OCEAN WAVE-DEPENDENT ROUGHNESS IMPACTS ON CLIMATE SYSTEM BY COUPLED ATMOSPHERIC GLOBAL CLIMATE-WAVE MODEL

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  • 全球大気気候-波浪結合モデルによる海面粗度を通した波浪の気候への影響評価
  • ゼン キュウ タイキ キコウ-ハロウ ケツゴウ モデル ニ ヨル カイメンソド オ トオシタ ハロウ ノ キコウ エ ノ エイキョウ ヒョウカ

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Abstract

 Ocean surface waves take important roles at an interface between atmosphere and ocean. The wave-dependent surface roughness was implemented into the Atmospheric Global Climate Model using the spectral wave model, and climate simulations were conducted. Wave steepness- and wave age-dependent roughness were considered. The spatial distributions of roughness climatology correspond to the dominance of swells for the climate simulation with wave steepness-dependent roughness and the stationarity of wind direction for that with wave age-dependent one, respectively. The differences of roughness cause the differences in surface wind climatology by 1m/s compared with uncoupled simulations, large differences especially at the lower-latitude. Furthermore, we indicate that the influences can extend to upper-atmosphere such as the climatology of tropical cyclone track. Implementing ocean waves into a climate model can have a wide impacts on the climate simulations.

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