17 April 1995
Vortex NOAA Aircraft Mission #4
Flight ID:
Flight Track:
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Flight Crew:
Chief Scientist: Watson/Ziegler Flight Director: Damiano
Doppler Radar: Shepherd Pilots: Tenneson/Kennedy
Cloud Physics: --- Data Technician: Pradas
Radiometer: Fedor Systems Engineer: Lynch/McNamara
Observer: Irisov
Observer: Hutchinson
Takeoff Time: 1817 UTC Landing Time: 0053 UTC
Official Mission Duration: 7.0 hrs
Mission Breakdown VORTEX: 7.0 hrs ARM: 0.0 hrs
Number of Data Tapes Used: Radar: 6 Cloud Physics: 1 Video: 3
Data Systems Log
Radar Data System Log Time On(UTC) Time Off(UTC) Comments
Tape #1 1913 Start LF&TA
2130 Radar down
Tape #2 2140
2206 Radar down
Tape #3 2216 No Spectral Width
2344 Radar Problems
Tape #4 2350
0054
Cloud Physics Log Time On(UTC) Time Off(UTC) Comments
1830 0030
ETL Radiometer Log Time On (UTC) Time Off (UTC) Comments
1805 0002 Poor data til 2000
UTC
Reason: Due to precipitation before and after takeoff, signal level on one
channel was erratic due to precipitation.
Summary:
The predeparture plan was that strong dynamics would produce
severe convection in the slot between clouds and the dryline. The ground
intercept teams departed OUN at 1510 UTC for Wichita Falls, TX. The P-3
departed OKC at 1817 UTC climbing, in clouds, to FL100 and heading for
Wichita Falls.
We reconnoitered weak developing high base convection near
and south of Guthrie, TX. We setup on cells near Seymour, TX, executing
6 Doppler legs as the cells weakened considerably. We then drifted
westward for a somewhat stronger-looking cell. Our first Doppler leg
began at 2120 UTC. Intermittent radar problems plagued data collection
until 2209 UTC. Thinking that the problem was data overload, we eliminated
recording of spectral width, and in desperation, eliminated the second
tape copy. Radar appeared to work well after that. BWER and tops to
18 km were observed at 2150 UTC. At 2256 UTC, a tornado was reported by
the ground teams near Temple, OK. By 2312 UTC, the mesocyclone seemed
to occlude in on itself. The mesocyclone appeared to detached itself
from the parent cloud while a new notch began to form.
Tornado sightings and warnings of tornadoes continued past 0045 UTC
when another tornado was reported near Davis, OK. The P-3 documented
the evolution of this supercell from 2120 UTC until we broke for OKC at
0031 UTC when it became apparent that OKC was going to have thunderstorms.
Twenty-four Doppler legs were completed on this supercell.
The NCAR Electra, after doing frontal and dryline work, joined us on
the tornadic storm around 2330 UTC. Both aircraft landed back at OKC
just ahead of the squal line. It appears that a great dataset was collected
Due to the evolution of the mesocyclone southward, many of the legs
appeared to be 20-25 km from the main portion of the storm. Seven hours
of flight time were consumed.
Irv Watson
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