Initial Impressions

Very impressed with the Octane CTC product. This loop is probably a bit too fast. But It captured and area of rapid cooling east of Perry Park

At that time radar was not picking up on much at all.

20 minutes later the cell really took off with a deep core of over 60dbz reaching above -20C (panel in the top right)

While the storm was pretty vertically stacked there low ZDR and lack of melting near the surface likely lead to hail production. The fact that the CTC ID’d the area before any signal on the radar is very impressive.

The other thing that caught my eye today was the WVT Ratio. After playing around with the color map ranges I was able to tease out the moisture feed streaming into the Front Range. Overlaying this with observations matches the overall surface streamlines well. Would be very interested to see this in a dry line set up.

IsthataTOR

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Dry Signals in Synthetic GeoXO

Today’s setup featured a typical high plains return flow pattern with low-level moisture upslope evident on surface observations and both the synthetic WVT & 5.15um channel imagery. One feature that caught my attention initially in the synthetic imagery was a dry pool over the Cheyenne Ridge, spanning from Weld County, CO up into Kimball County, NE (highlighted with yellow circle in the image below).  Observed surface dew points in this area were in the mid to upper 40s in southeasterly flow, likely on the leading edge of the plume of higher moisture in KS and CO. I did not see this level of detail on any other satellite imagery.

With this feature, I was curious on two fronts: the placement of this feature compared to reality, but also how would this dry pool affect convection later in the day. Compared with surface obs, the dry pool seemed to be slightly displaced to the east from reality, but not by far.  My gut was telling me that convective initiation on the Cheyenne Ridge itself would be nil due to the dry pool (perhaps with a hint of subsidence?), and that any established convection moving through the drier air would not exhibit explosive growth and would overall be weaker, and/or perhaps we’d see an enhanced downdraft wind threat.

See below the loop of synthetic imagery highlighting the 5.15um imagery that covered the majority of our test period. Reality played out pretty close to the evolution of convection as seen in the loop. A left split fired off the mountains near Fort Collins and persisted northeast up into Wyoming. This storm produced severe hail slightly larger than quarter size in Cheyenne, but then appeared to weaken on visible satellite as it progressed further east-northeast along the Cheyenne Ridge where the drier air was forecast to reside.

This case shows the utility of highlighting moisture content, or lack thereof, that you cannot necessarily see on traditional satellite imagery.

Astrophage

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Overview: Week 3, Day 1

Week 3 kicks off today and the ridge that stymied us in week two is….still there! Thankfully we’ve recovered a good bit of moisture across the plains and southeast for convection to work with. We began today with product introductions and an orientation session, followed by our forecast discussion to decide where we would target today. The forecast was pretty clean cut, with two options of elevated convection in NE Colorado/SE Wyoming and additional convection from a remnant MCS across Mississippi/Arkansas. Based on timing of CI, instability in the high plains, and the size of the MesoAnywhere domain, we decided to localized to the NWS offices of Cheyenne, WY (CYS) and Boulder, CO (BOU).

 

1 PM
SPC issued an MD just before operations began for our area, citing thunderstorm development and a high chance for a watch to be issued later. And by 2pm we had a watch!

In the CYS office, forecasters looked at synthetic GXI imagery and identifying the moisture advection northward into their CWA later in the forecast period. This also led to the discovery that a few of the procedures had ‘inverted’ color maps for WVT. While not intended, we did compare how they looked from each color map. Which is better? You decide!

Original colormap. Dry air/clouds are white, moisture is dark.

‘Flipped’ color map. Dry air/clouds are black, moisture is light.

First impressions of SZA from this morning’s imagery was positive with forecasters in both the CYS and BOU offices. A forecaster with experience in AK said they regularly adjust brightness of visible imagery on the fly, especially in lower light seasons. A forecaster with more experience in the central plains said they rarely adjust the brightness. Some of the areas we examined included over Colorado and Montana. Forecasters mentioned using the DCPD RGB frequently, and having more time with that imagery would be welcome. Additionally, one mentioned liking that the colors stayed more consistent throughout the day.

Forecasters in the CYS office compared LightningCast v1 and v2 from GOES-East and GOES-West along with the timing of the first lightning flash. V2 introduced more heterogenety in the bands, while V1 appeared fairly uniofrm and more widespread. Also LightningCast v2 seemed to be ahead of v1 for thunderstorm growth over the Denver metro.

