Characteristics of Tropical Cyclones over the Western North Pacific in 2008

2008년 태풍 특징

  • Cha, Eun-Jeong (National Typhoon Center, Korea Meteorological Administration) ;
  • Hwang, Ho-Seong (National Typhoon Center, Korea Meteorological Administration) ;
  • Yang, Kyung-Jo (National Typhoon Center, Korea Meteorological Administration) ;
  • Won, Seong-Hee (National Typhoon Center, Korea Meteorological Administration) ;
  • Ko, Seong-Won (National Typhoon Center, Korea Meteorological Administration) ;
  • Kim, Dong-Ho (National Typhoon Center, Korea Meteorological Administration) ;
  • Kwon, H. Joe (Department of Atmospheric Sciences/Typhoon Research Center, Kongju National University)
  • 차은정 (기상청 국가태풍센터) ;
  • 황호성 (기상청 국가태풍센터) ;
  • 양경조 (기상청 국가태풍센터) ;
  • 원성희 (기상청 국가태풍센터) ;
  • 고성원 (기상청 국가태풍센터) ;
  • 김동호 (기상청 국가태풍센터) ;
  • 권혁조 (공주대학교 대기과학과/태풍연구센터)
  • Received : 2009.03.09
  • Accepted : 2009.05.07
  • Published : 2009.06.01

Abstract

The purpose of this study is to summarize the tropical cyclone (TC) activity of 2008 over the western North Pacific including the verification of the official track and intensity forecast errors of these TCs. The TC activity - frequency, Normalized Typhoon Activity (NTA), and life span - was lower than 58-year (1951-2008) average. 22 tropical cyclones of tropical storm (TS) intensity or higher formed in the western North Pacific and the South China Sea in 2008. The total number is less than 58-year average frequency of 26.4. Out of 22 tropical cyclones, 11 TCs reached typhoon (TY) intensity, while the rest 11 TCs only reached severe tropical storm (STS) and tropical storm (TS) intensity - six STS and five TS storms. One typhoon KALMAEGI (0807) among them affected the Korea peninsula. However, no significant impact - casualty or property damage - was reported. On average of 22 TCs in 2008, the Korea Meteorological Administration (KMA) official track forecast error for 48 hours was 229 km. There was a big challenge for individual cyclones such as 0806 FENGSHEN and 0817 HIGOS presenting significant forecast error, with both intricate tracks and irregular moving speed. The tropical cyclone season in 2008 began in April with the formation of NEOGURI (0801). In May, four TCs formed in the western North Pacific in response to enhanced convective activity. On the other hand, the TC activity was very weak from June to August. It is found that the unusual anti-cyclonic circulation in the lower level and weak convection near the Philippines are dominant during summertime. The convection and atmospheric circulation in the western North Pacific contributed unfavorable condition for TC activity in the 2008 summertime. The 2008 TC activity has continued the below normal state since mid 1990s which is apparent the decadal variability in TC activity.

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