Starting the day in ABQ

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

Pre Storm Environment

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

Lubbock CWA Conditions

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 1000 J/kg, with some spotty areas of up to 1100 J/kg.

Daily Summary: Week 1 Day 1 (May 4, 2015)

Today marked the first day of the EWP Spring Experiment in the Hazardous Weather Testbed in Norman, OK. This year, 5 NWS forecasters and 1 broadcast meteorologist will evaluate various GOES-R and JPSS algorithms, as well as Earth Networks total lightning products. Participants, working in pairs, will use the experimental products to issue area forecast discussions and severe thunderstorm/tornado warnings for their designated CWA. All of the products being demonstrated are available in AWIPS-II.

Much of the focus for the first day of the week was hands-on training for each of the products under evaluation. After some initial familiarization with AWIPS-II and procedure building, the various PI's worked with forecasters on how to interpret the products, and what to look for during the week. Forecasters also became familiar with saving images, and posting to the blog. By the end of the day, participants had already made several informative blog posts.

We began today's operations in the Topeka, Omaha, and Midland CWA's. As activity subsided in the Omaha CWA, that pair moved operations to the Wichita CWA. Participants were able to utilize all of the products today, including the PGLM total lightning from the West Texas LMA.

Tomorrow, we will start activities at 12:00 pm in the Dev Lab for the daily debrief before moving to the HWT for the 12:45 EFP briefing. Operations will likely take place in West Texas.

- Bill Line, SPC/HWT Satellite Liaison and Week 1 EWP Coordinator

Feedback from Daily Debrief:

GOES-R LAP products
- I looked at CAPE and TPW mostly
- DCAPE would be helpful to have, if possible
- The gradients in these fields were most helpful, not so much the absolute values.

NUCAPS
- I liked it and thought it was useful to have today. My office is in between RAOB sites, so it would be nice to have this additional environmental information.
- It would be nice to have automated surface modifications so that I don't have to waste time doing it myself. It is too time intensive, especially during warning operations
- I would like QC flags for each of the individual soundings to know which ones I should trust most.

GOES-R CI
- Today, I used it moreso after the fact
- There were a couple of cases where it worked well. One exampele was an 80% probability, and those cells blew up an hour or so later.
- In Topeka, there were a lot of thicker cirrus, so it was not effective.
- Further to the south in Oklahoma, it did well. 80% probabilities continued to develop into convection
- The display covered up too much of the imagery that I wanted to see.

ProbSevere
- I liked the readout, seeing the various fields was helpful.
- It might be a good idea to include Dual Pol fields in the future, specifically ZDR.
- In my situation, cells were pretty small, so I wish the contour had been a little thinner in this case as it covered up too much of the cell. I made it transparent so I could still see the cell.

Lightning Jump
- Of all the ENI lightning products, I found this to be most useful. It was easy to use, it broguht my attention to the relevant storms, and showed transitions in intensity.
- I had one situation where lightning increased rapidly with a newly developing storm, but no jump was recorded.
- It was pretty successful in indicating rapid intensification.
- I liked having it as a confidence booster.

Convective Initiation in Southwest Kansas

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

Another CI Case

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

CZ (left) and GOES Vis and CI (right) at 1830Z. The orange areas show 81% probability of CI.

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

Lightning Jump and Cell Intensification

Another significant lightning jump occurred in west Texas (Midland CWA) around 2134Z (434 PM CDT). The jump was 4 sigma - shaded red below.

 

A time series reveals this was the first in a series of jumps.

The second jump around 22Z was 2 sigma. A loop of the 0.5 deg reflectivity shows the cell intensifying after the lightning jumps occurred. The max Z at the 0.5 deg tilt increaed from around 63 dBZ to around 71 dBZ in 8 minutes, or two volume scans.

(click image to animate)

In this case, the lightning jump is a good indicator of imminent storm intensification.

-V Darkbloom

All set up

Procedures and perspective displays set up. Time to start watching current storms.

Warned on this storm with a 5 sigma lightning jump. It appears to be a right-mover. 

Lynford

3rd SVR for TOP area

3rd severe warning for a hail core over southwestern Ottawa county, moving northeast. Lightning Jump Algorithm jumped over 4 sigmas around the time when the hail core aloft looked the best. ProbSevere jumped from 69% to 92% with MESH building to over 1.50 inches. DTA came out well in advance though it overlaid with a 2nd, more appropriate DTA, related to the more intense storm approaching from the south. Although fairly large area of 60 dBZ above -20 C, and MESH at 1.50 inches, only used 1 inch hail in warning due to lack of large hail reports during the afternoon.

Brick Tamland

A Limitation of Prob Severe Algorithm

While observing the Probability of severe throughout the event today, I have noticed that it seems to do well when there are discrete or individual convective cells and was useful in the warning operations when combined with the base data we were looking at interrogating the storms.  The storm we originally warned on seen in the image below had high prob severe values and verified with a 60 mph wind gust report.

However, later in the event the convection became linear and looking at the base data interrogating the storm there was not evidence supporting a warning along the line as the 50dbz cores were relatively low and the line of storms had become outflow dominated with the outflow boundary pushing well away from the storms.  The probability of severe though was showing values near 85% along the entire line.

So I think it is important to note for the users of this product that when the convection becomes linear the probability of severe may not be as useful and should not be as relied on compared to individual convective storm environments.

Jack Bauer