Liu Jiayi, Deng Lijiao, Fu Guobin, et al. The applicability of two statistical downscaling methods to the Qinling Mountains. J Appl Meteor Sci, 2018, 29(6): 737-747. DOI:  10.11898/1001-7313.20180609.
Citation: Liu Jiayi, Deng Lijiao, Fu Guobin, et al. The applicability of two statistical downscaling methods to the Qinling Mountains. J Appl Meteor Sci, 2018, 29(6): 737-747. DOI:  10.11898/1001-7313.20180609.

The Applicability of Two Statistical Downscaling Methods to the Qinling Mountains

DOI: 10.11898/1001-7313.20180609
  • Received Date: 2018-05-11
  • Rev Recd Date: 2018-08-23
  • Publish Date: 2018-11-30
  • The Qinling Mountains is not only the dividing line of northern China and southern China, but also the dividing line between monsoon climate of medium latitudes and subtropical monsoon climate in China, i.e., the dividing line between China's warm temperate and subtropical regions. It also has abundant natural resources because of its special geographical location and complex climate environment. In the context of global warming, impacts of climate change on forest ecosystems in the Qinling Mountains are of great significance. Global climate model which is widely used in large-scale climate simulation studies, cannot be applied in this region due to low resolution. Statistical downscaling model can be used to provide local-scale daily temperature and precipitation for studying climate change impacts of this region. Different statistical downscaling models have different principals, as well as different predictors. Therefore, it is necessary to compare different downscaling models and to select more appropriate downscaling model to obtain reasonable simulation results. Focusing on the future daily mean temperature and precipitation for the Qinling Mountains, the multiple linear regression and the ridge regression downscaling approaches based on ASD (automated statistical downscaling) model are implemented. Outputs from the general circulation model (MPI-ESM-LR) under RCP4.5 and RCP8.5 scenarios are analyzed. Simulation results of two statistical downscaling approaches during calibration and validation periods are analyzed and future climate change projections in periods of 2006-2040, 2041-2070 and 2071-2100 are generated. During the calibration and validation periods, both statistical downscaling approaches perform well in simulating the mean temperature and precipitation. However, the multiple linear regression perform better than the ridge regression, and the mean of simulated temperature is better than that of precipitation. Both statistical downscaling approaches project an increase for the mean temperature and its magnitudes depending on the emission scenarios, i.e., RCP8.5 resulting in a higher temperature than RCP4.5. The annual precipitation would slightly decrease but not statistically significantly, while the seasonal distribution of annual precipitation will change, a slightly increase in spring and a decrease in other seasons, especially in summer. In summary, the multiple linear regression is more suitable for statistical downscaling research in the Qinling Mountains.
  • Fig. 1  Location of meteorological stations in the Qinling Mountains

    Fig. 2  Comparison of monthly mean value(a) and standard deviation(b) of temperature between the observed and the simulated by two statistical downscaling approaches in the Qinling Mountains during calibration period

    Fig. 3  Comparison of different climate variables of precipitation between the observed and the simulated by two statistical downscaling approaches in the Qinling Mountains during calibration period

    Fig. 4  Comparison of mean value(a) and standard deviation(b) of temperature between the observed and the simulated by two statistical downscaling approaches in the Qinling Mountains during validation period

    Fig. 5  Comparison of different climate variables of precipitation between the observed and the simulated by two statistical downscaling approaches in the Qinling Mountains during validation period

    Fig. 6  Future mean temperature change in the Qinling Mountains generated by two statistical downscaling approaches under different scenarios in different periods

    (a)the multiple linear regression, (b)the ridge regression

    Fig. 7  Future precipitation change in the Qinling Mountains generated by two statistical downscaling approaches under different scenarios in different periods

    (a)the multiple linear regression, (b)the ridge regression

    Table  1  Predictors used for NCEP/NCAR and MPI-ESM-LR

    序号 变量
    1 500 hPa相对湿度
    2 700 hPa相对湿度
    3 850 hPa相对湿度
    4 海平面气压
    5 500 hPa温度
    6 700 hPa温度
    7 850 hPa温度
    8 近地面温度
    9 500 hPa纬向风速
    10 700 hPa纬向风速
    11 850 hPa纬向风速
    12 近地面纬向风速
    13 500 hPa经向风速
    14 700 hPa经向风速
    15 850 hPa经向风速
    16 近地面经向风速
    17 500 hPa位势高度
    18 700 hPa位势高度
    19 850 hPa位势高度
    DownLoad: Download CSV

    Table  2  Explained variance and root mean square error of the multiple linear regression in calibration period

    站点 气温 降水量
    解释方差 均方根误差 解释方差 均方根误差
    宝鸡 0.969 0.0060 0.208 0.648
    西安 0.968 0.0063 0.182 0.569
    华山 0.919 0.0093 0.241 1.14
    略阳 0.961 0.0043 0.266 2.30
    汉中 0.958 0.0053 0.227 2.08
    佛坪 0.956 0.0053 0.184 0.955
    商县 0.973 0.0040 0.196 0.826
    镇安 0.962 0.0059 0.153 1.24
    石泉 0.964 0.0075 0.297 1.95
    安康 0.957 0.0082 0.204 1.21
    DownLoad: Download CSV

    Table  3  Explained variance and root mean square error of the ridge regression in calibration period

    站点 气温 降水量
    解释方差 均方根误差 解释方差 均方根误差
    宝鸡 0.969 0.0157 0.207 0.899
    西安 0.968 0.0188 0.179 0.749
    华山 0.919 0.0164 0.240 1.35
    略阳 0.961 0.0227 0.267 2.55
    汉中 0.959 0.0256 0.234 2.73
    佛坪 0.956 0.0180 0.182 1.18
    商县 0.973 0.0175 0.196 1.12
    镇安 0.962 0.0211 0.155 1.61
    石泉 0.962 0.0231 0.297 2.02
    安康 0.957 0.0253 0.204 1.97
    DownLoad: Download CSV
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    • Received : 2018-05-11
    • Accepted : 2018-08-23
    • Published : 2018-11-30

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