JpGU-AGU Joint Meeting 2020

講演情報

[E] ポスター発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS06] 台風研究の新展開~過去・現在・未来

コンビーナ:宮本 佳明(慶應義塾大学 環境情報学部)、金田 幸恵(名古屋大学宇宙地球環境研究所)、和田 章義(気象研究所台風・災害気象研究部)、伊藤 耕介(琉球大学)

[AAS06-P15] Monthly Variation and Spatial Distribution of Quadrant Tropical Cyclone Size in the Western North Pacific

*Tonghua Su4Wei Hong1Yulan Zheng2Bin Chen3Xiaoqing Ke5 (1.Fujian Meteorological Observatory of of China Meteorological Administration、2.Fujian Meteorological Information Center of China Meteorological Administration、3.Electric Power Research Institute of State Grid Fujian Electric Power Company、4.Fujian Climate Center of China Meteorological Administration、5.Fujian Meteorological Service Center of China Meteorological Administration)

キーワード:tropical cyclone, size, quadrant, lifetime, circulation, symmetry

With the tropical cyclone (TC) size parameter defined as the radius of 17-m·s−1 oceanic surface wind, 225 TC cases were recorded in the western North Pacific during 2000–2009 based on the QuikSCAT near-surface wind vector database and the best-track dataset. In accordance with the symmetry index (the ratio of minimum and maximum quadrant sizes), the TCs were classified into symmetric and asymmetric structures. The asymmetric TCs were divided into four types: the northeast, southeast, southwest, and northwest. The spatio-temporal characteristics of these TC types were further investigated. The monthly variation and the spatial distribution of maximum quadrant TC size exhibited significant differences among the four types. By contrast, the quadrant size of the symmetric TCs from June to November showed few changes (2.6°–2.7° latitude). It was found that the TC lifetime is an important factor affecting the quadrant TC size because of its close relationship with the activities of the western Pacific subtropical high. In addition, the climatological mean circulation also has a notable influence on the quadrant TC size through superposition of prominent background wind. Symmetric TCs are more likely to occur in the oceanic region where the background low-level wind is the weakest.