OCTANE Speed Product Shows Weakening Trend in Storm Well

A strong storm with a well defined mid-level mesocyclone entered the western portion of the MKX CWA at around 4:00 PM CDT. At the time, the OCTANE speed product showed a well defined gradient and the divergence product showed fairly high values, indicating that the updraft was quite strong. We decided to issue a severe thunderstorm warning with a tornado possible tag on this cell as a result.

Not long after the warning was issued, we noticed a significant weakening trend in the reflectivity signatures. This weakening trend was supported by the OCTANE products as well, with a much more diffuse gradient in the speed product and lower values in the cloud top divergence. An interesting thing to note, though, is that the Day Cloud Phase imagery looks nearly identical to when we issued the warning, so it did not capture the weakening trend.

Another interesting thing to note is that the IR imagery did not seem to indicate that there was as much weakening either. One image from around the time of warning issuance and one from around the time when the warning expired are shown below.

In all, the OCTANE products seem to be very useful in assessing the strength of a storm’s updraft. Looking forward to gaining more experience with it and the other products throughout the rest of the week.

- EI2018

Severe thunderstorm warning issued for South Central Wisconsin

 Solid signature from both nearby radars but the beam height was at least 8k feet. PHS environmental fields were supportive of a primary wind hazard. OCTANE divergence fields distinctly noted this cell with persistent strong divergence as it moved into the CWA. Low level wind fields were not as impressive with widespread STP of less than 0.2, despite strong instability in the PHS fields.

-Hellothere

THE TALE OF TWO GUIDANCE SYSTEMS

THE PHS MODEL GUIDANCE has had difficulty providing an accurate near term forecast with respect to the purely linear mode to the MCS as it moves east into the Texarkana region. This is most noticeable with respect to the southern portion of the linear convection. This can be seen easily below with the 3 hr forecast (in the image below) is the top panel of the image. The composite reflectivity (considered verification) is the bottom panel of the image.

THE GREMLIN MACHINE LEARNING GUIDANCE on the other hand has performed very well with the linear MCS in the near terms, along with other convection further downstream to the east. In the images below Gremlin is the top image and MRMS (considered verification) is the bottom image.

-5454wx

High Confidence in Lightning activity:

There is high confidence in lightning activity with the storms moving across southern Wisconsin this afternoon into this evening.  Based on the lightningcast product shown below, there is a greater than 90% chance of lightning within the orange outlines over the next hour.

As you can see on the image below, this is a point forecast for Camp Randall Stadium, showing the same results.

-ULMCUBMAN

High Confidence in Progressive/Weak MCS

KSHV radar trends illustrate a cold-pool dominated, weak MCS approaching the NW corner of the CWA. Many satellite products illustrated a consistent mainly sub-severe weather episode unfolding giving increasing confidence in the near-term forecast and expected impacts. Focus would be on any stronger individual updrafts for potential isolated severe thunderstorm warnings. 

Overall, there was high confidence in approaching thunderstorms per radar and LightningCast data pinpointed the ongoing widespread nature of the convection, given several embedded impulses of GLM spikes behind the leading southeastward surging outflow boundary:

 

East Octane SpeedDirCTD-CTD_4Pan procedure provides more calculated parameters on top of RGB and ABI products to quickly diagnose convective strength/intensity.

The top 3 panels below (OCTANE speed, direction and Cloud-top Cooling and Divergence) identify a large-scale cirrus canopy with embedded updraft impulses.

Situational awareness was enhanced by adding on local KSHV and KLZK radar which helped to identify a SSW to NNE boundary and associated CI ahead of the main line, which OCTANE products began to illustrate (see center of each product, identifying increasing speed/directional divergence colocated to the convection along the boundary)

Given the environmental parameters, this would have been a location to examine for the potential of a severe thunderstorm warning, especially if associated radar trends (RIJ via radial velocity) indicate increasing downdraft wind potential.

- RED11248

GLM Data Quality Under the Shadow of the Anvil

 

As we are watching a cluster of thunderstorms develop across Nebraska, we're in a region where GLM may not be able to most efficiently detect flashes in the region. However, underneath the shadow of the cirrus blow off, the flash detection efficiency increases, and the stoplight colormap begins to suggest that the data quality is better. Perhaps this offers a bit of hope when forecasting charge moving along with the anvil.

Kadic

A Tale of Two Storms From OCTANE, LightningCast, and GREMLIN

 

This is an interesting comparison of two storms that show two initially different satellite and LightningCast signals that produce very different results on radar. The southern cell shows an initially much more consistent cloud top divergence signal from OCTANE with a more robust looking anvil shield and an above anvil cirrus plume. That aside, the northern storm consistently had a higher probability of >10 GLM flashes from LightningCast and eventually developed a far stronger radar signature and eventual severe thunderstorm. The southern storm struggled to even develop a 40 dBZ core. The animation below shows the same progression but with the OCTANE speed and direction RGBs. In this case if a severe decision was to be made with just the satellite presentation, the wrong decision may have been made (at least initially). 

-Joaq

Finally, here is how GREMLIN handled the southern storm, which it understandably initially intruduced high reflectivity to the southern storm. 

-Joaq

OCTANE Trends for Ongoing Convection in ABR CWA

Taking a look at OCTANE - it seems like the IR/Nighttime data shows especially the directional details a bit more than the Visible/Daytime products. This has been a continuing trend this week. The CTD and CTC products have been useful with monitoring the strength of the storms (especially which may become severe) as well as with the newer convection/updrafts.

OCTANE - Visible (Daytime) vs IR (Nighttime)

OCTANE - Cloud Top Cooling and Cloud Top Divergence

Forecaster Cumulus

A Tale of Two Thunderstorms

Two thunderstorms developed with mixed signals between the variety of tools available. Satellite tools would've suggested that the southern storm was the area of interest, but the radar signature was much better for the northern storm. GREMLIN is shown below, with the GOES West on the left and GOES East on the right. LightningCast is contoured, and the probability of 10 flashes mainly favored the northern storm. The appearance on GREMLIN was much stronger for the southern storm.

When looking at the GLM RBG, the more frequent and shorter flashes were associated with the southern storm.

Looking at OCTANE, the southern storm appeared more impressive. Although towards the end, the northern storm began to exhibit stronger upper level divergence.

But again, if one were to look at radar, it would be readily apparent that the northern storm should be ranked as the biggest threat. In a situation involving satellite alone, I might have missed the event that did produce the severe event.

And of course remembering how significant parallax is. From GREMLIN with GOES West, my storms were neatly in their boxes, but from GOES East, it would've looked quite strange.

And despite the signal from satellite, the southern storm essentially collapsed in on itself. GREMLIN using GOES West does not seem to catch on to this fact, but GOES East has corrected to a stronger storm up north.
 

Kadic

Finding Boundaries in OCTANE Direction and Comparing to Satellite

As a forecaster, I'm most accustomed to pulse severe conditions, and I work in an area where there tends to be abundant cloud cover. So being able to find boundaries is really helpful. So I decided to review some of the low-level cumulus fields in OCTANE and looking how accurate they are compared to current derived GOES East winds. From what I sampled, they were within 5 degrees of OCTANE.

Now zooming out, we see that there will be an area of confluence in the wind field based on the low-level cu field. Further aloft, you can see some of the diffluence along the warm conveyor belt. Sometimes, wind barbs are really useful tools to assessing an environment, and I think a similar function in OCTANE could be useful for mesoanalysis.

 

Kadic