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