Open AccessAn observational study of the relationship between cloud, aerosol and meteorology in broken low‐level cloud conditions
Author(s) -
Loeb Norman G.,
Schuster Gregory L.
Publication year - 2008
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jd009763
Subject(s) - aerosol , angstrom exponent , cloud cover , cloud fraction , longitude , environmental science , atmospheric sciences , latitude , cloud computing , satellite , liquid water content , optical depth , meteorology , atmosphere (unit) , cloud top , climatology , radiative transfer , sea salt aerosol , geography , geology , physics , geodesy , quantum mechanics , astronomy , computer science , operating system , sea salt
Global satellite analyses showing strong correlations between aerosol optical depth and cloud cover have stirred much debate recently. While it is tempting to interpret the results as evidence of aerosol enhancement of cloud cover, other factors such as the influence of meteorology on both the aerosol and cloud distributions can also play a role, as both aerosols and clouds depend upon local meteorology. This study uses satellite observations to examine aerosol‐cloud relationships for broken low‐level cloud regions off the coast of Africa. The analysis approach minimizes the influence of large‐scale meteorology by restricting the spatial and temporal domains in which the aerosol and cloud properties are compared. While distributions of several meteorological variables within 5° × 5° latitude‐longitude regions are nearly identical under low and high aerosol optical depth, the corresponding distributions of single‐layer low cloud properties and top‐of‐atmosphere radiative fluxes differ markedly, consistent with earlier studies showing increased cloud cover with aerosol optical depth. Furthermore, fine‐mode fraction and Angstrom Exponent are also larger in conditions of higher aerosol optical depth, even though no evidence of systematic latitudinal or longitudinal gradients between the low and high aerosol optical depth populations are observed. When the analysis is repeated for all 5° × 5° latitude‐longitude regions over the global oceans (after removing cases in which significant meteorological differences are found between the low and high aerosol populations), results are qualitatively similar to those off the coast of Africa.