I do wonder though if they'll go a step farther than that.

Moderator: S2k Moderators
MiamiensisWx wrote:Cells will likely be discrete because of 1) the low's motion and 2) the lack of linear forcing. If shear is too strong while surface winds are backed ("backed" implies westerly winds), the discrete supercells would eventually evolve into a broken or continuous squall line. Squall lines would also reduce instability ahead of the surface boundary, thus reducing the tornado threat. In this case, there is a large warm sector with decent THETA-E ahead of the boundary. The progged 500 mb ridge juxtaposition and consolidated trough also ensures adequate low-level moisture return. A large dry slot would also cap convection (in addition to less lift) over the northern Gulf, which allows an uncontaminated "return flow" and higher 12-hour maximum temps well into the Mississippi Valley. Winds will likely be veered (S or SSE) in this case, which also heightens the threat. Even closer to the low, the lack of linear forcing would likely support strong discrete cells with backed (WSW) winds.
THETA-E link:
http://www.theweatherprediction.com/habyhints/324/
Linear forcing:
http://meetings.aps.org/Meeting/DFD05/Event/36922
MiamiensisWx wrote:MiamiensisWx wrote:Cells will likely be discrete because of 1) the low's motion and 2) the lack of linear forcing. If shear is too strong while surface winds are backed ("backed" implies westerly winds), the discrete supercells would eventually evolve into a broken or continuous squall line. Squall lines would also reduce instability ahead of the surface boundary, thus reducing the tornado threat. In this case, there is a large warm sector with decent THETA-E ahead of the boundary. The progged 500 mb ridge juxtaposition and consolidated trough also ensures adequate low-level moisture return. A large dry slot would also cap convection (in addition to less lift) over the northern Gulf, which allows an uncontaminated "return flow" and higher 12-hour maximum temps well into the Mississippi Valley. Winds will likely be veered (S or SSE) in this case, which also heightens the threat. Even closer to the low, the lack of linear forcing would likely support strong discrete cells with backed (WSW) winds.
THETA-E link:
http://www.theweatherprediction.com/habyhints/324/
Linear forcing:
http://meetings.aps.org/Meeting/DFD05/Event/36922
Umm... why did no one appreciate my response?!
I guess you are ignored if you aren't a met...
RL3AO wrote:MiamiensisWx wrote:MiamiensisWx wrote:Cells will likely be discrete because of 1) the low's motion and 2) the lack of linear forcing. If shear is too strong while surface winds are backed ("backed" implies westerly winds), the discrete supercells would eventually evolve into a broken or continuous squall line. Squall lines would also reduce instability ahead of the surface boundary, thus reducing the tornado threat. In this case, there is a large warm sector with decent THETA-E ahead of the boundary. The progged 500 mb ridge juxtaposition and consolidated trough also ensures adequate low-level moisture return. A large dry slot would also cap convection (in addition to less lift) over the northern Gulf, which allows an uncontaminated "return flow" and higher 12-hour maximum temps well into the Mississippi Valley. Winds will likely be veered (S or SSE) in this case, which also heightens the threat. Even closer to the low, the lack of linear forcing would likely support strong discrete cells with backed (WSW) winds.
THETA-E link:
http://www.theweatherprediction.com/habyhints/324/
Linear forcing:
http://meetings.aps.org/Meeting/DFD05/Event/36922
Umm... why did no one appreciate my response?!
I guess you are ignored if you aren't a met...
I read it and checked out your links. I just didn't respond. Maybe it had too many big words?
MiamiensisWx wrote:Cells will likely be discrete because of 1) the low's motion and 2) the lack of linear forcing. If shear is too strong while surface winds are backed ("backed" implies westerly winds), the discrete supercells would eventually evolve into a broken or continuous squall line. Squall lines would also reduce instability ahead of the surface boundary, thus reducing the tornado threat. In this case, there is a large warm sector with decent THETA-E ahead of the boundary. The progged 500 mb ridge juxtaposition and consolidated trough also ensures adequate low-level moisture return. A large dry slot would also cap convection (in addition to less lift) over the northern Gulf, which allows an uncontaminated "return flow" and higher 12-hour maximum temps well into the Mississippi Valley. Winds will likely be veered (S or SSE) in this case, which also heightens the threat. Even closer to the low, the lack of linear forcing would likely support strong discrete cells with backed (WSW) winds.
THETA-E link:
http://www.theweatherprediction.com/habyhints/324/
Linear forcing:
http://meetings.aps.org/Meeting/DFD05/Event/36922
HarlequinBoy wrote:SPECIAL WEATHER STATEMENT
NATIONAL WEATHER SERVICE MEMPHIS TN
256 PM CST SUN FEB 3 2008
ARZ008-009-017-018-026>028-035-036-048-049-058-MOZ113-115-
MSZ001>017-020>024-TNZ001>004-019>021-048>055-088>092-041200-
ALCORN-BENTON MS-CALHOUN-CARROLL-CHESTER-CHICKASAW-CLAY-COAHOMA-
CRAIGHEAD-CRITTENDEN-CROCKETT-CROSS-DESOTO-DECATUR-DUNKLIN-DYER-
FAYETTE-GIBSON-GREENE-HARDEMAN-HARDIN-HAYWOOD-HENDERSON-HENRY-
ITAWAMBA-LAFAYETTE-LAKE-LAUDERDALE-LAWRENCE-LEE AR-LEE MS-MADISON-
MARSHALL-MCNAIRY-MISSISSIPPI-MONROE-OBION-PANOLA-PEMISCOT-
PHILLIPS-POINSETT-PONTOTOC-PRENTISS-QUITMAN-RANDOLPH-SHELBY-
ST. FRANCIS-TALLAHATCHIE-TATE-TIPPAH-TIPTON-TISHOMINGO-TUNICA-
UNION-WEAKLEY-YALOBUSHA-
INCLUDING THE CITIES OF...ABERDEEN...AMORY...BARTLETT...
