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Relating MODIS‐derived surface albedo to soils and rock types over Northern Africa and the Arabian peninsula
Author(s) -
Tsvetsinskaya Elena A.,
Schaaf C. B.,
Gao F.,
Strahler A. H.,
Dickinson R. E.,
Zeng X.,
Lucht W.
Publication year - 2002
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2001gl014096
Subject(s) - albedo (alchemy) , shortwave , moderate resolution imaging spectroradiometer , environmental science , vegetation (pathology) , arid , land cover , remote sensing , geology , climatology , shortwave radiation , atmospheric sciences , satellite , radiative transfer , land use , radiation , art , performance art , art history , medicine , paleontology , physics , civil engineering , pathology , quantum mechanics , aerospace engineering , engineering
We use the MODerate resolution Imaging Spectroradiometer (MODIS) aboard the Terra spacecraft to derive surface albedo for the arid areas of Northern Africa and the Arabian peninsula. Albedo in seven MODIS spectral bands for land and three broad bands (for shortwave, near infrared, and visible portions of the spectrum) is produced. Surface albedo is derived from MODIS observations during a sixteen‐day period and is analyzed at 1 km spatial resolution. MODIS data show considerable spatial variability of surface albedo in the study region that is related to soil and geological characteristics of the surface. For example, solar shortwave white‐sky albedo varies by a factor of about 2.5 from the darkest volcanic terrains to the brightest sand sheets. Vegetation contribution to surface reflectance is essentially negligible since we only considered pixels with under 10 percent fractional canopy cover. Few, if any, coupled land‐atmosphere global or regional models capture this observed spatial variability in surface reflectance or albedo. Here we suggest a scheme that relates soil groups (based on the United Nations Food and Agriculture Organization, FAO, soil classification) and rock types (based on the United States Geological Survey, USGS, geological maps) to MODIS derived surface albedo statistics. This approach is a first step towards the incorporation of the observed spatial variability in surface reflective properties into climate models.