Retrieval of aerosol optical depth in vicinity of broken clouds from reflectance ratios: Sensitivity study

被引:19
作者
Kassianov, Evgueni [1 ]
Ovchinnikov, Mikhail [1 ]
Berg, Larry K. [1 ]
McFarlane, Sally A. [1 ]
Flynn, Connor [1 ]
机构
[1] Pacific NW Natl Lab, Richland, WA 99352 USA
基金
美国国家航空航天局;
关键词
Continental cumulus clouds; Aerosol optical depth; Multi-spectral reflectance; ATMOSPHERIC RADIATION MEASUREMENT; MODIS; ABSORPTION; ALBEDO;
D O I
10.1016/j.jqsrt.2009.01.014
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
We conducted a sensitivity study to better understand the potential of a new method for retrieving aerosol optical depth (AOD) under partly cloudy conditions. This method exploits ratios of reflectances in the visible spectral range and provides an effective way to avoid three-dimensional (3D) cloud effects. The sensitivity study is performed for different observational conditions and random errors in input data. The results of the sensitivity study suggest that this ratio method has the ability to detect clear pixels even in close proximity to clouds. Such detection does not require a statistical analysis of the two-dimensional (2D) horizontal distribution of reflected solar radiation, which makes it suitable for operational retrievals. in comparison with previously suggested approaches, the ratio method has the capability to increase the "harvest" of clear pixels. Similar to the traditional independent pixel approximation (IPA), the ratio method has a low computational cost for retrieving AOD. In contrast to the IPA method, the ratio method provides much more accurate estimations of the AOD values under broken cloud conditions: pixel-based and domain-averaged estimations of errors in AOD are about 25% and 10%, respectively. Finally, both the ratio-based cloud screening and the accuracy of domain-averaged ratio-based AOD values do not suffer greatly when 5% random errors are introduced in the reflectances. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1677 / 1689
页数:13
相关论文
共 33 条
[1]   Discriminating clear sky from clouds with MODIS [J].
Ackerman, SA ;
Strabala, KI ;
Menzel, WP ;
Frey, RA ;
Moeller, CC ;
Gumley, LE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D24) :32141-32157
[2]   The 13RC -: Bringing together the most advanced radiative transfer tools for cloudy atmospheres [J].
Cahalan, RF ;
Oreopoulos, L ;
Marshak, A ;
Evans, KF ;
Davis, AB ;
Pincus, R ;
Yetzer, KH ;
Mayer, B ;
Davies, R ;
Ackerman, TP ;
Barker, HW ;
Clothiaux, EE ;
Ellingson, RG ;
Garay, MJ ;
Kassianov, E ;
Kinne, S ;
Macke, A ;
O'Hirok, W ;
Partain, PT ;
Prigarin, SM ;
Rublev, AN ;
Stephens, GL ;
Szczap, F ;
Takara, EE ;
Várnai, T ;
Wen, GY ;
Zhuravleva, TB .
BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2005, 86 (09) :1275-+
[3]  
CHIU J, 2008, ATMOS CHEM PHYS DISC, V8, P17549
[4]  
d'Entremont RP, 2003, EARTH INTERACT, V7, DOI 10.1175/1087-3562(2003)007<0001:AOGSIU>2.0.CO
[5]  
2
[6]   A first look at band-differenced angular signatures for cloud detection from MISR [J].
Di Girolamo, L ;
Wilson, MJ .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2003, 41 (07) :1730-1734
[7]  
Dubovik O, 2002, J ATMOS SCI, V59, P590, DOI 10.1175/1520-0469(2002)059<0590:VOAAOP>2.0.CO
[8]  
2
[9]   The potential for improved boundary layer cloud optical depth retrievals from the multiple directions of MISR [J].
Evans, K. Franklin ;
Marshak, Alexander ;
Varnai, Tamas .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2008, 65 (10) :3179-3196
[10]   Retrieval and climatology of the aerosol asymmetry parameter in the NOAA aerosol monitoring network [J].
Fiebig, M. ;
Ogren, J. A. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D21)