Atmospheric Simulations Using OGCM-Assimilation SST: Influence of the Wintertime Japan Sea on Monthly Precipitation

  • Author(s): Masaru Yamamoto and Naoki Hirose
  • DOI: 10.3319/TAO.2009.03.18.03(IWNOP)
  • Keywords: Precipitation, SST, Japan Sea, Mesoscale atmospheric model, Data assimilation
  • Citation: Yamamoto, M. and N. Hirose, 2010: Atmospheric simulations using OGCM-assimilation SST: Influence of the wintertime Japan Sea on monthly precipitation. Terr. Atmos. Ocean. Sci., 21, 113-122, doi: 10.3319/TAO.2009.03.18.03(IWNOP)

Temperature data for the Japan Sea obtained from ocean data assimilation modeling is applied to atmospheric simulations of monthly precipitation for January 2005. Because the volume of flow of the Tsushima Warm Current was large during the winter season, the sea surface temperature (SST) and coastal precipitation were higher in comparison with those in 2003. In order to evaluate influence of SST on monthly precipitation, we use surface temperatures of the Japan Sea in 2003 and 2005 for comparative simulations of precipitation for January 2005. The precipitation in experiment C (using cool SST data in 2003) is smaller than that in experiment W (using warm SST data in 2005) in a large part of the sea area, since the small evaporation results from the low SST over the upstream area of northwesterly winter monsoon. In the domain of 33.67 - 45.82°N and 125.89 - 142.9°E, the averaged evaporation and precipitation in experiment C are 10% and 13% smaller than those in experiment W, respectively. About half of the difference between the precipitations observed for January 2003 and 2005 in a heavy snow area is equal to the difference between the two simulations. Our results show that the mesoscale SST difference between 2003 and 2005 is related to the local difference of monthly precipitation.

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