Infrared Radiance Modeling by Optimal Spectral Sampling

被引:82
作者
Moncet, Jean-Luc [1 ]
Uymin, Gennady [1 ]
Lipton, Alan E. [1 ]
Snell, Hilary E. [1 ]
机构
[1] Atmospher & Environm Res Inc, Lexington, MA USA
关键词
D O I
10.1175/2008JAS2711.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper describes a rapid and accurate technique for the numerical modeling of band transmittances and radiances in media with nonhomogeneous thermodynamic properties (i.e., temperature and pressure), containing a mixture of absorbing gases with variable concentrations. The optimal spectral sampling (OSS) method has been designed specifically for the modeling of radiances measured by sounding radiometers in the infrared and has been extended to the microwave; it is applicable also through the visible and ultraviolet spectrum. OSS is particularly well suited for remote sensing applications and for the assimilation of satellite observations in numerical weather prediction models. The novel OSS approach is an extension of the exponential sum fitting of transmittances technique in that channel-average radiative transfer is obtained from a weighted sum of monochromatic calculations. The fact that OSS is fundamentally a monochromatic method provides the ability to accurately treat surface reflectance and spectral variations of the Planck function and surface emissivity within the channel passband, given that the proper training is applied. In addition, the method is readily coupled to multiple scattering calculations, an important factor for treating cloudy radiances. The OSS method is directly applicable to nonpositive instrument line shapes such as unapodized or weakly apodized interferometric measurements. Among the advantages of the OSS method is that its numerical accuracy, with respect to a reference line-by-line model, is selectable, allowing the model to provide whatever balance of accuracy and computational speed is optimal for a particular application. Generally only a few monochromatic points are required to model channel radiances with a brightness temperature accuracy of 0.05 K, and computation of Jacobians in a monochromatic radiative transfer scheme is straightforward. These efficiencies yield execution speeds that compare favorably to those achieved with other existing, less accurate parameterizations.
引用
收藏
页码:3917 / 3934
页数:18
相关论文
共 39 条
[1]  
Anderson G., 1986, ENV RES PAPERS, V954
[2]   Improved method of exponential sum fitting of transmissions to describe the absorption of atmospheric gases [J].
Armbruster, W ;
Fischer, J .
APPLIED OPTICS, 1996, 35 (12) :1931-1941
[3]   AIRS/AMSU/HSB on the aqua mission: Design, science objectives, data products, and processing systems [J].
Aumann, HH ;
Chahine, MT ;
Gautier, C ;
Goldberg, MD ;
Kalnay, E ;
McMillin, LM ;
Revercomb, H ;
Rosenkranz, PW ;
Smith, WL ;
Staelin, DH ;
Strow, LL ;
Susskind, J .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2003, 41 (02) :253-264
[4]   Prelaunch characteristics of the Moderate Resolution Imaging Spectroradiometer (MODIS) on EOS-AM1 [J].
Barnes, WL ;
Pagano, TS ;
Salomonson, VV .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1998, 36 (04) :1088-1100
[5]   Practical methods for rapid and accurate computation of interferometric spectra for remote sensing applications [J].
Barnet, CD ;
Blaisdell, JM ;
Susskind, J .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2000, 38 (01) :169-183
[6]  
BINDER K, 1997, MONTE CARLO SIMULATI
[7]  
CHEDIN A, 1985, J CLIM APPL METEOROL, V24, P128, DOI 10.1175/1520-0450(1985)024<0128:TIIIMA>2.0.CO
[8]  
2
[9]   LINE-BY-LINE CALCULATIONS OF ATMOSPHERIC FLUXES AND COOLING RATES - APPLICATION TO WATER-VAPOR [J].
CLOUGH, SA ;
IACONO, MJ ;
MONCET, JL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D14) :15761-15785
[10]  
Eyre J. R., 1991, 176 ECMWF