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7. REFERENCESBauer, P., L. Schanz and L. Roberti, 1998: Correction of the three-dimensional effects forpassive microwave remote sensing of convective clouds. J. Appl. Meteor., 37, 1619-1632.Bohren, C.F., and D.R. Huffman, 1983: Absorption and Scattering of Light by Smal particles.John Wiley & Sons, 530 pp.Cotton, W.R., G.J. Tripoli, R.M. Rauber and E.A. Mulvihill, 1986: Numerical simulation of theeffects of varying ice crystal nucleation rate and aggregation processes on orographicsnowfall. J. Clim. Apl. Meteor. 25: 1658-1680.Czekala, H., P. Bauer, D. Jones, F. Marzano, A. Tassa, L. Roberti, S. English, J.P.V. PoiaresBaptista, A. Mugnai and C. Simmer, 2000: Clouds and Precipitation. Radiative TransferModels for Microwave Radiometry (C. Matzler, Ed.), COST Action 712, Directorate-General for Research, European Commission, Brussels, Belgium, 37-72.Di Michele S., A. Tassa, A. Mugnai, F.S. Marzano, P. Bauer and J.P.V. Poiares Baptista,2005: The Bayesian Algorithm for Microwave-based Precipitation Retrieval: Descriptionand application to TMI measurements over ocean. IEEE Trans. Geosci. Remote Sens.,43, 778-791.Di Michele S., F.S. Marzano, A. Mugnai, A. Tassa and J.P.V. Poiares Baptista, 2003:Physically-based statistical integration of TRMM microwave measurements forprecipitation profiling. Radio Sci., 38, 8072-8088.English, S.J., and T.J. Hewison, 1998: A fast generic millimetre wave emissivity model. Proc.SPIE on Microwave Remote Sensing of the Atmosphere and Environment, 22- 30.Flatau P., G.J. Tripoli, J. Berlinde and W. Cotton, 1989: The CSU RAMS Cloud MicrophysicsModule: General Theory and Code Documentation. Technical Report 451, ColoradoState University, 88 pp.Grenfell, T.C., and S.G. Warren, 1999: Representation of a nonspherical ice particle by acollection of independent spheres for scattering and absorption of radiation. J.Geophys. Res., 104, 31697-31709.Hewison, T.J., 2001: Airborne measurements of forest and agricultural land surface emissivityat millimeter wavelengths. IEEE Trans. Geosci. Remote Sens., 39, 393-400.Hewison, T.J., and S.J. English, 1999: Airborne retrievals of snow and ice surface emissivity atmillimetre wavelengths. IEEE Trans. Geosci. Remote Sens., 37, 1871-1879.Hewison, T.J., and S.J. English, 2000: Fast models for land surface emissivity. RadiativeTransfer Models for Microwave Radiometry (C. Matzler, Ed.), COST Action 712,Directorate- General for Research, European Commission, Brussels, Belgium, 117-127.Liu, G., C. Simmer and E. Ruprecht, 1996: Three-dimensional radiative transfer effects ofclouds in the microwave spectral range. J. Geophys. Res., 101, 4289-4298.Mugnai, A., Casella, D., Formenton, M., Sanò, P., Tripoli, G. J., Leung, W. L., Smith, E. A.,Mehta, A., 2009, Generation of an European Cloud-Radiation Database to be usedfor PR-OBS-1 (Precipitation Rate at Ground by MW Conical Scanners), ActivityReport, EUMETSAT – HSAF Project, 39 pp.Mugnai, A., S. Di Michele, F.S. Marzano and A. Tassa, 2001: Cloud-model based Bayesiantechniques for precipitation profile retrieval from TRMM microwave sensors.ECMWF/EuroTRMM Workshop on Assimilation of Clouds and Precipitation, ECMWF,Reading, U.K., 323-345.Neshyba, S.P., T.C. Grenfell and S.G. Warren, 2003: Representation of a nonspherical iceparticle by a collection of independent spheres for scattering and absorption ofradiation: 2. Hexagonal columns and plates. J. Geophys. Res., 108, 4448-4465.32
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Page 1 and 2: SATELLITE APPLICATION FACILITY ON S
Page 3 and 4: 1. INTRODUCTIONIt is rather a very
Page 5 and 6: In total, there are four C Band Dop
Page 7 and 8: channel has a different cloud struc
Page 10 and 11: Table 4.2. NMS model featuresNon-hy
Page 12 and 13: 5. ANALYSIS PROCEDURE5.1. Statistic
Page 14 and 15: Table 5.3. Statistics indexes of si
Page 16 and 17: High Frequency Channels pdfs Over L
Page 18 and 19: Figure 5.6. 19.35 GHz vs. 37 GHz sc
Page 20 and 21: deviations in Figure 5.12a. This is
Page 22 and 23: The statistical properties of both
Page 24 and 25: As the last example from rather mou
Page 26 and 27: 5.2.2. Validation of Retrieval by u
Page 28 and 29: 6) It is very obvious in Figure 5.2
Page 30 and 31: Mean Error, Standart Deviation and

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