It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
...EASTERN OK/TX INTO THE OZARKS AND LOWER/MID MS VALLEY -- WEDNESDAY MORNING INTO EARLY AFTERNOON... SHORTWAVE IMPULSES WILL EJECT AHEAD OF THE MAIN UPPER TROUGH ACROSS THIS REGION DURING THE MORNING...AND THUNDERSTORMS MAY ALREADY BE ONGOING 12Z/WED ACROSS PARTS OF OK/TX INTO SW MO. WEAK TO MODERATE ELEVATED INSTABILITY WILL BE IN PLACE ATOP RESIDUAL EML...AND VERTICAL SHEAR WILL BE ADEQUATE FOR SEMI ORGANIZED STORM CLUSTERS. THIS EARLY ACTIVITY WILL INCREASE IN COVERAGE AND PRODUCE SPORADIC SEVERE HAIL THROUGH THE MORNING AND SHIFT EAST/NORTHEAST TOWARD THE OZARKS AND LOWER/MID-MS VALLEY REGION THROUGH THE AFTERNOON. ...SOUTHERN AND CENTRAL PLAINS -- WEDNESDAY AFTERNOON INTO THE EVENING... THE BREADTH OF MORNING ACTIVITY WILL HAVE AN IMPACT ON HOW THINGS EVOLVE DURING THE AFTERNOON ACROSS CENTRAL/EASTERN OK/TX...AND GREATER UNCERTAINTY EXISTS AS A RESULT. HOWEVER...DETERMINISTIC AND SOME HI-RES GUIDANCE SUGGESTS ADEQUATE RECOVERY WILL OCCUR ACROSS THE WARM SECTOR AND ADDITIONAL THUNDERSTORM DEVELOPMENT FROM EASTERN OK/TX INTO WESTERN AR/LA IS EXPECTED. THE SURFACE DRYLINE WILL SURGE EASTWARD DURING THE DAY TO ROUGHLY THE I-35 CORRIDOR FROM CENTRAL KS THROUGH CENTRAL OK INTO TX...AND AN UNCAPPED AND MODERATELY UNSTABLE AIRMASS WILL EXIST. GIVEN THE ORIENTATION OF THE UPPER TROUGH...FORCING FOR ASCENT WILL BE STRONGEST OVER KS AND THE MID-MO VALLEY...WEAKENING WITH SOUTHWARD EXTENT. HOWEVER...A SOUTHWESTERLY LLJ ACROSS THE SOUTHERN PLAINS TO THE OZARKS AND STRONGER CONVERGENCE ALONG THE MOIST AXIS SHOULD BE ENOUGH TO COMPENSATE FOR MORE SUBTLE FORCING. DEVELOPMENT DURING THE AFTERNOON IS LIKELY NEAR THE SURFACE LOW/TRIPLE POINT AND ALONG THE DRYLINE FROM PARTS OF EASTERN NEB/KS INTO SOUTHWEST IA/NORTHWEST MO. THERE MAY BE A RELATIVE MIN IN ACTIVITY ACROSS PARTS OF SOUTHEAST KS/NORTHEAST OK/SOUTHWEST MO...AND THEN REDEVELOPMENT ACROSS THE WARM SECTOR IN SOUTHEAST OK/NORTHEAST TX AND ADJACENT PARTS OF AR/LA. THERMODYNAMIC AND KINEMATIC PROFILES WILL SUPPORT ALL HAZARD TYPES BOTH NEAR THE SURFACE LOW AND SOUTHWARD ALONG THE DRYLINE AND THROUGH THE WARM SECTOR. LARGE HAIL WILL BE THE MAIN THREAT...BUT TORNADOES ARE ALSO POSSIBLE. GIVEN DISPARITY AMONGST DETERMINISTIC GUIDANCE REGARDING LOW LEVEL MOISTURE AND THE EASTWARD POSITION OF THE DRYLINE...IN ADDITION TO ADDED UNCERTAINTY DUE TO MORNING CONVECTION...NO UPGRADES WILL BE MADE AT THIS TIME...THOUGH MAY BE POSSIBLE IN SUBSEQUENT OUTLOOKS.
