The role of ocean‐atmosphere interaction in <scp>T</scp>yphoon <scp>S</scp>inlaku (2008) using a regional coupled data assimilation system

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  • Akiyoshi Wada
    Meteorological Research Institute, Japan Meteorological Agency Tsukuba Ibaraki Japan
  • Masaru Kunii
    Meteorological Research Institute, Japan Meteorological Agency Tsukuba Ibaraki Japan

書誌事項

公開日
2017-05
資源種別
journal article
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1002/2017jc012750
公開者
American Geophysical Union (AGU)

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説明

<jats:title>Abstract</jats:title><jats:p>For improving analyses of tropical cyclone (TC) and sea surface temperature (SST) and thereby TC simulations, a regional mesoscale strongly coupled atmosphere‐ocean data assimilation system was developed with the local ensemble transform Kalman filter (LETKF) implemented with the Japan Meteorological Agency's nonhydrostatic model (NHM) coupled with a multilayer ocean model and the third‐generation ocean wave model. The NHM‐LETKF coupled data assimilation system was applied to Typhoon Sinlaku (2008) along with the original NHM‐LETKF system to investigate the sensitivity of Sinlaku to SST assimilation with the Level 2 Pre‐processed (L2P) standard product of satellite SST. SST calculated in the coupled‐assimilation experiment with the coupled data assimilation system and the satellite SST (CPL) showed a better correlation with Optimally Interpolated SST than SST used in the control experiment with the original NHM‐LETKF (CNTL) and SST calculated in the succession experiment with the coupled system without satellite SST (SUCC). The time series in the CPL experiment well captured the variation in the SST observed at the Kuroshio Extension Observation buoy site. In addition, TC‐induced sea surface cooling was analyzed more realistically in the CPL experiment than that in the CNTL and SUCC experiments. However, the central pressure analyzed in each three experiments was overestimated compared with the Regional Specialized Meteorological Center Tokyo best‐track central pressure, mainly due to the coarse horizontal resolution of 15 km. The 96 h TC simulations indicated that the CPL experiment provided more favorable initial and boundary conditions than the CNTL experiment to simulate TC tracks more accurately.</jats:p>

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