G. Heinemann, TOVS RETRIEVALS OBTAINED WITH THE 3I-ALGORITHM - A STUDY OF A MESOSCALE CYCLONE OVER THE BARENTS SEA, Tellus. Series A, Dynamic meteorology and oceanography, 47(3), 1995, pp. 324-330
ECMWF analyses and TOVS retrievals obtained with the Improved Initiali
sation Inversion (version 2) algorithm are used to study a meso-scale
cyclone over the western Barents Sea during 26-27 February 1987. Due t
o the good spatial and temporal coverage of the polar regions by TOVS
data, the development of this vortex was documented in detail. Results
from TOVS retrievals are compared with results from a simulation usin
g a limited area model. The retrievals reveal the intensification of a
cold air outbreak over the period of a few hours, leading to enhanced
formation of the vortex. The development of an extended warm belt ove
r the Barents Sea is observed, but the weak warm core, shown by the nu
merical simulation at lower layers inside this warm belt, is not resol
ved.