Takemi (2007) ¤ÎÀßÄê¤Ë¤ª¤±¤ëÆ󼡸µ·×»» (²¹ÅÙ: Ç®ÂÓ¾ì, ¼¾ÅÙ: Q18, 0.0 km¡Á2.5 km ¤Ë±ôľ¥·¥¢¡¼¤Î¤¢¤ëÉ÷, Us = 15 ms^-1)

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• Takemi, 2007 ¤Ç¤ÎÀѱÀÂÐή¤Î¿ôÃÍ¥·¥ß¥å¥ì¡¼¥·¥ç¥ó¤ËÍѤ¤¤é¤ì¤¿, ²¹ÅÙ¡¦¼¾ÅÙ¡¦É÷¤òÍѤ¤¤Æ·×»»¤ò¤·¤¿.

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    • 0.0 km-2.5 km
  • É÷¤Î¥·¥¢¡¼Ãæ¤ÎºÇÂçÉ÷® (Us)
    • U_s = 15 m/s

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• ¿åÊ¿³Ê»Ò´Ö³Ö : 1 km
• ±ôľ³Ê»Ò´Ö³Ö : 500 m
• Ť¤»þ´Ö¥¹¥Æ¥Ã¥× : 1 s
• û¤¤»þ´Ö¥¹¥Æ¥Ã¥× : 0.2 s
• ¿åÊ¿Îΰè : 450 km
• ±ôľÎΰè : 18 km
• ÀÑʬ»þ´Ö : 6 h
• ÂÐή·÷³¦Ì̹âÅÙ : 12 ­Ò

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• Takemi, T., 2007: A sensitivity of squall-line intensity to environmental static stability under various shear and moisture conditions Atmospheric Research Volume 84, Issue 4, June 2007, Pages 374-389
• Takemi, T., 2006: Impacts of moisture profiles on the evolution and organization of midlatitde squall lines under various shear conditions, Atmos. Res., Vol.82.
• Weisman, M.L., Klemp, J.B., 1982. The dependence of numerically simulated convective storms on vertical wind shear and buoyancy. Mon. Weather Rev. 110, 504-520.