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Numerical prediction of an intense convective system associated with the July 1987 montreal flood. part II: A trailing stratiform rainband
1995
ATMOSPHERE-OCEAN
In this study, thé internai circulation structures of thé 14 July 1987 intense mesoscale convective System (MCS) are investigated using an improved high-resolution version of thé Canadian régional finite-element model. It is found that although thé MCS is characterized by a leading convective Une followed by a trailing stratiform rainband, thé associated circulation structures differ substantially from those in thé classical midlatitude squall System. Thèse include thé rapid propagation and
doi:10.1080/07055900.1995.9649541
fatcat:ajgfggva25ealnrst4o35lmdpa