從1996-2005年間發源於北太平洋西南海域且經過130°E-135°E， 15°N-25°N的颱風後來侵台或轉北者，有32個颱風，其中有23個颱風會繞行100 mb等壓面高壓中心，佔72%。這23個會繞行100 mb等壓面高壓中心的颱風中，有15個轉向， 8個侵台。所有轉向的颱風，其 100 mb等壓面高壓中心，比較靠東南，侵台者較偏西北。 北太平洋西南海域颱風行經關鍵區後轉向者，平均來說，在颱風頂上100 mb等壓面上，比侵台者有更強的南風與西風。100 mb等壓面高壓環狀系統的西北側的輻散現象，造成其下方產生輻合區，其輻合現象有利颱風發展。所以颱風避開下對流層輻散區，偏北進入下對流層輻合區時，產生相當於對100 mb等壓面高壓中心繞行的現象。地面高壓在高空向颱風所在方向傾斜後，與100 mb等壓面高空高壓結合。100 mb等壓面高空高壓也引導500 mb等壓面駛流層風向量，避開高空輻合投射區，指向高空輻散投射區。

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