STRUCTURES OF SNOW CLOUDS ASSOCIATED WITH A COLD AIR FLOW

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  • 冬期石狩湾における陸からの冷気流フロント上に発生する降雪雲観測
  • トウキ イシカリワン ニ オケル リク カラ ノ レイキリュウ フロント ジョ

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This study analyzes snow clouds associated with cold air flow around Ishikari Bay which occurred during 1993-1996 in winter seasons. Formation, growth, movement and decay of snow clouds associated with cold air flow were confirmed by using Kite baloon observation, Pinneshiri Radar data, SNET data and Sonde data. According to their scales, snow clouds were classified into 4 levels, that is, LEVEL0, LEVEL1, LEVEL2 and LEVEL3. It was found that 4 levels were distinguished by V-component of wind.

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