In meteorology, convective available potential energy (CAPE),[1] sometimes, simply, available potential energy (APE), is the amount of energy a parcel of air would have if lifted a certain distance vertically through the atmosphere. CAPE is effectively the positive buoyancy of an air parcel and is an indicator of atmospheric instability, which makes it very valuable in predicting severe weather. It is a form of fluid instability found in thermally stratified atmospheres in which a colder fluid overlies a warmer one. As explained below, when an air mass is unstable, the element of the air mass that is displaced upwards is accelerated by the pressure differential between the displaced air and the ambient air at the (higher) altitude to which it was displaced. This usually creates vertically developed clouds from convection, due to the rising motion, which can eventually lead to thunderstorms. It could also be created by other phenomena, such as a cold front. Even if the air is cooler on the surface, there is still warmer air in the mid-levels, that can rise into the upper-levels. However, if there is not enough water vapor present, there is no ability for condensation, thus storms, clouds, and rain will not form.
originally posted by: TechniXcality
a reply to: TechniXcality
First let me link to CAPE and what it means when the term is used WIKI
In meteorology, convective available potential energy (CAPE),[1] sometimes, simply, available potential energy (APE), is the amount of energy a parcel of air would have if lifted a certain distance vertically through the atmosphere. CAPE is effectively the positive buoyancy of an air parcel and is an indicator of atmospheric instability, which makes it very valuable in predicting severe weather. It is a form of fluid instability found in thermally stratified atmospheres in which a colder fluid overlies a warmer one. As explained below, when an air mass is unstable, the element of the air mass that is displaced upwards is accelerated by the pressure differential between the displaced air and the ambient air at the (higher) altitude to which it was displaced. This usually creates vertically developed clouds from convection, due to the rising motion, which can eventually lead to thunderstorms. It could also be created by other phenomena, such as a cold front. Even if the air is cooler on the surface, there is still warmer air in the mid-levels, that can rise into the upper-levels. However, if there is not enough water vapor present, there is no ability for condensation, thus storms, clouds, and rain will not form.
Onto wrf ttu model prediction & forecast of available CAPE tomorrow at 5pm, when storms should be in the Dallas metro
This is showing anywhere from 2000 - 2500j/kg and exceeding of CAPE which is more than enough instability for surface based super cells & tornadoes, the models are now starting to agree that indeed a severe weather outbreak across the southern plains is imminent!
Here is the forecast picture just after peak heating (5pm) Wednesday North central Texas will have widely scattered super cells with intense amount of instability available - all modes of severe weather are possible. If you live in the southern plains please pay attention to your local weather stations or you can check your weather at National Weather Service simply click your state and county/city to view current watches/warnings and forecasts. This is a dangerous set up tomorrow and Ii would not be surprised if somewhere in the southern plains & or north central Texas is effected by multiple Tornadoes, Damaging winds, and very large hail to the size of softballs.
Here is a graphic for my area from NWS concerning tomorrow
As always everyone stay safe, will update
