Tuesday, June 9, 2015

High CI in an area of showers

Watching the CI values along a line of weak showers, the 1945Z image popped up an 83%. The corresponding radar image out of FGF showed nothing more than a weak thunderstorm in the area with only one lightning strike detected (not displayed)




Fast forward to 2000Z, the higher CI values (71%) have moved westward along the line. This makes sense as the line of weak showers/thunderstorms continue to build west. There has been no further development of cell that had the earlier flag of 83%.




Fast forward even further to the 2015Z images. The CI output disappears and the corresponding radar image shows no further development.




-Shasta

SRSO showing marine stratus over SE coast of New England

The GOES SRSO imagery from 1848-2015 UTC shows the influence of the cool onshore flow with marine stratus holding on the southeast coast of New England from Groton, CT (KGON) to Providence, RI (KPVD) to Marshfield, MA.  Just to the north of that region the smooth texture of the marine stratus changes to rolls/streets showing us where it might be possible to convection to develop. MrSnow/inthecards


Rapid City Meso Discussion Charley

Moving to a high CAPE and DCAPE environment.  SPC Meso analysis has 5000/1700 for each.  Near cast model shows the region is fairly unstable.  Area under clear skies now.  12Z sounding had 12 kft freezing level as well as 8500 wbz.  PW of 0.67 is dry.  Have some cu over western Pennington that is blowing up now.  Seems region is unstable.  CI had a high value just before that cell went up.





The yellow area above did not blow up, but the next image below did go quickly…see following image as well.



CI Increasing – Small Area of Showers and Storms Develops

CI accurately depicted increasing chances for showers and storms across western MN this afternoon, with around 30 minutes of lead time with regard to the developing convection.



-Wacha

NUCAPS sounding over MA




We were able to retrieve a NUCAPS sounding in a relatively clear area…at least looked the most free of high clouds in the area. I manipulated the surface conditions to closer match those at the surface and came up with somewhat similar values of CAPE to what we where seeing on the SPC mesoscale analysis…a little higher than what was on the GOES-R LAP Algorithm cape.

NUCAPS Update Charley




Had a NUCAPS sounding in a clear spot over the area.  CAPE was higher than LAP data indicated, with a surface adjustment to 77 degrees over 66 dewpoint.  Freezing level is fairly low at ~10 kft, so will be watching for hail growth.  DCAPEs around 500, similar to SPC mesoanalysis.

In addition, ALB did an 18Z sounding.  Shows CAPE not as high as my estimate, and freezing level a little higher as well.

SPS 1 Charley

SPS for Litchfield county.  Saw this cell earlier get a CI blip of 60-70%.  Cell moving to the left of the mean flow.  Not overly tall yet, but growing faster than other parts as it merges into the line to its west.  Will have to watch to see if this one gets more organized.




DLH – AREA FORECAST DISCUSSION

Weak disturbance moving through the forecast area currently resulting in little more than cloud cover at this time. Behind that shortwave, skies are relatively cloudless across the western boundary waters in northwest Minnesota. This clearing has allowed temperatures to quickly jump into at least the upper 70s, lower 80s in some locations. A corridor of higher dewpoints were noted along eastern North Dakota with values commonly in the low 60s. The result is that SB CAPE values are >1500 J/KG, but a weak mid-level cap exists. Hi-res near term models indicate that this corridor of higher dewpoints will remain ahead of the front and push eastward into the CWA by 23Z. This will help fuel whatever convection does develop. To balance the moderate CAPE values, 50kts of deep 0-6km shear were noted. Freezing levels are about 12kft, so hail does seem plausible with stronger cells, but the inverted v shape to the soundings indicate that this may be more of a wind threat. SPC has a slight risk issued for the area including a 2% tornado area.

Agitated cu field beginning to develop along and ahead of the cold front nearing the Canadian/ND/MN border. While we don’t have access to the 1min super rapid scan, we have noted some expansion of the cu field over the last 45mins. The Convective Initiation Product returning a modest 10-27%, but even those numbers have started to increase over the last few scans. Looking at the total PW values sampled by the GOES-R LAP algorithm, values do seem consistent with the numbers from the SPC Mesoanalysis Webpage. However, the 18Z Total PW has shown a few bullseyes of values >1.4″ coincident with the aforementioned cu field.

Shasta/Wacha

CI product 1845 BOS





CI product showing 58% chance of development at 1845Z in the western portion of our CWA



By the 1908 frame here on the box radar you can see that development has continued to occur in both areas that it showed the 50% and the over 70% to the SW of BOS CWA, here a new storm cell developed in front of the area. Here is the loop.


Charley Warning 1





Not much lightning with this cell, and jump was not there.  Wind signature on radar above as well as refl. is bowing out indicated a need for a quick warning here.  ProbSevere not useful here, as line has been ongoing for awhile.  Line was over an area of higher CAPE as well as lowering LI, around -5.