EWP Blog

GOES-R/CIMSS CAPE values continue to increase across southeastern portions of the Albuquerque, NM, area towards the southwestern portions of the AMA CWA. Values are not markedly high, on the order of 400-500 J/KG, but skies continue to clear in the wake of convection earlier this morning allowing for greater destabilization later this afternoon.

The UAH GOES-R convective initiation probabilities continue to also increase for southeastern portions of the ABQ CWA and southern portions of the AMA CWA. Reflectivities remain weak moving northeast in the southern AMA CWA, but expect coverage to increase as the storms move into the more favorable environment.

Brick Tamland

I’ll be starting out the day in ABQ. There is a short wave rotating through the region and convection has already fired off the higher terrain and is moving towards the NE. The GOES-R LAP CAPE and LI are enhanced in this area.

Interestingly, there has been very few CG lightning strikes with the stronger cells.

Time to go load up more data.

-V. Darkbloom

Briefing and water vapor loop showed short wave crossing north central New Mexico. Drying on Water vapor loop lines up with the clearing on the leading edge of the short wave. Better indications of CI in far sw CWA. CAPES have increased to near 1100 J/KG just south of the forecast area. Have DTA  set up and awaiting the next pass for NUCAPS availability.

Lynford

My warning operations will focus over the Lubbock CWA this afternoon.  Clearing of this morning’s cloud cover began to occur around 1830 UTC.  A cumulus field has quickly developed in the areas which cleared.  I will be watching the GOES CI Probability in this region as instability continues to increase.  GOES LAP CAPE values through the CWA range from 500 to 8000 J/kg, with some spotty areas of up to 1100 J/kg.

Looking at the Convective initiation product over southwest Kansas in an area where the earlier cirrus had cleared out showed some enhanced probabilities in the 60-70% range at 2000 UTC over Hodegman county, KS.

At that time there was not any radar returns showing up in that part of the county where the CI was identified.  When looking at the radar imagery at 2045 UTC there was new convection that had developed across northeastern Hodgeman county.  I think this is a great example of the benefit of the CI product and how it does especially well in environments where only cumulus cloud development is occurring.

I think this can be a very useful product in the WFO, especially in offices where pulse convection can be a problem, such as the eastern United States.

Jack Bauer

Just another brief example of using the GOES-R Convective Initiation Algorithm.

Convection did indeed initiate soon after, becoming severe by 20Z. There were several reports of golf ball sized hail associated with this storm between 20Z and 22Z.

As of  2312Z this cell is still going strong. A pair of weak cells has popped up just to the south and the CI algorithm is showing two more 80% areas with these cells.

We’re about to start wrapping up for the day, but it’ll be interesting to see how these cells evolve over the next 30 minutes or so.

-V. Darkbloom

The time series lightning plot for the 3rd SVR in Topekas area is below. Note the peak close to 125 flashes/min around 2245Z which coincided with another hail core development aloft, 60 dBZ to around 22k ft/-25 C. This area is also tricky because it at the western tail end of a line of thunderstorms, so the centroid designation may be off since it is close to several other centroids, thus skewing the point values.

Brick Tamland