SENSITIVITY STUDIES OF TOVS RETRIEVALS WITH 3I AND ITPP RETRIEVAL ALGORITHMS - APPLICATION TO THE RESOLUTION OF MESOSCALE PHENOMENA IN THE ANTARCTIC

Citation
G. Heinemann et al., SENSITIVITY STUDIES OF TOVS RETRIEVALS WITH 3I AND ITPP RETRIEVAL ALGORITHMS - APPLICATION TO THE RESOLUTION OF MESOSCALE PHENOMENA IN THE ANTARCTIC, Meteorology and atmospheric physics, 55(1-2), 1995, pp. 87-100
Citations number
35
Categorie Soggetti
Metereology & Atmospheric Sciences
ISSN journal
01777971
Volume
55
Issue
1-2
Year of publication
1995
Pages
87 - 100
Database
ISI
SICI code
0177-7971(1995)55:1-2<87:SSOTRW>2.0.ZU;2-M
Abstract
Retrievals from TIROS-N Operational Vertical Sounder (TOVS) data with the International TOVS Processing Package (ITPP version 3.3) and the I mproved Initialisation Inversion (3I version 2) algorithms are investi gated. The comparative study comprises the retrieval mechanism from th e first guess to the final result for collocated radiosonde/satellite data as well as the problem of horizontal resolution for simulated Ant arctic cold air pools. For the latter problem, TOVS brightness tempera tures are computed for simulated NOAA-10 overpasses in the Weddell Sea region of Antarctica by the ITPP and the 3R (Rapid Radiance Recogniti on) forward models for retrievals with ITPP and 3I, respectively. The main results of this study are: Comparisons of ITPP and 3R forward mod els with collocated radiosonde data for cloudless Antarctic profiles y ield differences less than 2 K except for HIRS-channel 1 and water vap our channels. For typical examples of Antarctic profiles for the coast al region, results of 3I retrievals lie closer to the collocated radio sonde profiles than ITPP retrievals even for cases with surface invers ions. Simulations of cold air pools for cloud-free conditions show tha t cold air pools with a strong temperature anomaly and with diameters of 800 km and greater are well reproduced by ITPP and 3I. For smaller cold air pools with a moderate temperature perturbation, the resolutio n limits are reached if the diameter is smaller than 400 and 200 km fo r ITPP and 3I, respectively. ITPP retrievals have smaller horizontal g radients and higher values for geopotential thicknesses in the center of the cold air pools. The better performance of the 3I retrievals for smaller cold air pools is a consequence of the better first guess of the TIGR dataset compared with the regression first guess of the ITPP.