Importance of Rapid Scan
Operations Satellite Imagery
in Monitoring Severe Convection
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Fifteen-minute Intervals
Loop 1
Five-minute Intervals
Loop 2
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This satellite interpretation
discussion serves as a reminder to NWS offices that they may request 7
½ minute interval (8/hour) satellite imagery, called Rapid Scan
Operations or RSO, and to present an example of why such imagery is beneficial
during severe weather outbreaks. The following imagery was taken
on April 7, 1998, during the GOES-10 checkout period. Although the
satellite was imaging every 5 minutes instead of every 7 ½ minutes,
as would be the case during an RSO, the arguments for the more frequent
imaging can still be made.
The included loops compare six images at 15 minute intervals
(Loop1) and fourteen images at 5 minute intervals (Loop 2) in capturing
the intersection between two low level thunderstorm outflow boundaries
and its subsequent evolution into a thunderstorm which produced a tornado
during the central Illinois outbreak of April 7, 1998. In both loops,
the 2145 UTC image shows the two low level thunderstorm outflows whose
intersection is monitored at 5 and 15 minute intervals up to 2300 UTC,
five minutes before the report of a tornado 2.5 miles west of Mt. Pulaski,
IL. Comparison of the two sets reveals that although both sets record
the developing thunderstorm, the five minute data contain, as would be
expected, information that is not seen at the 15 minute interval. |
In particular, compare the six 5 minute images starting at
2200 UTC and ending at 2230 UTC with the three 15 minute images taken at
2200 to 2230 UTC. In the five minute imagery, it is clearly seen
that the low level outflows from the two thunderstorms approach each other,
intersect, and form the cloud mass pointed out in the 2215 UTC image, which
continues to develop. The early growth of the cloud is seen between
2215 UTC and 2230 UTC.
With the fifteen minute imagery, the approach and intersection
of the two outflows is not as obvious, and one needs to wait for the 2230
UTC image to confirm the growth of the cloud. The continued development
of the thunderstorm to just before the time of the reported tornado is
better monitored by the 5 minute data.
Such interactions between low level thunderstorm outflow
boundaries have been shown to be important in convective processes.
In this case, the interaction resulted in a tornadic thunderstorm.
With 5 minute data (or 7 ½ minute data), these interactions are
better monitored than with the conventional 15 minute data, and provide
important complementary data to radar analyses. AWIPS equipped NWS
offices can (today) receive and view the RSO data 1-3 minutes after scan
time.
Click
on images to enlarge
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