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Linear MCS (with
overall look of leading line-trailing stratiform MCS) formed along
inland seabreeze front during the late afternoon / early evening hours
on 8/15/04. System began dissipating by late evening. However, leading
line and stratiform regions do not appear to be dynamically linked,
leaving system with a loose organizational structure and perhaps not a
true LLTS system (see explanation in S-Pol Scan Summary below).
2130 Z:
Visible seabreeze front along much of GOC coast in vicinity of S-Pol.
2200 Z:
Convection developing along a seabreeze front starting to look
organized.
2300 Z:
Increasing organization along seabreeze front - developing leading-line
MCS.
2350 Z:
Southern portion of MCS moving westward, toward GOC.
0100 Z:
Linear structure breaking up, leaving several multcellular systems. |
