MODIS aerosol product analysis for data assimilation: Assessment of over-ocean level 2 aerosol optical thickness retrievals

被引:211
作者
Zhang, Jianglong [1 ]
Reid, Jeffrey S. [1 ]
机构
[1] USN, Res Lab, Marine Meteorol Div, Monterey, CA 93940 USA
关键词
D O I
10.1029/2005JD006898
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Currently, the Moderate-resolution Imaging Spectroradiometers (MODIS) level II aerosol product (MOD04/MYD04) is the best aerosol optical depth product suitable for near-real-time aerosol data assimilation. However, a careful analysis of biases and error variances in MOD04/MYD04 aerosol optical depth product is necessary before implementing the MODIS aerosol product in aerosol forecasting applications. Using 1 year's worth of Sun photometer and MOD04/MYD04 aerosol optical depth (tau) data over global oceans, we studied the major biases in MODIS aerosol over-ocean product due to wind speed, cloud contamination, and aerosol microphysical properties. For t less than 0.6, we found similar uncertainties in the mean MOD04/MYD04 tau as suggested by the MODIS aerosol group, while biases are nonlinear for tau larger than 0.6. We showed that uncertainties in MOD04/MYD04 data can be reduced, and the correlation between MODIS and Sun photometer t can be improved by reducing the systematic biases in MOD04/MYD04 data through empirical corrections and quality assurance procedures. By removing noise and outliers and ensuring that only the highest-quality data were included, we created a modified aerosol optical depth product that removes most massive outliers and ultimately reduced the absolute error (MODIS-Sun photometer) in MODIS tau at 0.55 mu m (tau(0.55)) by 10-20%. Averaged over 1 year's worth of Terra MODIS aerosol product over global oceans, we found a 12% reduction in MODIS tau(0.55) with extremes of 30% over the southern midlatitudes and the North Pacific due to a reduction in cloud contamination. This modified aerosol optical depth product will be used operationally.
引用
收藏
页数:17
相关论文
共 32 条
[1]   Testing the MODIS satellite retrieval of aerosol fine-mode fraction [J].
Anderson, TL ;
Wu, YH ;
Chu, DA ;
Schmid, B ;
Redemann, J ;
Dubovik, O .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2005, 110 (D18) :1-16
[2]  
Chu D.A., 2002, GEOPHYS RES LETT, V29, pGL013205, DOI [10.1029/2001GL013205, DOI 10.1029/2001GL013205]
[3]   MEASUREMENT OF THE ROUGHNESS OF THE SEA SURFACE FROM PHOTOGRAPHS OF THE SUNS GLITTER [J].
COX, C ;
MUNK, W .
JOURNAL OF THE OPTICAL SOCIETY OF AMERICA, 1954, 44 (11) :838-850
[4]  
Dabberdt WF, 1996, B AM METEOROL SOC, V77, P305, DOI 10.1175/1520-0477(1996)077<0305:ROFEAO>2.0.CO
[5]  
2
[6]  
Daley R., 1991, Atmospheric data analysis
[7]  
ESPOSITO J, 2004, P SPIE SOC OPT ENG, V5542, P437, DOI DOI 10.1117/12.558106
[8]   An algorithm using visible and 1.38-μm channels to retrieve cirrus cloud reflectances from aircraft and satellite data [J].
Gao, BC ;
Yang, P ;
Han, W ;
Li, RR ;
Wiscombe, WJ .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2002, 40 (08) :1659-1668
[9]  
HOGAN TF, 1993, MON WEATHER REV, V121, P2373, DOI 10.1175/1520-0493(1993)121<2373:SSOTNG>2.0.CO
[10]  
2