金少华, 周泓, 白学文, 艾永智. “2010.07”两次影响低纬高原西行台风对比分析[J]. 云南大学学报(自然科学版), 2014, 36(S1): 53-63. doi: 10.7540/j.ynu.20130731
引用本文: 金少华, 周泓, 白学文, 艾永智. “2010.07”两次影响低纬高原西行台风对比分析[J]. 云南大学学报(自然科学版), 2014, 36(S1): 53-63. doi: 10.7540/j.ynu.20130731
JIN Shaohua, ZHOU Hong, BAI Xuewen, AI Yongzhi. Comparative analysis of two westward moving typhoons entering low latitude plateau in 2010.07[J]. Journal of Yunnan University: Natural Sciences Edition, 2014, 36(S1): 53-63. DOI: 10.7540/j.ynu.20130731
Citation: JIN Shaohua, ZHOU Hong, BAI Xuewen, AI Yongzhi. Comparative analysis of two westward moving typhoons entering low latitude plateau in 2010.07[J]. Journal of Yunnan University: Natural Sciences Edition, 2014, 36(S1): 53-63. DOI: 10.7540/j.ynu.20130731

“2010.07”两次影响低纬高原西行台风对比分析

Comparative analysis of two westward moving typhoons entering low latitude plateau in 2010.07

  • 摘要: 利用地面加密观测资料、自动站降雨量资料、FY-2C卫星TBB资料和NCEP再分析等资料,对1002号台风“康森”和1003号台风“灿都”进入低纬高原后引发云南强降水天气的成因及其在陆上维持机制进行对比分析,结果表明:西行台风“康森”和“灿都”生成源地不同,登陆地点不同,台风低压进入云南后除了自身携带的大量水汽和能量外,南侧强盛偏南急流有助于台风低压维持,“康森”进入云南后受到来自孟加拉湾西南气流卷入,为台风低压提供了充足水汽,使得台风低压在云南持久不消,移向滇西时与高原东侧下滑冷空气形成冷暖交汇,是“康森”进入云南西部后降水加强的主要原因.2次西行台风进入低纬高原后,低层水汽辐合都得到加强,水汽辐合区中低层对应为上升气流,高层为下沉气流,对强降水维持起到重要作用.进入低纬高原后的台风低压受地形抬升作用,激发出的中尺度云团是产生强降水的直接原因.

     

    Abstract: Based on surface intensive observational data,automatic rainfall station data,TBB data of FY-2C satellite and reanalysis data of NCEP,the weather causes of Yunnan heavy rainfall induced by the typhoon No.1002 “Conson” and No.1003“Chanthu” entering low latitude plateau and the maintaining mechanism on the land area have been compared and analyzed.The results show that the birthplaces and the landing locations of two typhoons were different.Typhoon depression,after entered into Yunnan,besides carrying a large quantity vapor and energy itself,involved south jet flow is long subsistence.The main reason that “Conson” caused heavy rainfall in Yunnan was that the convergence of the cold and warm air over west Yunnan.The moisture convergence strengthened on the lower level after typhoon depression entered into Yunnan.The updraft appeared on the lower level in convergence area of vapor and the downdraft appeared on the higher level,which maintaining heavy rainfall.After typhoon depression entering low latitude plateau,a few mesoscale cloud cluster excited by the mountain dynamic effect that led to heavy rainfall.

     

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