Precipitation profile retrievals using temperature‐sounding microwave observations

[1] A Bayesian retrieval algorithm was developed to demonstrate the potential of microwave temperature-sounding channels for precipitation profile retrieval from spaceborne observations. The algorithm uses a database from combined cloud-radiative transfer model simulations of Hurricane Bonnie which was observed during the field campaign Convection and Moisture Experiment 3 (CAMEX-3). Sounding channels from two oxygen absorption complexes at 50–57 GHz and 118.75 GHz were combined to make use of their differential response to absorption and scattering by hydrometeors. The retrieval method was applied to airborne observations with the National Polar-Orbiting Operational Environmental Satellite System (NPOESS) Aircraft Sounder Testbed-Microwave (NAST-M) radiometer on board the ER 2 aircraft. The retrieved profiles were used to simulate radar reflectivities to be compared to ER 2 Doppler observations from the same aircraft. The results lead to the following conclusions: (1) The sounding channels provide the unique potential of cloud slicing because the channel-dependent variation of clear-air absorption allows the adjustment of maximum sensitivity to different altitudes. (2) The validation with radar data indicates a good performance of the algorithm; however, at least four channels in each absorption complex are required to constrain the retrieval well enough with the observations. (3) The validation also shows that even though a Hurricane Bonnie cloud model simulation was used, the simulated database does not represent the observations very well. (4) The database may bias the retrievals by the underlying assumptions on temperature, humidity, and hydrometeor distributions. Sounding channels are more sensitive to a possible temperature bias in the database. While this bias can be corrected, the retrievals forward the database bias to the retrieved products independent of sensor. For global applications, more flexible retrieval approaches are required that are capable of constraining the algorithm according to the local situation.

[1]  Paul Racette,et al.  The EDOP Radar System on the High-Altitude NASA ER-2 Aircraft , 1996 .

[2]  Peter Bauer,et al.  Variational retrieval of rain profiles from spaceborne passive microwave radiance observations , 2003 .

[3]  Christian Kummerow,et al.  A simplified scheme for obtaining precipitation and vertical hydrometeor profiles from passive microwave sensors , 1996, IEEE Trans. Geosci. Remote. Sens..

[4]  A. J. Gasiewski,et al.  Numerical modeling of passive microwave O2 observations over precipitation , 1990 .

[5]  William S. Olson,et al.  Improving Global Analysis and Short-Range Forecast Using Rainfall and Moisture Observations Derived from TRMM and SSM/I Passive Microwave Sensors , 2001 .

[6]  Paul Fieguth,et al.  Observations of Thermal and Precipitation Structure in a Tropical Cyclone by Means of Passive Microwave Imagery near 118 GHZ , 1996 .

[7]  Peter Bauer,et al.  The Effect of the Melting Layer on the Microwave Emission of Clouds over the Ocean , 1999 .

[8]  P. Bauer,et al.  Algorithms for the retrieval of rainfall from passive microwave measurements , 1994 .

[9]  Ziad S. Haddad,et al.  The TRMM 'Day-1' Radar/Radiometer Combined Rain-Profiling Algorithm , 1997 .

[10]  Christian D. Kummerow,et al.  A Method for Combined PassiveActive Microwave Retrievals of Cloud and Precipitation Profiles , 1996 .

[11]  Tim J. Hewison,et al.  A comparison of ocean emissivity models using the Advanced Microwave Sounding Unit, the Special Sensor Microwave Imager, the TRMM Microwave Imager, and airborne radiometer observations , 2003 .

[12]  Philip W. Rosenkranz,et al.  Atmospheric 60-GHz oxygen spectrum : new laboratory measurements and line parameters , 1992 .

[13]  F. Marzano,et al.  Combined cloud-microwave radiative transfer modeling of stratiform rainfall , 2000 .

[14]  Eric A. Smith,et al.  The emergence of inversion‐type profile algorithms for estimation of precipitation from satellite passive microwave measurements , 1994 .

[15]  Philip W. Rosenkranz,et al.  NPOESS Aircraft Sounder Testbed-Microwave (NAST-M): instrument description and initial flight results , 2001, IEEE Trans. Geosci. Remote. Sens..

[16]  Christian D. Kummerow,et al.  On the accuracy of the Eddington approximation for radiative transfer in the microwave frequencies , 1993 .

[17]  F. Marzano,et al.  Use of cloud model microphysics for passive microwave-based precipitation retrieval : Significance of consistency between model and measurement manifolds , 1998 .

[18]  Albin J. Gasiewski,et al.  Aircraft-based Radiometric Imaging of Tropospheric Temperature and Precipitation Using the 118.75-GHz Oxygen Resonance , 1990 .

[19]  C. Kummerow,et al.  Determination of Precipitation Profiles from Airborne Passive Microwave Radiometric Measurements , 1991 .

[20]  G. Tripoli A Nonhydrostatic Mesoscale Model Designed to Simulate Scale Interaction , 1992 .

[21]  Giulia Panegrossi,et al.  Using TRMM observations to improve numerical simulations of precipitation within tropical cyclones , 2001 .

[22]  Eric A. Smith,et al.  Intercomparison of microwave radiative transfer models for precipitating clouds , 2002, IEEE Trans. Geosci. Remote. Sens..

[23]  Peter Bauer,et al.  Including a melting layer in microwave radiative transfer simulation for clouds , 2001 .

[24]  P. Bauer,et al.  On the Effect of the Melting Layer on the Microwave Emission of Clouds. , 1996 .

[25]  Virginie Marécal,et al.  Variational Retrieval of Temperature and Humidity Profiles from TRMM Precipitation Data , 2000 .