Physics
Scientific paper
Dec 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002georl..29w..31k&link_type=abstract
Geophysical Research Letters, Volume 29, Issue 23, pp. 31-1, CiteID 2116, DOI 10.1029/2001GL014492
Physics
22
Atmospheric Composition And Structure: Aerosols And Particles (0345, 4801), Global Change: Remote Sensing
Scientific paper
Data from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument that flies in polar orbit on the Terra and Aqua satellites, are used to derive the aerosol optical thickness and properties over land and ocean. The relationships between visible reflectance (at blue, ρblue, and red, ρred), and mid-infrared (at 2.1 μm, ρ2.1) are used in the MODIS aerosol retrieval algorithm to derive global distribution of aerosols over land. These relations have been established from a series of measurements indicating that ρblue ~ 0.5 ρred ~ 0.25 ρ2.1. Here we use a model to describe the transfer of radiation through a vegetation canopy composed of randomly oriented leaves to assess the theoretical foundations for these relationships. Calculations for a wide range of leaf area indices and vegetation fractions show that ρblue is consistently about 1/4 of ρ2.1 as used by MODIS for the whole range of analyzed cases, except for very dark soils, such as those found in burn scars. For its part, the ratio ρred/ρ2.1 varies from less than the empirically derived value of 1/2 for dense and dark vegetation, to more than 1/2 for bright mixture of soil and vegetation. This is in agreement with measurements over uniform dense vegetation, but not with measurements over mixed dark scenes. In the later case, the discrepancy could be probably mitigated by shadows due to uneven canopy and terrain on a large scale.
Gobron Nadine
Kaufman Yoram J.
Pinty Bernard
Verstraete Michel M.
Widlowski Jean-Luc
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