BATESVILLE...BLYTHEVILLE...BOLIVAR...BOONEVILLE...
CARUTHERSVILLE...CLARKSDALE...COLLIERVILLE...CORINTH...
COVINGTON...DRESDEN...DYERSBURG...FORREST CITY...GERMANTOWN...
HARRISBURG...HELENA...HUMBOLDT...HUNTINGDON...IUKA...JACKSON...
JONESBORO...KENNETT...LEXINGTON...MARTIN...MEMPHIS...MILAN...
MILLINGTON...NEW ALBANY...OLIVE BRANCH...OXFORD...PARAGOULD...
PARIS...SAVANNAH...SOMERVILLE...SOUTHAVEN...TUNICA...TUPELO...
UNION CITY...WALNUT RIDGE...WEST MEMPHIS...WYNNE
256 PM CST SUN FEB 3 2008
...MAJOR SEVERE WEATHER OUTBREAK POSSIBLE ACROSS THE MIDSOUTH
TUESDAY AFTERNOON AND EVENING...
A STRONG COLD FRONT WILL MOVE INTO THE MIDSOUTH BEGINNING TUESDAY
AFTERNOON. THE FRONT WILL COLLIDE WITH A UNSEASONABLY WARM...MOIST
AIR MASS THAT WILL BE IN PLACE OVER THE REGION. THIS COMBINATION WILL
PRODUCE NUMEROUS SHOWERS AND THUNDERSTORMS OVER THE AREA.
THUNDERSTORMS THAT DEVELOP WILL LIKELY BECOME SEVERE FAIRLY QUICKLY.
THE MAIN THREATS FROM THE SEVERE STORMS WILL BE DAMAGING
WINDS...LARGE HAIL...AND POSSIBLE TORNADOES. THE BEST TIMING FOR THE
SEVERE WEATHER WILL BE BETWEEN 1 PM AND 9 PM CDT. PLEASE STAY
INFORMED WITH THE LATEST FORECASTS CONCERNING THE SEVERE WEATHER
POTENTIAL TUESDAY AFTERNOON AND EVENING.
The NWS office here seems pretty concerned/confident about this outbreak, so we'll see. Local media isn't mentioning anything other than "showers and thunderstorms" yet.
From this diagram it is seen that the ageostrophic wind is divergent in the right-entrance and left-exit regions of the jet streak, and convergent in the other regions (see diagram below). This leads to upward motion in the right-entrance and left-exit regions of the jet streak.
FXUS64 KLIX 032133
AFDLIX
AREA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE NEW ORLEANS LA
333 PM CST SUN FEB 3 2008
.DISCUSSION
MAIN FORECAST CONCERN CENTERS AROUND CONVECTION EXPECTED TUESDAY
AFTERNOON AND TUESDAY NIGHT.
...snip...
MODELS HAVE REMAINED QUITE CONSISTENT WITH EACH OTHER AND WITH
THE TIMING OF THE UPPER TROUGH NOW IMPACTING THE WEST COAST AS IT
TRAVERSES THE WESTERN U.S. AND MOVES ACROSS THE MID SECTION OF THE
COUNTRY AND THE MISSISSIPPI VALLEY TUESDAY AND TUESDAY NIGHT. AT
THIS TIME IT LOOKS AS IF MOST OF THE CONVECTION WILL HOLD OFF
UNTIL LATE TUESDAY AND TUESDAY NIGHT...ALTHOUGH THE WESTERN ZONES
WILL SEE MORE IN THE WAY OF COVERAGE TUESDAY AFTERNOON. SOME OF THIS
CONVECTION COULD BE STRONG TO SEVERE FROM LATE TUESDAY AFTERNOON
THROUGH TUESDAY EVENING. THE ASSOCIATED COLD FRONT WILL MOVE
ACROSS THE ENTIRE FORECAST AREA TUESDAY NIGHT.
icicle wrote:HarlequinBoy wrote:
The NWS office here seems pretty concerned/confident about this outbreak, so we'll see. Local media isn't mentioning anything other than "showers and thunderstorms" yet.
my local mets are mentioning it, big time.
Ed Mahmoud wrote:OK, the equations bear an uncomfortable resemblance to the diffusivity equation that petroleum engineers have to learn, before forgetting, but skimming past the scientific discussion
I can't copy the images here, but there are helpful pictures.From this diagram it is seen that the ageostrophic wind is divergent in the right-entrance and left-exit regions of the jet streak, and convergent in the other regions (see diagram below). This leads to upward motion in the right-entrance and left-exit regions of the jet streak.
Link
RL3AO wrote:My predictions for 6z
Day 1: 5% T, 15% W, 30% H = slight
Day 2: 45% moderate
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