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Topography-slope坡度對山崩面積15山崩面積( 平方公里 )10500~10 11~2021~3031~40 41~5051~6061~70 71~8081~90坡度坡度對山崩崩壞比山崩崩壞比0.50.40.30.20.100~10 11~20 21~30 31~40 41~50 51~60 61~70 71~80 81~90坡度成功大學衛星資訊研究中心 5mX5m DTM
Topography-Aspect坡向對山崩面積6山崩面積( 平方公里 )4200~45 45~90 90~135135~180180~225225~270270~315315~360坡向坡向對山崩崩壞比0.06山崩崩壞比0.040.0200~45 45~90 90~135 135~180 180~225 225~270 270~315 315~360坡向成功大學衛星資訊研究中心 5mX5m DTM
Page 1 and 2: Geohazard Assessment withHigh Resol
Page 3 and 4: Basic Information from DTMAltitude
Page 5 and 6: Discrete points Grids
Page 7 and 8: Comparison the Error of HeightUnit:
Page 10 and 11: 2574000Photogrammetry VS2572000LiDA
Page 12 and 13: 3D View of Regional Bias
Page 14 and 15: Aerial 5m DTMLiDAR 1m DTMTrenchRoad
Page 16 and 17: Aerial40maerial5mLiDAR5mLiDAR1m
Page 18 and 19: Slope
Page 20 and 21: Summary of published result for Lan
Page 22: Aerial Photos集集 084_921 地
Page 25 and 26: Determine the Weighting forLandslid
Page 27: Geology-Dist. To Structure與構
Page 31 and 32: Environment-PGAPGA 對山崩面
Page 33 and 34: Unstable Index MethodRatio Index=(N
Page 35 and 36: Reclassify Results
Page 37 and 38: Validation Region
Page 39 and 40: Calculated Factors
Page 41 and 42: Discussion1.Dist to gully2.Slope3.r
Page 43 and 44: Slope vs height vs landslideratio w
Page 45 and 46: InterpretationsLidar have better ch
Page 47: Thanks……yutt@mail.ncku.edu.twTE

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