G4 Flight in support of FASTEX IOP 15
Low 38: Primary cyclone
Date: February 15, 1997
(report prepared by Jean-Pierre Cammas)
Ferry flight to Saint-Johns (New Foundland):
Take-off Time Shannon (approx): 1200Z, February 13, 1997
Landing Time Saint Johns (approx): 1700Z
Targetting flight nearby Saint-Johns:
Take-off Time Saint-Johns (approx): 2100Z, February 13, 1997
This flight was cancelled due to mechanical problems with
the aircraft.
Subjective flight from Saint-Johns to Shannon:
Take-off Time Saint-Johns (approx): 0300Z, February 15, 1997
Landing Time Shannon (approx): 0930Z, February 15, 1997
Flight Duration: 6h30mn
Scientists: Melvin Shapiro (NOAA/ETL),
Ron Gelaro (NRL),
Gerald Desroziers (METEO-FRANCE),
Diana Bartels (NOAA/NSSL),
Jean-Pierre Cammas (LA/CNRS, not in the aircraft
during this mission, proposed
and designed the flight plan
at Operations Center, Shannon)
Purpose:
The purpose of this flight was to document actual structures of
a primary mature cyclone over the Central Atlantic, Low 38. The
other MSA aircraft flights were scheduled to take-off right after
the G4 landing in Shannon with flights focused on precipitation
features in the occluded portion of the mature low on its
northeastern part. In order to get the best coverage of the
system, the G4 flight plan was designed to sample the northwestern
back-bent surface front, the low center and its southwestern part,
the upper-level potential vorticity anomaly and the apex of
the warm sector with surface frontal structures on the eastern
part of the low.
Description of the flight:
The entire track has been flown at FL260. About 29 dropsondes were
sent on the GTS. Seven dropsondes were launched across the north
part of the bent-back surface front, a nice easterly low level jet
was observed (> 35 ms-1). With about 5 dropsondes, the next
north-south leg sampled a cross-section across the low center
observed as a warm and humid core, as well as across the
potential vorticity maximum aloft. Mid-tropospheric dryness is
observed on the south part of this leg. The third leg involved 5
dropsondes in the northwesterlies south of the bent back surface
front. Strong low level winds were observed (35-40 ms-1).
The last zonal leg involved about 15 dropsondes across features
east of the low center (dry intrusion, cold front, apex of warm
air and warm front, southerly upper-level jet). Wind speeds
in excess of 60 ms-1 were observed with the dropsondes (400 hPa)
when crossing the jet core. The upper-level frontal zone and the
surface cold front were well resolved by the dropsonde sampling.
Overall assessment of the flight:
Very good data on the mature phase of a primary cyclone. Focus was
put first on the northhwestern bent back surface front, the
surface low center and the lowest tropopause part. The flight
ended with a nicely sampled cut across the dry intrusion, the
cold front, the apex of warm air and the warm front, and the
southerly upper-level jet.