周海霞, 刘春霞. 1321号强台风“蝴蝶”发生与发展特点分析[J]. 云南大学学报(自然科学版), 2014, 36(S1): 35-44. doi: 10.7540/j.ynu.20140130
引用本文: 周海霞, 刘春霞. 1321号强台风“蝴蝶”发生与发展特点分析[J]. 云南大学学报(自然科学版), 2014, 36(S1): 35-44. doi: 10.7540/j.ynu.20140130
Analysis on characteristics of occurrence and development of strong typhoon Wutip(1321)[J]. Journal of Yunnan University: Natural Sciences Edition, 2014, 36(S1): 35-44. DOI: 10.7540/j.ynu.20140130
Citation: Analysis on characteristics of occurrence and development of strong typhoon Wutip(1321)[J]. Journal of Yunnan University: Natural Sciences Edition, 2014, 36(S1): 35-44. DOI: 10.7540/j.ynu.20140130

1321号强台风“蝴蝶”发生与发展特点分析

Analysis on characteristics of occurrence and development of strong typhoon Wutip(1321)

  • 摘要: 利用地面、高空、天气雷达探测资料、卫星云图和NCEP再分析资料综合分析研究,发现:1321号强台风“蝴蝶”形成具有螺旋桨特征,即暖洋面上各高度层存在的3支水平风切变与对流层顶3支强分流构成螺旋桨,正绝对涡度分布与切变线相对应,切变线的辐合抬升、涡旋以及螺旋桨中心暖湿气柱的上升运动推动螺旋桨发生旋转,环境能量的注入、东北季风的加强则促进螺旋桨旋转加强.“蝴蝶”外围(400~900km)的冷平流和降温对其发展具有很好的指示意义:(-4~-25)×10-5 k·m2·s-1强度的冷平流、中层-1~-2℃的降温有力促进热带气旋“蝴蝶”的发展,而冷平流入侵其内圈、破坏内核热力结构对“蝴蝶”的发展则会起削弱作用.值得一提的是,高分辨率天气雷达观测事实表明,“蝴蝶”移动的前方,积云对流产生、组织发展以及台前飑线的代谢会激发热带气旋发展;在台风稳定阶段,台风本体结构调整异常活跃,具有台风眼壁破裂—复原—破裂重复调整的特征;台风突变为强台风前,内、外螺旋云带发生调整,表现为台前飑线建立并卷入台风内圈,内外螺旋云带合并、形成密闭云带,并与云墙发生分离形成较大范围的下沉区;台风不同部位的云体均呈锥状,最密实、最强降水和最大风主要集中在6km高度以下区域.

     

    Abstract: Based on the high and low detection data,CIN-Radar and satellite cloud picture data,NCEP reanalysis data,analysis on characteristics of occurrence and development of strong typhoon Wutip(1321) is made.The results show that Wutip occurs with a screw propeller which is formed by the three level wind shears and the three strong shunts of tropopause on a warm ocean.Propeller rotation being occurred possibly because that absolute vorticity distribution overlaps shear line which is upthrow and vortex,and warm moist air column moves upward in the center of screw propeller.But ulteriorly,the screw propeller rotates because of energy injection and the northeast monsoon enhancing.It is usual to promote that cold advection ((-4—-25)×10-5 K·m2·s-1) and cooling (-1—-2℃) in the periphery of Wutip,but not that in typhoon kernel.It is worth mentioning that convection,organization and development of cumulus and metabolic typhoon squall in the front of typhoon moving can inspire developing of typhoon.During of typhoon stabilization,ontology structure adjusts so anomaly that typhoon squall is build and involved in inner ring,the spiral cloud bands combine to separate with cloud wall and form a larger range of subsidence area.There is the most dense cloud,the strongest rainfall and the strongest wind under 6km in different parts of typhoon.

     

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