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嵇磊, 黄梦宇, 李书严, 周珺. 探空气球漂移位置订正对一次大风降温过程的模拟研究[J]. 气候与环境研究, 2012, 17(6): 848-854. DOI: 10.3878/j.issn.1006-9585.2012.06.21
引用本文: 嵇磊, 黄梦宇, 李书严, 周珺. 探空气球漂移位置订正对一次大风降温过程的模拟研究[J]. 气候与环境研究, 2012, 17(6): 848-854. DOI: 10.3878/j.issn.1006-9585.2012.06.21
JI Lei, HUANG Mengyu, LI Shuyan, ZHOU Jun. Positioning of Sounding Balloon Drifting Associated with a Gale Process and Temperature Drop[J]. Climatic and Environmental Research, 2012, 17(6): 848-854. DOI: 10.3878/j.issn.1006-9585.2012.06.21
Citation: JI Lei, HUANG Mengyu, LI Shuyan, ZHOU Jun. Positioning of Sounding Balloon Drifting Associated with a Gale Process and Temperature Drop[J]. Climatic and Environmental Research, 2012, 17(6): 848-854. DOI: 10.3878/j.issn.1006-9585.2012.06.21

探空气球漂移位置订正对一次大风降温过程的模拟研究

Positioning of Sounding Balloon Drifting Associated with a Gale Process and Temperature Drop

  • 摘要: 应用改进后的MM5 模式, 采用包含有实际探空气球在各个气压层上精确的经纬度信息的新型探空资料, 研究探空资料对高分辨率中尺度数值模式的影响。通过对一次中尺度大风降温天气过程的模拟分析, 可以看出:位置订正对初始气象要素场的改变虽然总体上有低层较小, 高层较大的特征, 但是在500 hPa 以下大气运动剧烈的情况下, 低层气象要素场的改变量也会较大, 甚至会超过高层相应的气象要素场的变化, 速度场的改变尤为明显;位置订正使得模拟结果在数值和影响范围上都有效地减小了误差, 更加接近实况;位置订正后, 模式较准确的模拟出了该次向南推进的大风降温过程的移动变化, 尤其是模拟的大风前沿位置与实况的对应关系较好, 温度场的变化与速度场的变化有较好的一致性。

     

    Abstract: With the improved model MM5, the impact of a height-dependent sounding balloon’s drifting on a mesoscale numerical model is analyzed, using new sounding data with accurate position information at each pressure level. Simulations of a gale and a temperature decrease indicate the following: the differences in the initial meteorological element fields, especially the velocity field, caused by position correction would be great in the lower layers, even exceeding that in the upper layers, when the atmospheric motion becomes strong below 500 hPa, although the differences are greater in the upper layers than in the lower layers in the mass. Position correction can reduce the simulation errors not only in the numerical values but also in the sphere of influence, so the results approach the observed data more closely. After position correction, the model can accurately simulate the southward movement of the strong wind and temperature decrease. The simulated foreland of the strong wind corresponds with the observed data, and the variation in the temperature field is quite consistent with the variation in the velocity field.

     

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