|
2216: |
Line
of convection running from NW-SE through S-Pol scope and loose
convection over the mountains to the NE. Convective line has formed
along a seabreeze front visible in the GOES-10 Vis loop. |
2300: |
Increased organization along the seabreeze front. |
2330: |
Strong phase shifts through SE portion of the line. Southern portion of
system slowly propagating towards the GOC - perhaps due to onset of
landbreeze enhanced by outflow from mountain storms. |
0021: |
Linear organization breaking up into several multicellular systems,
gradual westward motion. |
|
0030: |
S-Pol
log discussion: MCS resembles a leading-line trailing-stratiform (LLTS)
MCS, with stratiform rain well to the east of the leading line. Leading
line (which consists of remnants of seabreeze front) looking good while
stratiform rain (which consists of remnants of mountain convection) is
dying out as sun sets. If origins of these 2 regions is correct, they
are not dynamically linked which may be responsible for the loose
organizational structure. |
0230: |
Begin Microphysical Scanning, Running NearPPI135:
Convection portion of system looking decreasingly organized, out over
the GOC. |
0245: |
Switching to MicroNear135: |
0300: |
Switching to MicroFar135:
Main convection well
to the N of line, looks detached from original line. |
|
0315: |
Switching to MicroFar90:
Concentrating on stronger cells to the N/NW, at far end of S-Pol scope. |
0330: |
End Microphysical Scanning, Switching to ClimoFar:
Convection dying. |
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