Development of precipitation retrievals at millimeter and sub-millimeter wavelengths for geostationary satellites

被引:24
作者
Defer, E. [1 ]
Prigent, C. [1 ]
Aires, F. [2 ]
Pardo, J. R. [3 ]
Walden, C. J. [4 ]
Zanife, O. -Z. [5 ]
Chaboureau, J. -P. [6 ]
Pinty, J. -P. [6 ]
机构
[1] Observ Paris, Lab Etud Rayonnement & Mat Astrophys, CNRS, F-75014 Paris, France
[2] Univ Paris 06, Meteorol Dynam Lab, Inst Pierre Simon Laplace, CNRS, Paris, France
[3] CSIC, Inst Estructura Mat, Dept Astrofis Mol & Infrarroja, E-28006 Madrid, Spain
[4] Rutherford Appleton Lab, Space Sci & Technol Dept, Didcot OX11 0QX, Oxon, England
[5] Collecte Localisat Satellite, Toulouse, France
[6] Univ Toulouse, Lab Aerol, CNRS, Toulouse, France
基金
英国自然环境研究理事会;
关键词
D O I
10.1029/2007JD008673
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We study the potential of millimeter and sub-millimeter wavelengths for precipitation retrieval from geostationary sensors based on mesoscale cloud modeling and radiative transfer computation. Hydrometeor profiles simulated with the Meso-NH cloud resolving model for five European midlatitude situations are used to compute the brightness temperatures at frequencies from 23.8 to 875 GHz with the Atmospheric Transmission at Microwaves (ATM). Performances of both rain detection and rain rate retrieval are analyzed for different frequency sets, over ocean and land separately, and compared to the user requirements. The performances of a frequency set such as that already planned for geostationary satellites (with channels in the O-2 lines at 50, 118, and 424 GHz, and in the H2O lines at 183, 325, 380 GHz) satisfy the requirements for Numerical Weather Prediction and NoWCasting in terms of rain detection as well as for rain rate retrieval above 1 mm/h. Suppressing the 50 GHz O-2 channels does not seriously degrade the performances, except for rain rate below 1 mm/h, and, in addition, limits the spatial resolution problem from a geostationary orbit. Adding the thermal infrared observations has a limited impact. The retrieval of other hydrometeor quantities (cloud, ice) is also tested as well as the possibility to retrieve rain and the other hydrometeor profiles. These theoretical results are evaluated at close-to-millimeter wavelengths with coincident AMSU-B and radar observations (BALTEX and CAMRa). The results are degraded with respect to the theory, as expected, but are consistent with the observations.
引用
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页数:16
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