|
| Mesoscale Discussion 1737 |
|
< Previous MD
Next MD >
|
|
MESOSCALE DISCUSSION 1737
NWS STORM PREDICTION CENTER NORMAN OK
0411 AM CDT WED JUL 09 2008
AREAS AFFECTED...PORTIONS NERN OK...OZARKS OF SRN MO AND NRN AR.
CONCERNING...HEAVY RAINFALL
VALID 090911Z - 091145Z
HEAVY RAIN HAZARD WILL INCREASE THROUGH REMAINDER PRE-DAWN HOURS
OVER OZARK PLATEAU ON BOTH SIDES OF MO/AR BORDER...AND SHOULD
PERSIST OVER NERN OK E OF I-35...WITH SOME SWD SHIFT LIKELY INTO
MORE OF TUL METRO AREA. RAIN RATES LOCALLY 2-3 INCHES/HOUR SHOULD
BECOME MORE COMMON FROM W-E...AS WILL THREAT FOR REPEATED PASSAGE OF
HEAVIEST RAIN RATES IN A FEW LOCALES WITHIN BROADER PRECIP BAND.
SCATTERED-NUMEROUS TSTMS ALREADY EVIDENT OVER NRN OK ARE EXPECTED TO
SHIFT EWD ALONG THEIR AXIS...WHICH RUNS PARALLEL WITH DEEP-LAYER
MEAN WIND VECTOR. THIS WILL RESULT IN NET INCREASE OF CONVECTIVE
INTENSITY AND COVERAGE OVER THAT PRESENTLY OBSERVED IN OZARKS...AND
MAINTENANCE OF INTERMITTENT HEAVY RAIN REGIME ALREADY UNDERWAY OVER
NERN OK. VWP/PROFILER DATA SHOW CONFLUENT 20-25 KT 850 MB FLOW
ACROSS NRN OK ATTM. THIS CORRESPONDS WELL TO AREA OF ENHANCED
CONVECTIVE PRECIP...NRN RIM OF STRONGEST MOISTURE TRANSPORT...AND
AXIS OF MAXIMIZED 700-500 MB LAYER UVV EACH EVIDENT IN SHORT-TERM
RUC GUIDANCE...AS WELL AS LATEST NAM-KF RUNS. THIS REGIME
REASONABLY IS PROGGED TO MOVE EWD INTO NWRN AR/SWRN MO AS UNDERLYING
850 MB FLOW VEERS ACROSS CENTRAL/NRN OK DURING NEXT 3-4 HOURS.
HEAVY RAIN POTENTIAL ALSO MAY SHIFT SLIGHTLY SWD FROM PRESENT
LOCATION OF PRECIP PLUME AS ASSOCIATED OUTFLOW BOUNDARY DOES
LIKEWISE...BRINGING MORE OF OK FROM SWO-TUL AREAS EWD BENEATH
STRONGER CORRIDOR OF ISENTROPIC ASCENT TO LFC. MUCAPES GENERALLY
1000-1500 J/KG WILL CHARACTERIZE PRECONVECTIVE/INFLOW AIR
MASS...ALONG WITH SOME 2-2.25 INCH PW VALUES...BASED ON MODIFIED
RUC/NAM-KF SOUNDINGS AND GPS DERIVED OBSERVATIONS.
..EDWARDS.. 07/09/2008
ATTN...WFO...LZK...SGF...TSA...OUN...
35739260 35859609 36189717 36929645 36919360 36709172
36239146
|
|
Top/All Mesoscale Discussions/Forecast Products/Home
|
|