• Geographical Research
  • Vol. 39, Issue 7, 1680 (2020)
Shi HU1, Jian HAN2, Chesheng ZHAN1、*, and Liangmeizi LIU1、3
Author Affiliations
  • 1Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China
  • 2Powerchina Northwest Engineering Corporation Limited, Xi'an 710065, China
  • 3University of Chinese Academy of Sciences, Beijing 100049, China
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    DOI: 10.11821/dlyj020190545 Cite this Article
    Shi HU, Jian HAN, Chesheng ZHAN, Liangmeizi LIU. Spatial downscaling of remotely sensed precipitation in Taihang Mountains[J]. Geographical Research, 2020, 39(7): 1680 Copy Citation Text show less
    Location, DEM, NDVI and meteorological stations of Taihang Mountains
    Fig. 1. Location, DEM, NDVI and meteorological stations of Taihang Mountains
    Spatial pattern of monthly original GPM data and downscaled GPM data in July 2015
    Fig. 2. Spatial pattern of monthly original GPM data and downscaled GPM data in July 2015
    Comparisons of observed precipitation with original GPM precipitation and downscaled GPM data at monthly scale
    Fig. 3. Comparisons of observed precipitation with original GPM precipitation and downscaled GPM data at monthly scale
    Comparisons of observed data with downscaling precipitation using different methods
    Fig. 4. Comparisons of observed data with downscaling precipitation using different methods
    Spatial pattern of monthly precipitation in Taihang Mountains in 2015
    Fig. 5. Spatial pattern of monthly precipitation in Taihang Mountains in 2015
    Effect of residual correction on downscaled precipitation
    Fig. 6. Effect of residual correction on downscaled precipitation
    时滞阶数1月2月3月4月5月6月7月8月9月10月11月12月平均
    R200.420.720.920.920.740.620.760.810.820.890.370.330.628
    10.450.690.920.930.750.600.710.760.810.890.370.330.618
    20.570.700.900.930.780.610.700.740.800.880.360.370.627
    30.460.680.910.930.740.600.760.750.790.870.340.460.627
    RMSE(mm/月)03.363.527.246.5918.4426.9332.6435.0515.717.7911.521.7314.211
    13.273.717.206.3118.5227.8036.2035.3816.218.1111.381.6814.647
    22.913.697.546.5217.6727.5636.3136.7016.448.4011.821.7114.771
    33.163.807.296.4917.9727.6732.6135.7116.708.6512.141.6314.487
    MAE(mm/月)02.252.515.865.0013.3220.6125.1728.4513.716.2410.091.2311.204
    12.252.915.824.8413.6321.1926.2228.9613.936.279.991.2711.439
    22.052.936.205.0213.1021.2625.5229.9414.166.299.751.2911.458
    32.192.946.075.0413.3521.6323.6829.7114.686.569.811.2311.407
    最优时滞阶数201120000013
    Table 1. Coefficients of determination (R2), Root Mean Square Error (RMSE) and Mean Absolute Error (MAE) between downscaled precipitation and observed precipitation in Taihang Mountains
    Shi HU, Jian HAN, Chesheng ZHAN, Liangmeizi LIU. Spatial downscaling of remotely sensed precipitation in Taihang Mountains[J]. Geographical Research, 2020, 39(7): 1680
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