Category: Live Blogs

Real-time posts made during testbed nowcast and warning operations.

GLM Assist In DSS

Posted in Forecaster Thoughts, Live Blogs, News on by Michael Bowlan.

The below image shows GOES-16 day cloud convection (DCC) beneath GLM Minimum Flash Area (MFA). Point F is a DSS event. DCC shows clouds glaciating a county upstream of our DSS event, with the storm becoming electrified shortly after glaciation per MFA. This prompted a call to the emergency manager providing support for the DSS event letting them know that lightning was imminent.

ENI total lightning also shows lightning (white points), but the point data fails to show the extent of the lightning, which may lead decision makers to think that they have more time to react to the approaching lightning than they actually do.Sandor Clegane

GLM MFA for Storm re-generation

Posted in Forecaster Thoughts, GOESR, Live Blogs on by Kristin Calhoun.

GLM Minimum Flash Area showed some utility in boosting lead time for storm re-generation. The storm in the center of the first image had started to weaken a bit after moving off of the outflow boundary that initiated it.

The storm continues to show no new updraft development in the sat imagery as well as MFA product.

At 20:29 GLM MFA begins to indicate that there may be a new updraft forming as it interacts with a differential heating boundary/outflow from the leading storm.

Over the next 20 minutes the updraft continues to strengthen as the storm becomes more robust. The MFA led the visible satellite depiction of the new updraft by 2-4 min. This could be useful when trying to decide whether to continue warnings or not.

 

 

 

Revisiting the AllSky Products

Posted in Live Blogs on by Michael Bowlan.

Went back to do a broader-scale mesoanalysis and noticed right away that storms are initiating right along the southwestern extent of a moisture/instability gradient, and following a SW to NE gradient between two areas of higher PWATs/CAPE, as depicted on the middle image below (reflectivity overlaid on AllSky CAPE). Just focusing on the trend aspect of these products is very useful in determining where storms may continue to develop and roll. I attempted to look at the merged TPW product, but unfortunately, the data I have is almost an hour old by the time of these screenshots, and the lower resolution isn’t as easy to work with in comparison. It’s possible the values of the TPW product may be closer to reality, but gravitating more toward the tendencies of the current state of the atmosphere found in the AllSky products seem to be more useful for this purpose.

~Gritty

Merged AzShear in West Texas – Large Distance from Radars

Posted in AzShear, Live Blogs on by Michael Bowlan.

Looking at the Merged AzShear across West Texas the issue of how many radars are taken into account when calculating different MRMS parameters. You can see the SRM from KMAF, the closest radar to the storms. These storms are rotating in the mid-levels but the radar is looking between 10,000 and 16,000 feet depending on which storm you reference. The Merged AzShear is pegging the storm storms where the circulation is evident, but the question is since KMAF is closest is the AzShear product taking in more than one radar? If it is all the other neighboring radars (KEPZ, KDFX, and KSJT) are all as far or farther away, which means they would be looking even higher in the storm. The image below shows how far the radar are from the ongoing storms.

  • Alexander T.

 

SJT MNDA

Posted in Live Blogs on by Kristin Calhoun.

Primary area of interest on this storm is the western-most mesocyclone highlighted by the NMDA. Unfortunately, the NMDA identifies this rotation with several different names, making it difficult to track through time.Sandor Clegane

More Lightning Analysis…

Posted in Live Blogs on by Michael Bowlan.

So far, the MFA is following the previous logic of using it as a way to identify vigorous updrafts. Below, the progression in a 15-minute period follows that correlation between the smaller flashes increasing in area indicating a strengthening cell(s). However, I could see its utility degraded in a larger-scale multicell environment with clusters close together, especially as the areas of smaller flashes increases, given the low-resolution of the grid itself. As for Total Optical Energy (TOE, at the bottom), I think there is benefit in using this product as well to monitor trends, but I had to use a different color curve for it to stand out to me more (last animation, below).

~Gritty

2146Z:

2155Z:

2200Z:

TOE Loops:

AllSkyLAP – CAPE vs Radar

Posted in Live Blogs on by Kristin Calhoun.

Easy display for SA is to plot radar (Z) over the AllSkyLayer CAPE.  In this case – storms are moving off slowly to the NE – in an area of similar CAPE values.  With expected cloud cover, further destabilization is not anticipated.  Thus, would expect storms to remain at current levels – or perhaps slowly intensity.  Would need to be monitored – but “rapid intensification” is not expected.

NUCAPS – PopUp SkewT – Needs Improvement

Posted in Forecaster Thoughts, Live Blogs on by Kristin Calhoun.

One way to increase NUCAPS sounding data usage is to improve the ability to display “mouse over” soundings using the PoP-Up SkewT.  See the example below – I was able to mouse over the various points and display the NUCAPS soundings.

However, the PoP Up SkewT display is small, crude, and cannot be enlarged.  If a version of NSharp could be integrated into the PoP Up SkewT (e.g. larger SkewT with thermodynamic variables below) – then forecasters might use it more often.  The current PoP Up SkewT is probably 10 yrs old – and needs improvement.

SJT Mesoscale Update #2

Posted in Live Blogs, Mesoscale Discussions on by Kristin Calhoun.

NUCAPS retrievals  became available around 21z, so I decided to do a new mesoscale analysis. I wanted to know about the air in the warm sector that the storms will likely be ingesting. The first retrieval I looked at was the southern-most green dot in the eastern most MUCAPS swipe. The sounding in this retrieval came in with a surface temp about 20 degrees cooler than the observation, so I’m thinking this retrieval is either being contaminated by ongoing convection or actually sampling north of the warm sector. The retrieval just to the south of that had surface temperatures more reasonable, and the associated skew-t is shown below.After a quick adjustment to the lowest points on the sounding, this clearly looks like a severe weather sounding. I’m hesitant to rely on CAPE estimates given the dependency on the boundary layer, but indicies more reliant on mid level obs (LI) are still indicative of strong to severe storms. This compares well to all-sky LAPS retrievals (above, right).In typical operations in which I do not have access to these products, I would rely on the SPC mesoanalysis (below) to estimate instability. The NUCAPS and LAPS All Sky retrievals do somewhat increase my confidence that the mesoanalysis is close to reality. However, Given my conceptual model of how the atmosphere should be behaving, I was already highly confident that the atmosphere is quite unstable in the warm sector, so the increase in confidence from NUCAPS/LAPS is somewhat limited.Sandor Clegane