[Objective] The research aimed to study the influences of GWDO parameterization scheme and terrain on a rainstorm in Dabie Mountain.[Method] By using NCEP/NCAR 1°×1° analytical data,the conventional and...[Objective] The research aimed to study the influences of GWDO parameterization scheme and terrain on a rainstorm in Dabie Mountain.[Method] By using NCEP/NCAR 1°×1° analytical data,the conventional and unconventional ground observation data,WRFV3.1.1 version of non-hydrostatic balance meso-scale mode,a meso-scale shear line rainstorm process which happened in Dabie Mountain zone during 05:00-14:00 on June 21,2008 was carried out the diagnostic analysis and numerical test.In the control experiment,the gravity wave drag by orography(GWDO) parameterization scheme was added.The influences of GWDO parameterization scheme and terrain on the rainstorm process were discussed respectively by the sensitivity test.[Result] The orography dragging coefficient had the good improvement role on the rainstorm intensity or falling zone.The result had the very big difference when considering or non-considering the orography dragging coefficient.After the parameterization scheme was added,the rainstorm intensity or falling zone was better than that of non-addition.When there was no dragging coefficient,the shear line disturbance was strong,and the gravity wave activity was obvious.The precipitation was stronger in the zone where the gravity wave was obvious.The terrain in Dabie Mountain and the surrounding place also had the important effect on the shear line precipitation.When the terrain in Dabie Mountain was removed,the precipitation intensity on the shear line increased significantly,and the strengthening of rain belt in the west was the most obvious.When the terrain in the southeast of Dabie Mountain was removed,the precipitation in the east had the obvious increasing effect.The terrain wasn’t favorable for the rainstorm strengthening.The intensity variation of rain belt not only related to the terrain,but also related to the disturbance variation on the shear line.[Conclusion] The research provided the theory basis for the prediction and forecast of rainstorm.展开更多
WRF(weather research and forecasting)模式中参数化方案的选择与近地面风场的仿真模拟结果关系密切。为解决新疆北部不同地形地区风场模拟准确性的问题,采用WRF中尺度气象模式,探究4类参数化方案(边界层、微物理、陆面过程、近地面层...WRF(weather research and forecasting)模式中参数化方案的选择与近地面风场的仿真模拟结果关系密切。为解决新疆北部不同地形地区风场模拟准确性的问题,采用WRF中尺度气象模式,探究4类参数化方案(边界层、微物理、陆面过程、近地面层)以及次网格地形方案对新疆北部不同地形地区风场模拟结果的影响。结果表明:每组试验均能模拟出风速的变化趋势;陆面过程RUC(rapid update cycle)方案和微物理Lin(Purdue Lin)方案对平原地区模拟结果较好,陆面过程Noah方案和微物理WSM6(WRF single moment 6 class)方案对山区地形模拟结果较好,且对于平原和山谷地形,次网格地形方案对模拟地区均能起到较好的修正作用。展开更多
区域气候模式对高原降水模拟存在系统性高估。该文从热力学角度考虑了局地(小尺度)地形对陆气过程的影响,以提高区域气候模式高原降水模拟能力。通过在天气研究与预报(weather research and forecasting, WRF)模式陆面过程模块耦合地形...区域气候模式对高原降水模拟存在系统性高估。该文从热力学角度考虑了局地(小尺度)地形对陆气过程的影响,以提高区域气候模式高原降水模拟能力。通过在天气研究与预报(weather research and forecasting, WRF)模式陆面过程模块耦合地形热力效应方案,将二维地形太阳辐射方案改进为三维地形太阳辐射方案,根据山区太阳辐射理论对太阳辐射直射、辐射散射、地形反射过程进行改进,得到改进方案;基于改进方案在亚东河谷开展高分辨率WRF模式降水模拟研究。结果表明:采用改进方案模拟的太阳辐射、降水结果与实测结果更接近,能够降低河谷降水高估的现象。改进方案能够体现出更多地形变化对地表辐射分布的影响:日间,山体坡面由于接收更多辐射得到加热(0.09~0.20℃),产生上升气流,在坡面形成更强上坡风(0.02~0.08 m/s),将河谷水汽携带到坡面以上,水汽在坡面以上区域爬升并形成降水,导致河谷区域降水减少(-4.54~-3.34 mm)、坡面以上区域降水增多(0.59~2.82 mm)。该研究对提高区域气候模式对山区降水的模拟效果具有重要意义。展开更多
