Impacts of SST Patterns on Rapid Intensification of Typhoon Megi (2010)

DOI Web Site Web Site 被引用文献10件 参考文献60件 オープンアクセス
  • Sachie Kanada
    Institute for Space‐Earth Environmental Research Nagoya University Nagoya Japan
  • Satoki Tsujino
    Institute for Space‐Earth Environmental Research Nagoya University Nagoya Japan
  • Hidenori Aiki
    Institute for Space‐Earth Environmental Research Nagoya University Nagoya Japan
  • Mayumi K. Yoshioka
    Institute for Space‐Earth Environmental Research Nagoya University Nagoya Japan
  • Yasumasa Miyazawa
    Japan Agency for Marine‐Earth Science and Technology Yokohama Japan
  • Kazuhisa Tsuboki
    Institute for Space‐Earth Environmental Research Nagoya University Nagoya Japan
  • Izuru Takayabu
    Meteorological Research Institute/Japan Meteorological Agency Tsukuba Japan

書誌事項

公開日
2017-12-27
資源種別
journal article
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1002/2017jd027252
公開者
American Geophysical Union (AGU)

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説明

<jats:title>Abstract</jats:title><jats:p>Typhoon Megi (2010), a very intense tropical cyclone with a minimum central pressure of 885 hPa, was characterized by especially rapid intensification. We investigated this intensification process by a simulation experiment using a high‐resolution (0.02° × 0.02°) three‐dimensional atmosphere‐ocean coupled regional model. We also performed a sensitivity experiment with a time‐fixed sea surface temperature (SST). The coupled model successfully simulated the minimum central pressure of Typhoon Megi, whereas the fixed SST experiment simulated an excessively low minimum central pressure of 839 hPa. The simulation results also showed a close relationship between the radial SST profiles and the rapid intensification process. Because the warm sea increased near‐surface water vapor and hence the convective available potential energy, the high SST in the eye region facilitated tall and intense updrafts inside the radius of maximum wind speed and led to the start of rapid intensification. In contrast, high SST outside this radius induced local secondary updrafts that inhibited rapid intensification even if the mean SST in the core region exceeded 29.0°C. These secondary updrafts moved inward and eventually merged with the primary eyewall updrafts. Then the storm intensified rapidly when the high SST appeared in the eye region. Thus, the changes in the local SST pattern around the storm center strongly affected the rapid intensification process by modulating the radial structure of core convection. Our results also show that the use of a high‐resolution three‐dimensional atmosphere‐ocean coupled model offers promise for improving intensity forecasts of tropical cyclones.</jats:p>

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