 助教授 (30201495)
EBISU Nobuhiro Ehime Univ., Faculty of Agriculture, Associate Professor, 農学部, 助教授 (60176782)
YSHIDA Hiromu Tokushima Univ., F. of Engineering, Associate Professor, 工学部, 助教授 (10210717)
TANAKA Takafumi Nagoya Univ., School of Agriculture, Research Associate, 農学研究科, 助手 (40192174)
開發 一郎 広島大学, 総合科学部, 教授 (60160959)
砂田 憲吾 山梨大学, 工学部, 教授 (20020480)
小池 俊雄 長岡技術科学大学, 建設系, 助教授 (30178173)
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| Project Period (FY) |
1998 – 2000
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| Project Status |
Completed (Fiscal Year 2001)
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| Budget Amount *help |
¥31,900,000 (Direct Cost: ¥31,900,000)
Fiscal Year 2000: ¥4,800,000 (Direct Cost: ¥4,800,000)
Fiscal Year 1999: ¥8,900,000 (Direct Cost: ¥8,900,000)
Fiscal Year 1998: ¥18,200,000 (Direct Cost: ¥18,200,000)
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| Keywords | The Lake Biwa Project / Hydrological Surficial Process / Remote Sensing / Scale Effect / Water Circulation / Evapotranspiration / Soil Moisture / Campaign Observation |
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| Research Abstract |
The Lake Biwa project is featured by "Campaign and Permanent Field Observations Synchronized with Space- and Air-borne Remote Sensing", "Collaboration by Scientists, Engineers and Agriculturists" and "the Goal as Understanding Hydrologic Circulation in the Lake Biwa Basin Using Hydrologic-Meteorological Combined Models Assimilated by the Field Observations". This project has been promoted about 20 groups from around Japan.
In the second stage, we shifted weight from every-year campaign observation into permanent observation at four representative points. Operation of the permanent system in paddy field and forested area started in 1998 and in urban area and lake surface in 1999. According to this weight-shift to the permanent observation, we set "seasonal and year-to-year variation " and "vegetation phenology" as additional targets by effectively utilizing operational satellite information. Of course, for understanding the scale effect up to 20 km scale, tuning of model parameters and data assimilation are unchanged targets.
At the site of the paddy field instruments for measuring or estimating radiation and heat budget and water budget based on Bowen ratio method were set up. Also photosynthesis active radiometer was set up in this April. Measurement in forested area is almost same as paddy field except for using SAT. Campaign observations for measuring LAI and heat pulse velocity has been carried out on typical days of each. Measurements at lake-surface and urban area sites are almost same except that basis is set on the bulk method. All data from these four sites are collected at office using mobile phone.
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