Operations started earlier today, in part to give the chance to use
some of the GOES-R products, such as convective initiation, before cirrus
contamination. The two initial locations
were Ft. Worth and San Angelo. The blog
post “CI/CTC Identifying Developing Convection in a Favorable Environment” (http://goesrhwt.blogspot.com/2013/05/cictc-identifying-developing-convection.html)
summarizes the use of CI earlier in the day in the San Angelo county warning
area.
By mid-afternoon, one group
shifted to the Lubbock county warning area to investigate the PGLM in that
region. The transfer to Lubbock occurred
as storms were already firing, but we took a look back to see what had occurred
previously.
Flipping back we observed the GOES-R CI provide a probability of convection
around 20 at 1930 UTC in northwestern Motley County (yellow arrow).
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The GOES-R CI (upper left), IR (upper right) and visible satellite (lower left), and Lubbock, Texas radar reflectivity (lower right) at 1930 UTC. |
The GOES-R CI remained at this level until 1945 UTC when an upper 70
value was observed at the junction of Motley, Floyd, and Briscoe Counties (yellow
arrow). The visible satellite imagery
shows that the features are nearly stationary.
![]() |
The GOES-R CI (upper left), IR (upper right) and visible satellite (lower left), and Lubbock, Texas radar reflectivity (lower right) at 1945 UTC. |
By the next scan, the GOES-R CI had topped 90 for the probability of convection at 2002 UTC (yellow arrow). Up to
this point, the radar was showing now activity in this area. Also take note of the GOES-R CI in Briscoe County
(red arrow) showing moderate strength of signal values around the county.
![]() |
The GOES-R CI (upper left), IR (upper right) and visible satellite (lower left), and Lubbock, Texas radar reflectivity (lower right) at 2002 UTC. |
We then move ahead to 2022 UTC, where radar first observes
reflectivities exceeding 35 dBZ and a developing cell can be seen in both the
IR and visible imagery in Motley County (yellow arrow). The GOES-R CI continues to trend upward in
Briscoe County (red arrow, and there is no current radar observations of
storms.
![]() |
The GOES-R CI (upper left), IR (upper right) and visible satellite (lower left), and Lubbock, Texas radar reflectivity (lower right) at 2022 UTC. |
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The GOES-R CI (upper left), IR (upper right) and visible satellite (lower left), and Lubbock, Texas radar reflectivity (lower right) at 2045 UTC. |
Finally, at 2115 UTC, the radar signature for the storms in Motley and
Briscoe Counties is well defined. Note
that the GOES-R CI stops tracking mature cells.
![]() |
The GOES-R CI (upper left), IR (upper right) and visible satellite (lower left), and Lubbock, Texas radar reflectivity (lower right) at 2115 UTC. |
The GOES-R CI provided the first indication of a
potential cell in Motley County at 1930 UTC, giving it a 50 minute lead
time. Even with waiting for a stronger probability of convection, the GOES-R CI provided 35 minutes of lead time (signal of 70+), and 20
minutes (signal of 90+), respectively. The
GOES-R CI followed that with roughly 40 minutes of lead time for the Briscoe
County storms. Once the storms got
rolling in this region, they became the focus of the PGLM total lightning blog
post “Warning Issued with only PGLM Lightning Jump” (http://goesrhwt.blogspot.com/2013/05/warning-issued-with-only-pglm-lightning.html).
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