基金Supported by National Key Basic Research Development Project Planning "973"(2009CB421503)National Natural Science Fund(40975037)Public Welfare Industry (Meteorology) Science Research Specific Item(GYHY200806009)
文摘[Objective] The research aimed to study the influences of GWDO parameterization scheme and terrain on a rainstorm in Dabie Mountain.[Method] By using NCEP/NCAR 1°×1° analytical data,the conventional and unconventional ground observation data,WRFV3.1.1 version of non-hydrostatic balance meso-scale mode,a meso-scale shear line rainstorm process which happened in Dabie Mountain zone during 05:00-14:00 on June 21,2008 was carried out the diagnostic analysis and numerical test.In the control experiment,the gravity wave drag by orography(GWDO) parameterization scheme was added.The influences of GWDO parameterization scheme and terrain on the rainstorm process were discussed respectively by the sensitivity test.[Result] The orography dragging coefficient had the good improvement role on the rainstorm intensity or falling zone.The result had the very big difference when considering or non-considering the orography dragging coefficient.After the parameterization scheme was added,the rainstorm intensity or falling zone was better than that of non-addition.When there was no dragging coefficient,the shear line disturbance was strong,and the gravity wave activity was obvious.The precipitation was stronger in the zone where the gravity wave was obvious.The terrain in Dabie Mountain and the surrounding place also had the important effect on the shear line precipitation.When the terrain in Dabie Mountain was removed,the precipitation intensity on the shear line increased significantly,and the strengthening of rain belt in the west was the most obvious.When the terrain in the southeast of Dabie Mountain was removed,the precipitation in the east had the obvious increasing effect.The terrain wasn’t favorable for the rainstorm strengthening.The intensity variation of rain belt not only related to the terrain,but also related to the disturbance variation on the shear line.[Conclusion] The research provided the theory basis for the prediction and forecast of rainstorm.
文摘WRF(weather research and forecasting)模式中参数化方案的选择与近地面风场的仿真模拟结果关系密切。为解决新疆北部不同地形地区风场模拟准确性的问题,采用WRF中尺度气象模式,探究4类参数化方案(边界层、微物理、陆面过程、近地面层)以及次网格地形方案对新疆北部不同地形地区风场模拟结果的影响。结果表明:每组试验均能模拟出风速的变化趋势;陆面过程RUC(rapid update cycle)方案和微物理Lin(Purdue Lin)方案对平原地区模拟结果较好,陆面过程Noah方案和微物理WSM6(WRF single moment 6 class)方案对山区地形模拟结果较好,且对于平原和山谷地形,次网格地形方案对模拟地区均能起到较好的修正作用。
文摘区域气候模式对高原降水模拟存在系统性高估。该文从热力学角度考虑了局地(小尺度)地形对陆气过程的影响,以提高区域气候模式高原降水模拟能力。通过在天气研究与预报(weather research and forecasting, WRF)模式陆面过程模块耦合地形热力效应方案,将二维地形太阳辐射方案改进为三维地形太阳辐射方案,根据山区太阳辐射理论对太阳辐射直射、辐射散射、地形反射过程进行改进,得到改进方案;基于改进方案在亚东河谷开展高分辨率WRF模式降水模拟研究。结果表明:采用改进方案模拟的太阳辐射、降水结果与实测结果更接近,能够降低河谷降水高估的现象。改进方案能够体现出更多地形变化对地表辐射分布的影响:日间,山体坡面由于接收更多辐射得到加热(0.09~0.20℃),产生上升气流,在坡面形成更强上坡风(0.02~0.08 m/s),将河谷水汽携带到坡面以上,水汽在坡面以上区域爬升并形成降水,导致河谷区域降水减少(-4.54~-3.34 mm)、坡面以上区域降水增多(0.59~2.82 mm)。该研究对提高区域气候模式对山区降水的模拟效果具有重要意义。
