Thermal radiative fluxes through inhomogeneous cloud fields: a sensitivity study using a new stochastic cloud generator

被引:16
作者
Benassi, A
Szczap, F
Davis, A
Masbou, M
Cornet, C
Bleuyard, P
机构
[1] Univ Clermont Ferrand, Lab Meteorol Phys, OPGC, Clermont Ferrand, France
[2] Los Alamos Natl Lab, Space & Remote Sensing Sci Grp, Los Alamos, NM USA
[3] Univ Sci & Technol Lille, Lab Opt Atmospher, F-59655 Villeneuve Dascq, France
关键词
cloud; fractal; inhomogeneity; radiative transfer; infra-red; stochastic processes;
D O I
10.1016/j.atmosres.2004.03.018
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We analyze the effects of flat and bumpy top, fractional and internally inhomogeneous cloud layers on large area-averaged thermal radiative fluxes. Inhomogeneous clouds are generated by a new stochastic model: the tree-driven mass accumulation process (tdMAP). This model is able to provide stratocumulus and cumulus cloud fields with properties close to those observed in real clouds. A sensitivity study of cloud parameters is done by analyzing differences between 3D fluxes simulated by the spherical harmonic discrete ordinate method and three "standard" models likely to be used in general circulation models: plane-parallel homogeneous cloud model (PPH), PPH with fractional cloud coverage model (FCPPH) and independent pixel approximation model (IPA). We show that thermal fluxes are strong functions of fractional cloud coverage, mean optical depth, mean geometrical thickness and cloud base altitude. Fluctuations of "in-cloud" horizontal variability in optical depth and cloud-top bumps have negligible effects in the whole. We also showed that PPH, FCPPH and IPA models are not suitable to compute thermal fluxes of flat top fractional inhomogeneous cloud layer, except for completely overcast cloud. This implies that horizontal transport of photon at thermal wavelengths is important when cloudy cells are separated by optically thin regions. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:291 / 315
页数:25
相关论文
共 98 条
[21]  
Cairns B, 2000, J ATMOS SCI, V57, P700, DOI 10.1175/1520-0469(2000)057<0700:AWICAI>2.0.CO
[22]  
2
[23]  
Carvalho LMV, 1998, J APPL METEOROL, V37, P1265, DOI 10.1175/1520-0450(1998)037<1265:AAOFBD>2.0.CO
[24]  
2
[25]  
Chambers LH, 2001, J APPL METEOROL, V40, P2144, DOI 10.1175/1520-0450(2001)040<2144:SFFSMR>2.0.CO
[26]  
2
[27]  
Chevallier F, 1998, J APPL METEOROL, V37, P1385, DOI 10.1175/1520-0450(1998)037<1385:ANNAFA>2.0.CO
[28]  
2
[29]  
DAVIES R, 1978, J ATMOS SCI, V35, P1712, DOI 10.1175/1520-0469(1978)035<1712:TEOFGO>2.0.CO
[30]  
2