Possible relation of the western North Pacific monsoon to the tropical cyclone activity over western North Pacific. (16th December 2015)

• Record Type: Journal Article
• Authors: Choi, Jae‐Won; Kim, Baek‐Jo; Zhang, Renhe; Park, Ki‐Jun; Kim, Jeoung‐Yun; Cha, Yumi; Nam, Jae‐Cheol
• Is Part Of: International journal of climatology. Volume 36:Number 9(2016)
• Page Start: 3334
• Page End: 3345
• Publication Date: 2015-12-16
• Subjects: western North Pacific monsoon -- tropical cyclone -- TC genesis frequency; Climatology -- Periodicals; Climat -- Périodiques; Climatologie -- Périodiques; 551.605
• DOI: 10.1002/joc.4558
• Languages: English
• ISSNs: 0899-8418

Abstract

ABSTRACT: This study examined the relationship between the western North Pacific monsoon (WNPM) and the tropical cyclone (TC) activity over western North Pacific during the summer (June to August) in a period from 1977 to 2013. According to the western North Pacific monsoon index (WNPMI), 10 years with high indices (referred to as the positive WNPMI phase) and 10 years with low indices (referred to as the negative WNPMI phase) were chosen. TCs frequently formed in the southeast quadrant of the subtropical western North Pacific in the positive WNPMI phase, and in the northwest quadrant in the negative phase. With respect to the TC track, TCs tended to move northward from the distant sea off the east coast of the Philippines towards Korea and Japan past the East China Sea in the positive WNPMI phase, whereas the characteristic pattern of the negative phase was the TC movement from the Philippines to southern China and the Indochinese peninsula over the South China Sea. As for the TC intensity, the TCs were stronger in the positive WNPMI phase than in the negative WNPMI phase. The anomalous cyclonic circulations in the south of the 30°N signified strong convection, causing the high TC genesis frequency in the positive WNPMI phase. In addition, the East China Sea, Korea and Japan were shown to be influenced by the anomalous southeasterly, which contributed as the anomalous steering flows and was favourable for the TCs to move into these regions in the positive WNPMI phase. Meanwhile, the positive anomaly of 600 hPa relative humidity and sea surface temperature as well as the negative anomaly of vertical wind shear presented in most regions of the subtropical western North Pacific, creating an environment that facilitated the generation of TCs in the positive WNPMI phase.