ISSN 1000-0526
CN 11-2282/P
CN 11-2282/P
Archive > Volume 32 Issue 12 > 2006,32(12):72-75. DOI:10.7519/j.issn.1000-0526.2006.12.012 Prev Next
Analysis of Mesoscale and Microscale Structures of a Strong Squall Line
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Abstract:
Based on the routine data and the observations of CINRAD/SA radar and automat-ic weather stations,a squall line affecting Fujian on May 22,2005 is analyzed.The squall line is a kind of instable and strong convective weather caused by the air with upper-layer dry and lower-layer wet in front of the upper-troposphere trough.The Mesoscale structure,such as bow echo,strong rear inflow and weak echo region on the inflow entrance etc,with the squall line,caused the disasterous wind.
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