NATIONAL WEATHER SERVICE FORT WORTH TX 316 AM CDT WED MAR 30 2016 .DISCUSSION... AN ACTIVE WEATHER DAY IS LIKELY ACROSS THE ENTIRE REGION AS SEVERAL KEY INGREDIENTS FOR SEVERE WEATHER COME TOGETHER. THESE INGREDIENTS INCLUDE...ABUNDANT LOW LEVEL MOISTURE...STEEP MID LEVEL LAPSE RATES...LARGE SCALE LIFT SUPPLIED BY AN APPROACHING 150+ KNOT JET AND SMALLER SCALE LIFT GENERATED BY AN EASTWARD MOVING DRYLINE. ALTHOUGH THERE ARE MULTIPLE SCENARIOS WITH REGARDS TO TIMING AND PLACEMENT OF STORMS TODAY AND TONIGHT THE MOST LIKELY SCENARIO IS AS FOLLOWS: 1- ELEVATED SHOWERS AND STORMS DEVELOP NEAR OR SHORTLY AFTER SUNRISE TODAY...ESPECIALLY ALONG AND WEST OF THE INTERSTATE 35 CORRIDOR WHERE LARGE SCALE LIFT WILL BE THE STRONGEST. THESE STORMS WILL BE SCATTERED IN NATURE BUT WILL HAVE SOME POTENTIAL TO PRODUCE LARGE HAIL DUE TO THE COLD TEMPS ALOFT. 2 - THUNDERSTORMS WILL BECOME MORE NUMEROUS AND STRONGER BY LATE MORNING AS THE CAP WEAKENS AND EVENTUALLY DISSIPATES. ONCE THE CAP IS GONE...STORMS WILL BECOME MORE ROOTED IN THE BOUNDARY LAYER AND A MEDLEY OF HAZARDS INCLUDING HAIL...DAMAGING WINDS AND ISOLATED TORNADOES WILL BECOME POSSIBLE THROUGH THE AFTERNOON. 3 - BY LATE AFTERNOON A DRYLINE WILL ENTER THE WESTERN ZONES AND BECOME AN ADDITIONAL FOCUS FOR SHOWERS AND STORMS. THE EXTENT OF MORNING CONVECTION WILL HAVE AN IMPACT ON HOW EXTENSIVE STORMS ARE ON THE DRYLINE. WE STILL ANTICIPATE THAT STORMS WILL BE ONGOING IN THE EAST WHEN THE DRYLINE ENTERS THE REGION. STORMS BOTH ON THE DRYLINE AND EAST OF THE DRYLINE WILL HAVE A POTENTIAL TO BECOME SEVERE WITH ALL MODES OF SEVERE WEATHER POSSIBLE THROUGH THE EVENING. 4 - BY LATE EVENING A COLD FRONT WILL ENTER THE NORTHWEST ZONES AND WILL EVENTUALLY OVERTAKE THE DRYLINE. WHEN THIS OCCURS STORMS WILL END STEADILY FROM WEST TO EAST. THERE WILL STILL BE A POTENTIAL FOR SEVERE STORMS THROUGH THE EARLY MORNING HOURS...ESPECIALLY EAST OF THE INTERSTATE 35 CORRIDOR. AGAIN...WHAT IS DESCRIBED ABOVE IS THE MOST LIKELY SCENARIO FOR TODAY/TONIGHTS EVENTS. CONFIDENCE IS MODERATE TO HIGH THAT SEVERE WEATHER WILL OCCUR OVER THE NEXT 24 HOURS ACROSS PARTS OF NORTH AND CENTRAL TEXAS. WHAT COMPLICATES TODAYS FORECAST AND ANY SEVERE WEATHER EVENT FOR THAT MATTER IS MESO-SCALE PROCESSES THAT ARE DIFFICULT IF NOT IMPOSSIBLE TO ANTICIPATE. SO THE MESSAGE FOR TODAY IS THIS...BE PREPARED FOR SEVERE WEATHER TO DEVELOP AT ANY TIME TODAY/TONIGHT. SINCE THE KEY INGREDIENTS (MOISTURE... INSTABILITY...LIFT AND SHEAR) WILL ALL BE PRESENT...ANY STORM THAT FORMS WILL HAVE A GOOD POTENTIAL TO BECOME SEVERE.
originally posted by: TechniXcality
Watching for further development in this area would not be surprised to see a watch go up over north central Texas within the next hour, individual storms will move north east with an overall easterly movement. Stay tuned storms are firing
Severe Thunderstorm Watch SEVERE THUNDERSTORM WATCH OUTLINE UPDATE FOR WS 59 NWS STORM PREDICTION CENTER NORMAN OK 210 PM CDT WED MAR 30 2016 SEVERE THUNDERSTORM WATCH 59 IS IN EFFECT UNTIL 900 PM CDT FOR THE FOLLOWING LOCATIONS TXC035-049-059-081-083-085-093-097-113-121-133-143-151-181-193- 207-221-237-251-253-333-337-353-363-367-399-417-425-429-439-441- 447-497-503-310200- /O.NEW.KWNS.SV.A.0059.160330T1910Z-160331T0200Z/ TX . TEXAS COUNTIES INCLUDED ARE BOSQUE BROWN CALLAHAN COKE COLEMAN COLLIN COMANCHE COOKE DALLAS DENTON EASTLAND ERATH FISHER GRAYSON HAMILTON HASKELL HOOD JACK JOHNSON JONES MILLS MONTAGUE NOLAN PALO PINTO PARKER RUNNELS SHACKELFORD SOMERVELL STEPHENS TARRANT TAYLOR THROCKMORTON WISE YOUNG $$ ATTN...WFO...FWD...SJT...
originally posted by: TNMockingbird
a reply to: TechniXcality
Thank you handsome Texan!
(you know that's my pet name for you! LOL)
I really appreciate your early warnings as often is the case when Texas sees bad weather we are not far behind.
On occasion, especially in the Spring, the severe weather events travel straight up through Mississippi and Alabama and swing up through Memphis and on...
Sometimes, if a front is pushing hard enough downward from the North it can keep it to our South but then our Southerly neighbors are in for it. The storms are able to build and grow more severe.
I am up on a mountain, of sorts, and storms can easily fizzle out and we say "It couldn't make it up the West side of the mountain" but when they do...make...they are usually doozies. THAT'S a very technical meteorological term!