http://www.cnr.it/ontology/cnr/individuo/prodotto/ID296451
A VERIFICATION STUDY OVER EUROPE OF AMSU-A/MHS AND SSMIS PASSIVE MICROWAVE PRECIPITATION RETRIEVALS (Comunicazione a convegno)
- Type
- Label
- A VERIFICATION STUDY OVER EUROPE OF AMSU-A/MHS AND SSMIS PASSIVE MICROWAVE PRECIPITATION RETRIEVALS (Comunicazione a convegno) (literal)
- Anno
- 2013-01-01T00:00:00+01:00 (literal)
- Alternative label
GIULIA PANEGROSSI , Daniele Casella , Alberto Mugnai , Marco Petracca , Paolo Sanò , Stefano
Dietrich (2013)
A VERIFICATION STUDY OVER EUROPE OF AMSU-A/MHS AND SSMIS PASSIVE MICROWAVE PRECIPITATION RETRIEVALS
in 2013 Joint EUMETSAT/AMS Meteorological Conference, Vienna, Austria, 16-20 Sept, 2013
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- GIULIA PANEGROSSI , Daniele Casella , Alberto Mugnai , Marco Petracca , Paolo Sanò , Stefano
Dietrich (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Institute of Atmospheric Sciences and Climate, ISAC-CNR, Rome Italy (literal)
- Titolo
- A VERIFICATION STUDY OVER EUROPE OF AMSU-A/MHS AND SSMIS PASSIVE MICROWAVE PRECIPITATION RETRIEVALS (literal)
- Abstract
- Within the EUMETSAT H-SAF program (Satellite Application Facility on Support to Operational Hydrology
and Water Management, http://hsaf.meteoam.it) we have developed two different passive microwave
precipitation retrieval algorithms, one based on a physically-based Bayesian approach for conically
scanning radiometers (i.e., SSMIS), and the other one based on Neural Network approach for cross-track
scanning radiometers (i.e., AMSU-A/MHS). The two algorithms are based on the same physical
foundation, i.e., same cloud-radiation model simulations to be used as a priori information in the Bayesian
solver and as training dataset in the neural network approach. They also use similar procedures for
screening of non-precipitating pixels, identification of frozen background surface, presence of snowfall, and
determination of a pixel based quality index of the surface precipitation retrievals. These procedures are
calibrated according to the different characteristics (i.e., viewing angle, horizontal resolution, channel
frequencies) of the cross-track and conically scanning radiometers used. The two algorithms use
dynamical/meteorological/environmental variables as ancillary information to characterize the observed
event, and mitigate the ambiguity of the cloud microphysical structures (and rainfall rates at the ground)
associated to any given set of measured multichannel brightness temperatures. A verification study of the
latest versions of the two algorithms has been carried out within the H-SAF program, where the rainfall
estimates are compared against radar observations and rain gauge network measurements for several
precipitation events in Europe, characterized by different environmental, meteorological, dynamical
conditions, and by different precipitation regimes. We will present the main results of this study, discussing
strengths and potentials of the two algorithms in relation to the different characteristics of the observed
events. In addition the consistency of the retrievals from close in time overpasses of the cross-track and
conically scanning radiometers for the same event will be discussed. Consistency, besides accuracy of the
retrievals, is necessary in order to be able to fully exploit all current of future cross-track and conically
scanning radiometer overpasses for monitoring precipitation, and to be able to use them in conjunction with
IR GEO observations in blending/morphing resolution enhancing techniques for nowcasting and/or
hydrological applications. (literal)
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