In using the tracking tool, I could see it being quite useful operationally if some things were added.  I would really like to be able to put in a freezing level height (or one derived from a model) and be able to track reflectivity above that level.  This would be a good way to monitor hail cores, better than the current method of just tracking a storm at a particular slice.

-Deitsch

CIMSS Prob Severe Product did a great job illustrating a developing severe storm over South Central Ohio.  The SVR PROB increased from 32% at 1840 UTC, 94% at 1856 UTC, then decreased to 69% at 1920 UTC.  The MESH increased from 0.64 in. at 1840 UTC to 1.78 in. at 1856 UTC, then decreased to 0.95 in. at 1920 UTC.  Normal Vertical Growth Rate rose from 0.87%/min at 1840 UTC to 1.00%/min at 1856 and 1920 UTC.  The Glaciation Rate went from 0.02/min at 1840 UTC, 0.03/min at 1856 UTC, to 0.03/min at 1920 UTC.

The MUCAPE was around 1500 J/kg and ENShear ranged between 38 and 43 kt. The change in colors from blue to red and expansion in width of the outlined area depicting the reflectivity core provides warning forecasters valuable information for making warning decisions.  A Severe Thunderstorm Warning was issued for this storm in the HWT.

Michael Scotten

Mike Smith and I tracked a convective cell cluster that was developing in the Allegheny Mountains of Virginia and West Virginia on Tuesday afternoon. We used the rapid scan GOES imagery to get a good look at developing overshooting tops and we were also looking for boundaries that could produce strong downbursts. At 1830Z, or 2:30pm local time, the surface observation data shows a buoyant environment to the east of the developing storm cells. The wind barbs also show a southeast flow in this area, and the obs to the west of the clouds were showing westerly and southwesterly winds. We were not able to look at radar data today in AWIPS as a verification tool, so we pulled up radar from the NWS’s site and looked at severe warnings as they were issued. This first image is from 1830Z, when the developing Cu aren’t looking too dramatic just yet. However, the GOES-R convective initiation product is showing a 90% probability for the middle Shenandoah Valley, indicated in red.

We decide to keep an eye on this area as the GOES-R CI was showing a strong signal for further development. In particular, Mike was looking for an outflow boundary to develop on the east side of this convective cell, which would produce a short-lived severe wind gust event. I was also following the northern edge of the clouds, in the area of the WV and MD panhandles. There was a large area of 60%-70% probability just to the northeast of the cloud. The cloud seemed to be growing in this direction, and I felt that having such a large area that the GOES-R CI was signaling on sort of increased the chance that something might happen in that area. I know that’s not the way the model is supposed to work, but larger spatial coverage just triggers higher confidence in my mind. So, I kept an eye on that area, as well.

Just 6 minutes later, at 1836Z, the CI product crashed down to an 8% reading for the cloud cluster in the Shenandoah Valley.

I wondered if this was an erroneous reading, or if the mountainous terrain might be challenging for the GOES-R CI algorithm. I know that the erratic percentage values are of particular interest in this experiment, so when I noticed that sudden change, it caught my attention. In the meantime, the yellow shading on the northern flank of the clouds has actually expanded in scope.

Skipping ahead about 45 minutes, the CI value has jumped back up in the cell in the Shenandoah Valley.

Just about 20 minutes later, a Flash Flood Warning was issued right over this area of erratic CI values. Later, it was confirmed via storm report that a creek overflowed its banks in the area. In the meantime, notice that the CI product has disappeared in the other area of interest in the WV/MD panhandles. At the same time, a SVR was issued for counties in West Virginia that are under that convective cloud shield. Later, a report of quarter-sized hail came in from the warned area, in Washington County, MD.

Obviously, the convective initiation product was not useful for the SVR development in WV because there was already convection happening in the warned area, hours before the storm became severe. It would have been interesting to see the ProbSevere product in this situation, to see if it picked up on any of the severe parameters, including MESH. Hindsight is 20/20!

The Overshooting Top Detection algorithm seemed to be poorly observing overshooting tops with pulse convection over the Mid-Atlantic States.  From both images (one at 2245 UTC and 2300 UTC), no overshooting tops were observed by the algorithm with the convection in western Maryland and northern Virginia.  A few tops were observed over West Virginia.

Convection through the day in West Virginia has been strong, perhaps marginally severe at times but no reports have yet been received.  However, I noticed the probsevere tool began to struggle once this convection congealed into a linear segment.  The highest probs appear to be driven by a falsely high MESH value, which was at 1.41 inches at this time.  There was no satellite data going into the probsevere tool at this time.  Looking at reflectivity data, the bulk of the reflectivity (60+ dBz echoes) were below the freezing level, so I’m not quite sure why the MESH was so high.  But this tool was definitely overdone in this instance.

-Deitsch

In this image from 2158z over southern South Carolina the ProbSevere model highlighted an area where there was hardly a cloud in the sky. The readout shows a 78% prob of severe storm with 1600 J/kg MUCAPE, 2.1kts of EBShear and MRMS MESH of 2.08 inches.

Talking with the developer of this model, he indicated this is a known problem associated with QC of the MRMS MESH data.

Shawn Smith

Simulated satellite imagery did not perform too well today on May 13. The simulated imagery seemed to be too slow with the development of storms over the Great Lakes, and depicted too much convection across the Mid Atlantic states at 2200 UTC (second image).  Deep moisture indicated by water vapor satellite moved east faster than simulated.

Michael Scotten

Click the image for an animated loop of GOES East visible imagery between 16z and 1745z along with the Convective Initiation product.

The color scale on the convective initiation product has been adjusted to three colors to simplify identification of the various probabilities. Blue is a 0-30% probability, Yellow is a 31-70% Probability and Red is 70% to 100%. I feel this helps to show increasing probabilities better than the standard multi-color scale. In the looping image notice the outlined area over eastern W. Virginia to the west of the Shenandoah Valley. Watch how the CI product shows increasing probs starting at 1615z along a ridge top 30 to 45 minutes before a line of thunderstorms exploded along the ridgeline. This product also highlighted these storms about 3 hours before a Satellite Precipitation Estimate message was issued by NESDIS. (1907z)

Shawn Smith

This post shows how the Nearcast model did well in depicting a weak north/northwest moving boundary that initiated convection in southwestern WV.  In a rather “pulsey” environment, the ability to pick out this boundary aided in confidence as to where convection was going to form.  Definitely a good tool to use in conditions where forcing is subtle and there is uncertainty on location on CI.

-Deitsch

CIMSS NearCast 780mb Theta E product depicted decreasing values from 15 UTC (first image – around 329 K in NW OH) to 19 UTC (second image – around 327 K in NW OH)  on May 13.  Storms seemed to decrease in coverage and intensity 18-20 UTC in NW OH.  The decrease in mid level moisture around 780 mb may have caused the decrease in storm coverage and intensity. The GOES Vertical Theta-e Differential Mid-Low product showed an increase 15 to 19 UTC from -5 K to +1 K, which may have helped to cause the decrease in storm coverage and intensity.

Michael Scotten