Remote sensing of smoke from MODIS airborne simulator during the SCAR-B experiment

被引:61
作者
Chu, DA
Kaufman, YJ
Remer, LA
Holben, BN
机构
[1] NASA, Goddard Space Flight Ctr, Sci Syst & Applicat Inc, Greenbelt, MD 20771 USA
[2] NASA, Goddard Space Flight Ctr, Atmospheres Lab, Greenbelt, MD 20771 USA
[3] NASA, Goddard Space Flight Ctr, Terr Phys Lab, Greenbelt, MD 20771 USA
关键词
D O I
10.1029/98JD01148
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
MODIS (moderate resolution imaging spectroradiometer) airborne simulator (MAS) data acquired during the SCAR-B (Smoke, Clouds, and Radiation-Brazil) experiment provide a test bed to evaluate aerosol retrievals for MODIS measurements over land. The SCAR-B MAS data covered forest and cerrado regions with varying smoke concentration as a result of fires in August-September, 1995. Excellent agreement is obtained by comparing the retrieved aerosol optical thickness from the MAS data with AERONET (Aerosol Robotic Network) ground-based Sun photometer observations. The evaluation of MODIS aerosol algorithm was performed for a range of smoke optical thickness from 0.1 to 2 at 0.66 mu m wavelength over cerrado and forest sites. All the retrieved values of optical thickness are found within the anticipated retrieval errors of Delta tau = +/-0.05+/-0.2 tau. This confirms for smoke aerosol the validity of the MODIS algorithms and the use of the new dynamic aerosol models in this algorithm (the algorithm was already validated previously for urban/industrial aerosol). The retrieved optical thickness is found to be very sensitive to the assumed value of the single-scattering albedo but not sensitive to the aerosol refractive index (real part). The single-scattering albedo of 0.90 suggested in the aerosol model yields the best results. Test of the MODIS use of a grid box of 10 x 10 km in the aerosol algorithm shows that the standard deviation of the retrieved aerosol should generally not be more than 10% of the average value for a large range of optical thickness values from 0.2 to 2.0, close and far from fires.
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收藏
页码:31979 / 31987
页数:9
相关论文
共 43 条
  • [1] ACKERMANN S, 1997, DISCRIMINATING CLEAR
  • [2] Andreae M.O., 1995, World Survey of Climatology, vol. 16, V16, P341, DOI 10.1016/S0168-6321(06)80033-7
  • [3] ANDREAE MO, 1996, BIOMASS BURNING GLOB, P278
  • [4] Braslau N., 1973, Journal of Applied Meteorology, V12, P601, DOI 10.1175/1520-0450(1973)012<0601:EOAOTT>2.0.CO
  • [5] 2
  • [6] CLIMATE FORCING BY ANTHROPOGENIC AEROSOLS
    CHARLSON, RJ
    SCHWARTZ, SE
    HALES, JM
    CESS, RD
    COAKLEY, JA
    HANSEN, JE
    HOFMANN, DJ
    [J]. SCIENCE, 1992, 255 (5043) : 423 - 430
  • [7] A MODIFIED FOURIER TRANSFORM METHOD FOR MULTIPLE SCATTERING CALCULATIONS IN A PLANE PARALLEL MIE ATMOSPHERE
    DAVE, JV
    GAZDAG, J
    [J]. APPLIED OPTICS, 1970, 9 (06): : 1457 - &
  • [8] Sun photometric measurements of atmospheric water vapor column abundance in the 940-nm band
    Halthore, RN
    Eck, TF
    Holben, BN
    Markham, BL
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D4) : 4343 - 4352
  • [9] SUN AND DUST VERSUS GREENHOUSE GASES - AN ASSESSMENT OF THEIR RELATIVE ROLES IN GLOBAL CLIMATE CHANGE
    HANSEN, JE
    LACIS, AA
    [J]. NATURE, 1990, 346 (6286) : 713 - 719
  • [10] SPATIAL AND TEMPORAL DISTRIBUTION OF TROPICAL BIOMASS BURNING
    HAO, WM
    LIU, MH
    [J]. GLOBAL BIOGEOCHEMICAL CYCLES, 1994, 8 (04) : 495 - 503