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K.Fukami, T.Matsuura and J.Yoshitani (2003) Evaluation ofDAD curves of the Tokai Rainstorm in September of 2000,3rd DPRI – IIASA International Symposium on IntegratedDisaster Risk Management, Kyoto.2.2 2000
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Page 1 and 2:
PWRI-USGS : Topic2PWRI1)2):1)Georg
Page 3 and 4:
Topic22.1 2.2
Page 5 and 6:
2.2(1)a) (1) (2) XYZb) (2) ()
Page 7 and 8:
SARSWE• •
Page 9 and 10:
SAR•
Page 11 and 12:
RADARSAT-SAR36.51.91.919.21.91.917.
Page 13 and 14:
• ()• (. SAR ?)• • (CREST?
Page 15 and 16:
( ) Structure damage Inundation( )
Page 17 and 18:
(2001)vol.43, No.1, pp.14-19(IKONOS
Page 19 and 20: TLS( )• 3 CCD 1 3• 33TLSTLS
Page 21 and 22: • ( 1.0 km) 2002/1/301/31
Page 23 and 24: TLS TLS =3.5cm (H=300m)
Page 25 and 26: TLS•2cm•210cm•1020cm•2080cm
Page 27 and 28: ) Landsat-TM
Page 29 and 30: KompongLuongPrekKdamPhnom Penh
Page 32 and 33: (Landsat- TM/ETM+)2000.3.252000.7.2
Page 35 and 36: c) GIS
Page 38 and 39: • GISGISGISGISGISGISA 0ABCA 0A 0A
Page 40 and 41: • =• =A 0ABCA 0A 0AABCBC
Page 42 and 43: (Ea)= Penman-Monteith
Page 44 and 45: Net Radiation: Rn ’ ’”
Page 46: ():)(1_11 QseepESdtSpervcobiw−−
Page 49 and 50: (254km 2 )254km 2
Page 51 and 52: 200m
Page 53 and 54: NDVI
Page 57 and 58: (2000)GISvol.42, No.11, pp.26-31.
Page 59 and 60: • (1997)(1997)
Page 61 and 62: WEHY • WEHY
Page 63 and 64: MCU) GIS
Page 65: • 1,16,11 2,12,177,620(• 13 3,8
Page 68 and 69: 1400120010008006004002000WEHYDischa
Page 72 and 73: 1. 2. DD (depth-duration)3. DA (dep
Page 74 and 75: 100150100150 6100200250250200100200
Page 76 and 77: 2DD (10 ) [mm] DD:6 =378mm D
Page 78 and 79: 3DA (Depth-Area)• 10• ()
Page 80 and 81: DAD(A,t)279t 0.5 exp(-0.0248t -0.41
Page 82 and 83: DAD Pa= a ⋅t0.5exp DAD: u=0.
Page 84 and 85: ( 2)• HortonDADDAD• DAD
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