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Journal of Applied Meteorology and Climatology

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Article Type:
Research Article

Correction of Three-Dimensional Effects for Passive Microwave Remote Sensing of Convective Clouds

P. BauerDeutsche Forschungsanstalt für Luft-und Raumfahrt, Cologne, Germany

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L. SchanzDeutsche Forschungsanstalt für Luft-und Raumfahrt, Cologne, Germany

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L. RobertiDipartimento di Elettronica, Politecnico di Torino, Torino, Italy

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Print Publication:
01 Dec 1998
DOI:
https://doi.org/10.1175/1520-0450(1998)037<1619:COTDEF>2.0.CO;2
Page(s):
1619–1632
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Abstract

This paper presents a simple approach to adjust microwave brightness temperature distributions obtained from slant-path measurements for projection effects. Horizontal displacement in the direction of sight is caused by signal contributions from other than near-surface layers that are projected to the footpoint of observation. In particular at frequencies sensitive to ice particle scattering the horizontal projection effect can amount to values as big as the vertical cloud extent. Based on cloud model–generating, three-dimensional hydrometeor distributions at subsequent model time steps and a modified one-dimensional radiative transfer model, the high correlation of effective radiance contribution altitudes and brightness temperatures at 37.0 and 85.5 GHz is demonstrated. For these altitudes, described by the centers of gravity of the spectral weighting functions, regression equations are derived with standard errors below 0.61 km at 85.5 GHz and 0.22 km at 37.0 GHz for both the Special Sensor Microwave/Imager (SSM/I) and Tropical Rainfall Measurement Mission Microwave Imager. Once the centers of gravity are retrieved a simple geometry correction can be applied to the measurements.

Application to model cloud fields at various time steps and different oberservation geometries shows a significantly improved correspondence of brightness temperature and hydrometeor distributions. This method is also applied to SSM/I observations during the Tropical Ocean Global Atmosphere Coupled Ocean–Atmosphere Response Experiment in the equatorial Pacific. Considerable improvements of single-channel rain retrievals based on 85.5-GHz measurements compared to shipborne radar data were achieved, which suggests that a major uncertainty of so-called scattering algorithms can be explained by geometry effects that can be easily corrected. Multichannel algorithms, however, require a more elaborate integration scheme to allow for both frequency and scene-dependent adjustments.

Corresponding author address: Mr. Peter Bauer, DLR, Space System Analysis Division, Linder Höhe, 51170 Köln, Germany.

peterb@dv.kp.dlr.de

Abstract

This paper presents a simple approach to adjust microwave brightness temperature distributions obtained from slant-path measurements for projection effects. Horizontal displacement in the direction of sight is caused by signal contributions from other than near-surface layers that are projected to the footpoint of observation. In particular at frequencies sensitive to ice particle scattering the horizontal projection effect can amount to values as big as the vertical cloud extent. Based on cloud model–generating, three-dimensional hydrometeor distributions at subsequent model time steps and a modified one-dimensional radiative transfer model, the high correlation of effective radiance contribution altitudes and brightness temperatures at 37.0 and 85.5 GHz is demonstrated. For these altitudes, described by the centers of gravity of the spectral weighting functions, regression equations are derived with standard errors below 0.61 km at 85.5 GHz and 0.22 km at 37.0 GHz for both the Special Sensor Microwave/Imager (SSM/I) and Tropical Rainfall Measurement Mission Microwave Imager. Once the centers of gravity are retrieved a simple geometry correction can be applied to the measurements.

Application to model cloud fields at various time steps and different oberservation geometries shows a significantly improved correspondence of brightness temperature and hydrometeor distributions. This method is also applied to SSM/I observations during the Tropical Ocean Global Atmosphere Coupled Ocean–Atmosphere Response Experiment in the equatorial Pacific. Considerable improvements of single-channel rain retrievals based on 85.5-GHz measurements compared to shipborne radar data were achieved, which suggests that a major uncertainty of so-called scattering algorithms can be explained by geometry effects that can be easily corrected. Multichannel algorithms, however, require a more elaborate integration scheme to allow for both frequency and scene-dependent adjustments.

Corresponding author address: Mr. Peter Bauer, DLR, Space System Analysis Division, Linder Höhe, 51170 Köln, Germany.

peterb@dv.kp.dlr.de

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