3 PM
Both offices issued severe thunderstorm warnings for severe wind and hail hazards. Looking ahead, we have a steady stream of SLGTs this week, so we should stay fairly active. Also wanted to noted the CYS radar was out today, so some questions about using Sat data (especially things like OCTANE) for warnings are of interest for the morning discussion tomorrow.
-Kevin
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LightningCast and Stoplight Chart Comparison

Today I tried to focus on the LightningCast and Stoplight Charts by comparing them. I noticed that in the case of lightning approaching, the probabilities on the dashboard went up. While version 2 in Figure 1 shows a blip around 20:15z, this was validated by a storm up to the north of the Airport which had lightning near 10 miles of the site. Version 1 had more of a persistent gradual increase which began sooner than Version 2. Version 1 would have most likely given more of a lead time than a quick ramp up.

Figure 2 represents the same timestamp as Figure 1 and shows the lightning increasing in coverage as storms approach. Figure 3 is a screenshot of the current lightning and LightningCast probabilities. The Stoplight Chart did very well with the area that the lightning was occurring.

Figures 4-6 show similar images but this time as the storms passed by. One thing I noticed was the LightningCast probabilities dropped off dramatically while lightning was still around the area. The lightning Stoplight Chart, in my opinion, handled the ramp down better with a more gradual end to the lightning.

So, it was interesting to see that both of them did fairly well ramping up lightning probabilities which increases confidence in forecasting and giving lead time for lightning DSS. However, there was a noticeable difference with the end time since the Stoplight Chart kept showing red over the area, meaning lightning was either nearby or occurring whereas the LightningCast rapidly dropped probabilities.

Overall, they both did well and they were both useful with lead/end times of lightning.

Figure 1: KAMA LightningCast ramped up the probabilities before lightning occurred.

Figure 2: Lightning Stoplight red boxes approached the 10 mile ring as lightning was approaching.

Figure 3: LightningCast showed the probabilities of lightning pretty well as lightning was occurring and approaching the site.

Figure 4: LightningCast ramped down the chances for lightning very quickly as storms passed.

Figure 5: Lightning Stoplight Chart kept lightning within the ring as storms passed.

Figure 6: LightningCast on AWIPS ramped down lightning very quickly as storms passed.

-Batman
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SPG Blog Post Day 4

Today’s Set-up: Strong low pressure system moves through the region, with associated cold front. Slight risk over northern Texas, Oklahoma panhandle, and western Kansas. I was simulating the Dodge City office today. Their primary threats were severe wind gusts from an incredibly deep inverted V sounding, and some possible small hail.

 

 

Figure 1: LightningCast Viewer

 

  • Got more experience with the LightningCast dashboards. I got the events pulled up fine, and I found myself pulling the dashboards up to get a quick visual on trends, and which site was more at threat.
    • This helps me, as a forecaster, get an idea on which event needs to be notified before the other. AKA – which event is the priority, based on the ongoing weather.
  • I explored some of the options that you can overlay on LightningCast viewer
    • Having METARs pulled up is VERY helpful for getting some ground truth to what I am looking at on satellite and radar.
    • I also appreciated having the SPC outlooks overlaid in the back, to have a quick guide for where is favorable for severe weather.

 

 

 

 

Figure 2: GXI-ALL Procedure

 

  • On a day like today, with a pretty strong frontal system and dry air in a lot of places, the GXI products worked well at highlighting the moisture ahead of the front. You can pretty clearly see the boundary moving through the CONUS.
    • I did not get much help when looking at the CWA level view, but looking at the “big picture” CONUS view was significantly more useful for me in operations today.

 

Figure 3: CONUS Octane Speed Product
  • This image was earlier in the operations period, and I thought it was interesting to see that the speed was all relatively uniform. We’re used to looking for plenty of speed and directional shear in severe weather, but here most systems were moving around 30kts or so.
Figure 4: CONUS OCTANE CTC
  • I took a peek at cloud top cooling for some of these storms, and they were very cold (~-55C).
    • I saw that the office to the south issued warnings based on that (shoutout!) and I looked into it a bit more, and realized we had even colder cloudtops. After radar analysis and further satellite, along with trying to find some ground truth, I put a warning out for the eastern portion of the CWA.

-Kelvin-Helm

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High-based convection over western Kansas Blog Post

On the last full day of the Hazardous Weather Testbed, we monitored convection over the Dodge City (DDC), KS County Warning Area (CWA). We were responsible for issuing convective warnings and providing IDSS to two mock DSS events, the Sunflower Balloon Festival near Dodge City, and the Emerald City Oz Festival in Liberal, KS.

The near thermodynamic environment over the Dodge City, KS CWA was characterized by moist mid-levels atop deep, well-mixed boundary layer profiles and steep low-level lapse rates as sampled by the special 18Z DDC sounding. The sounding revealed modest CAPE values around 766 J/kg,  but also significant CINH values of over 400 J/kg. See image below.

