4 . 4 Mips Observations of Bow Echoes During
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چکیده
In the late 1970s the convective system that is referred to as the bow echo was identified by Fujita (1978). It was identified as a type of convective storm structure associated with intense damaging winds or downburst (Johns 1993). As more of these systems were studied, a better understanding was made on their kinematic structure and dynamical processes. Bow echoes can range in size from 15 km to 150 km, and can occur at anytime of year (Klimowski et al. 2000). Much of the damage reported in the United Sates from non-tornadic winds is a result of bow echo systems.
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5j.14 Observations of the 24 June 2003 Bow Echo Case during Bamex
In the late 1970s the convective system that is referred to as the bow echo was identified by Fujita (1978). It was identified as a type of convective storm structure associated with intense damaging winds or downburst (Johns 1993). As more of these systems were studied, a better understanding was made on their kinematic structure and dynamical processes. Bow echoes can range in size from 15 km...
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