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2DD analysis (based on hour data)Rainfall [mm] Tokai Sta.Akuhi Sta.KuwabaraMax (zone)Kuwabara Max (Japan)Takara Max (Tokai)Kuwabara Max (Tokai) In zone, the overall rainfall records around the Nagoya Plainare smaller than those of the mountainous area. The Tokai rainstorm seems extremal at 6-12 hours scales inparticular.
3DA (Depth-Area) analysis• Source data 10minutes rainfall data,hourly rainfall data• Areal rainfall evaluation methodFixed area method( on the map of grid-rainfall data based on the ThiessenPolygons in the target area)
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Contents of Project-22.1 Remote Sen
Page 6 and 7:
Studies at PWRIrelated to2.1 Remote
Page 8 and 9:
Study area (Chuetsu District of the
Page 10 and 11:
Relationship between normalizedsumm
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SWE-rank classification map(1997-98
Page 14 and 15:
Studies at PWRIrelated to2.1 Remote
Page 16 and 17:
2. River monitoring1)Super high-res
Page 18 and 19:
Land cover classification and detec
Page 20 and 21:
Contents of TLS studies at PWRI•
Page 22 and 23:
Topography mapping with TLSwith thr
Page 24 and 25:
Investigation of river-bed material
Page 26 and 27: Potential to mapping riverbed topog
Page 28 and 29: Main water-stage observatoriesnear
Page 30 and 31: Study AreaCambodia, Tonle Sap Lake
Page 33 and 34: Estimation of flood inundationof th
Page 35 and 36: BackgroundDistributed-parameter mod
Page 37 and 38: Development of basin-wide distribut
Page 39 and 40: Characteristics of hydrologicproces
Page 41 and 42: Actual evapotranspiration (Ea)= Pen
Page 43 and 44: Net Radiation: Rn ’ ’”
Page 45 and 46: Soil moisture accounting (wet perio
Page 48 and 49: Location of the254km 2Kusaki-Damwat
Page 50 and 51: River-channel networks for Kusaki-D
Page 52 and 53: NDVI map for the Kusaki-Dam watersh
Page 54 and 55: Vegetation cover ratio map based on
Page 56 and 57: Long-termstreamflowsimulation witht
Page 58 and 59: Long-term streamflow simulationwith
Page 60 and 61: Characteristics of WEHY model• He
Page 62 and 63: Model computational unitsSoilparame
Page 64 and 65: Field survey for ground-truth data
Page 66 and 67: Verification cases of WEHY modelat
Page 68 and 69: Conclusions• A priori estimation
Page 70 and 71: General weather situation• Autu
Page 72 and 73: 1 Collect the rainfall data Ho
Page 74 and 75: 2DD (Depth-Duration) analysis• So
Page 78 and 79: 24-hour maximum areal rainfall extr
Page 80 and 81: Analysis of the Tokai-storm DAD cur
Page 82 and 83: Conclusion (1 of 2)• Tokai-storm
Page 84: Future subjects• Establishment of
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