Figure 1 above: 18Z DDC RAOB showing a classic inverted-V sounding.

While numerous thunderstorms developed across southwest KS, most of the storms remained below severe levels with several wind reports between 38 and 47 kt, likely due to the combination of the inverted-V thermodynamic environment and gradient winds. See Figure 2 below.

 

Figure 2 above: LightningCast V2 & Stoplight combined procedure showing numerous thunderstorms affecting southwest and south central KS.

 

Figure 3 above: shows the Fire channel (left) and the Fire Temperature RGB (right). Around 2016 UTC, GOES-East CONUS 5-minute imagery detected a fire south of Richfield in Morton County in southwest KS. The Fire Temperature RGB showed some white pixels at times indicating that this fire was having a strong heat signal in all of the three channels in this RGB indicating a very hot intense fire, this despite being obscured intermittently by mid-high level clouds.

Figure 4. A VIIRS pass around 2021 UTC also indicated an intense fire in southwest KS with energy being emitted in the 101 to 350 Mega Watts range.

Overall, this was a day of dangerous fire weather conditions with dry thunderstorms producing marginally severe wind gusts. It is possible that this fire was ignited by lightning. Red Flag Warnings were in effect for southwest KS and the OK and TX panhandles.

-Hurricane Specialist

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Overview: Week 2, Day 4

10AM

Thursday began with another group discussion, focusing on the following topics:

  • When to give the ‘all clear’ using the Lightning Stoplight tool
  • The limitations of satellite imagery and OCTANE-CONUS products on days with lots of convective anvil debris overtop developing convection, obscuring signals of stronger updrafts.
  • Playing with the color bars for the WVT product and finding what ‘works’ for showing different moisture boundaries like dry lines and sea breezes.
We played another round of ‘When does the satellite imagery become useful/useless?’ with the SZA imagery. This time we viewed a sunrise over the Mid-Atlantic with the 0.64 µm (ABI Channel 2) visible band, and forecasters stated when the imagery became useful. Here’s the results…
  • SZA Imagery: 0956 Z (x3), 1006 Z
  • Traditional Imagery: 1026 Z (x4)
SZA Imagery

Traditional Imagery

After a full week of MRGL and SLGT events, we were rewarded with…another SLGT! Surface moisture and instability was difficult to come by over nearly the full CONUS, and we relied on moisture transport from the Pacific front and sub tropical jet. Oddly enough this was positioned behind the dry line, which led to some large inverted-V forecast soundings and downburst potential from elevated thunderstorms. The 1630Z SPC convective outlook had a Slight Risk in the Central and Southern Plains, driven by a 15% CIG1 risk in SW KS and the TX panhandle. We decided to localize to the Goodland, KS (GLD) and Dodge City, KS (DDC) NWS offices today (Note: Later GLD office moved to Amarillo).

1 PM

Early on forecasters sent DSS messages to their mock events and waited for convection to develop. In the GLD office some convection tried to form in far-eastern CO, but dissipated and was unable to sustain itself. OCTANE-CONUS CTC showed low cooling values (<10C) and LightningCast was showing lower probabilities. Conversation moved to the Synthetic GXI imagery, and observing the moisture from the mid-level jet across the Southern and Central Plains. The group compared the 5.15µm Synthetic GXI band with the ABI 7.34 µm (Channel 10) IR band designed for ‘Low Level’ water vapor.

3PM

Decided to move the GLD office to Amarillo (AMA) after observing minimal instability in their CWA, and a more agitated cu field on the western edge of the AMA CWA. SPC also issued an MD and subsequent severe thunderstorm watch for the DDC and AMA forecast areas, which reinforced our thinking that convection would be focused further south during our forecast period.
4PM
After some discussion with the DDC forecasters and some developers, we made vis-IR sandwich procedure that mimicked the ‘oops all Day Cloud Phase Distinction RGB’ procedure. The motivation was that once convection gets going, forecaster may liked to transition away from the DCPD RGB and to imagery with more direct visible and infrared information.

5PM

At the very end of the day, we talked about the SZA imagery some more and its applications for OCONUS users in places like Alaska. While roaming the CONUS comparing SZA and traditional imagery, a developer pointed out a large blowing dust event in ND, which was evident even in the DCPD RGB, along with the Channel-2 visible imagery.

That’s a wrap for week 2!

-Kevin
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Cloud Obstruction with Octane Products

A cold front swept across Western Pennsylvania and Northern West Virginia with a line of strong to severe thunderstorms that produced hail and wind damage. One thing to note about the Octane Cloud Top Cooling (CTC) imagery is that the anvil cirrus masked other storms in its wake. This might be a limiting factor for the Octane imagery, especially in linear storm events.

