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  • The Influence of Atmosphere to Passive Microwave Retrieval of Snow Depth over Qinghai-Tibetan Plateau

    The Influence of Atmosphere to Passive Microwave Retrieval of Snow Depth over Qinghai-Tibetan Plateau

    LIU Jinjun, FU Yunfei, LI Rui, WANG Yu, FU Yuyun, HU Jiheng

    Plateau Meteorology, 2018 37 (2): 305-316.

    The microwave at low and moderate frequencies (e. g., 18.7 and 36.5 GHz) has good transmittance through the atmosphere, therefor in most algorithms for satellite passive microwave (PMW) remote sensing snow parameters, ig. . .

     
  • Diagnosis and Simulation on the Relationship between Snow Depth over Qinghai-Tibetan Plateau and Summer Precipitation in Eastern China

    Diagnosis and Simulation on the Relationship between Snow Depth over Qinghai-Tibetan Plateau and Summer Precipitation in Eastern China

    LI Yan, YAN Jiahai, ZHANG Dongfeng

    Plateau Meteorology, 2018 37 (2): 317-324.

    Snow cover over Qinghai-Tibetan Plateau (QTP) is an important component of climate system in East Asia. Its depth shows strong inter-annual variability. It is understood that the variation of snow depth over QTP is stron. . .

     
  • Comparison of Four Methods for Calculating Surface Fluxeson Alpine Grassland at Naqu

    Comparison of Four Methods for Calculating Surface Fluxeson Alpine Grassland at Naqu

    YAN Xiaoqiang, HU Zeyong, SUN Genhou, XIE Zhipeng

    Plateau Meteorology, 2018 37 (2): 358-370.

    The near-surface layer gradients observed data of wind speed, temperature and specific humidity combined with the radiative and soil heat fluxes have been widely applied in estimating the surface-air turbulent exchange o. . .

     
  • Experiment and Verification of the Convective-Scale Ensemble Forecast Based on BGM

    Experiment and Verification of the Convective-Scale Ensemble Forecast Based on BGM

    MA Shenjia, CHEN Chaohui, HE Hongrang, LI Xiang, LI Yi

    Plateau Meteorology, 2018 37 (2): 495-504.

    Based on breeding of growing modes (BGM) method, an ensemble forecast experiment was tested for a strong squall line considering the highly non-linear feature and detailed forecast requirement in convective-scale weather. . .

     
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