Figure 1: Anvil Cirrus was blown over other storms to the northeast and masked some overshooting tops/cloud top temperatures.

Shortly after, we noticed a similar problem so we then looked at the Octane Speed and Direction products in the mesosector. It is easier to make out the individual updrafts in these products as they appear less washed out and more defined. In this case, you can see 2 separate storms, one near Hundred, and one near Blacksville. These produced wind damage in northern West Virginia.

Figure 2: Octane Direction imagery in the mesosector.

Figure 3: Octane Speed imagery in the mesosector.

After seeing the initial problem, we changed the color table slightly in order to see if we can mitigate the masking issue. I personally like this color table more than the original but it still has the issue of masking other storms under the anvils. It is definitely easier to see individual storms but not as easy as the Octane Direction/Speed products.

Figure 4: New color table for the Octane CTC product.-Batman

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Severe Weather over western Pennsylvania

On Day 3 Wednesday of the Hazardous Weather Testbed, we monitored weather for the Pittsburgh CWA (PBZ), and in particular lightning and severe weather that could affect the Pittsburgh Mimosa Festival and the Allegheny Caribbean Carnival. We issued several SVRs that ended up verifying with multiple hail reports of 1.0” in diameter (quarter size) and a few damaging wind reports in northern WV. See SPC reports further below.

The main radar products that were used for severe weather decision making were the 0.5° Base Reflectivity and Base Velocity products, the MRMS @-20C, Vertically Integrated Ice, and MESH. LightningCast V2 and Stoplight V2 were also used to support DSS activities at the two festivals mentioned above. At the beginning of the event at 18Z, thunderstorms were already impacting the two festivals as seen on the Time-Series plot of LightningCast with observed GLM flash counts and near 100% lightning probability at the exact locations.

Figure 1 above shows the probability of lightning at the location of the Allegheny Caribbean Carnival from LightninCast V2 (green line) and the observed flash counts from the Geostationary Lightning Mapper (GLM) instrument. Notice that the second spike in lightning probabilities did not result in lightning activity detected at the exact location as shown by the lack of GLM flash counts. In this second spike in lightning probability, the LightningCast V2 had a small false alarm than the V1 product.

 

Figure 2 above shows the Pittsburgh Mimosa Festival experienced two rounds of thunderstorms, one between 18Z and 19Z and a second round between 1945Z and 20Z.
We also monitored the Stoplight V2 product to give the all clear message that the lightning threat had ceased.
Figure 3 above shows the Stoplight product indicating the cessation of lightning and when it was good to give the all clear message that activities could be resumed.

Figure 4 above shows the MRMS Isothermal Reflectivity product @-20C which often shows the most significant storms and the storms that might contain hail alongside the Vertically Integrated Ice. SVRs polygons are also shown to indicate where SVRs were issued.

Figure 5 above shows the SPC’s Severe Weather reports from Wed May 13 2026. Four hail reports of quarter size were reported in western Pennsylvania and three wind damage reports in northern WV.

-Hurricane Specialist
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OCTANE Cloud Top Cooling with Shallow Convection

Convection over the PIH CWA was fairly shallow today due to the limited instability. That being said, strong DCAPE developed, owing to pronounced Inverted-V profiles. The line of storms that developed was able to produce significant wind gusts, with multiple reports of 70 to 80 mph winds.

Satellite products were not particularly helpful in knowing what storms to issue warnings on due to the shallow nature of the convection. The loop below shows visible, IR, and water vapor imagery for the area of interest around the time we issued our first warning.

Figure 1 – Satellite imagery over the PIH forecast area around the time of warning issuance.

The thing that really stands out is that everything looks about the same. No single storm stands out as being particularly tall or possibly severe. The same is true when we look at the OCTANE Cloud Top Cooling product.

Figure 2 – Cloud Top Cooling around the time of warning issuance.

There was never a value of more than 3°C per 5 minutes over any of the developing convection, indicating the weak instability present. This doesn’t help much in figuring out what storms we need to focus on.

So we turned to radar. The KSFX radar showed an area of 50 knots inbounds associated with an area of higher reflectivity. This led to us issuing the first severe thunderstorm warning of the day.

Figure 3 – KSFX radar loop showing base velocity around the time of warning issuance.

After this, it became clear that almost any shower in the area was capable of producing severe wind gusts due to the favorable low-level thermodynamics and we began looking for similar looking signals in the satellite and radar products. We then issued several more severe thunderstorm warnings as the line progressed eastward.

-ei2018

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