Atmospheric Aerosol Optical Properties in the Persian Gulf Region

dc.contributor.authorSmirnov, Alexander
dc.contributor.authorHolben, Brent N.
dc.contributor.authorDubovik, Oleg
dc.contributor.authorNeill, Norm T. O’
dc.contributor.authorEck, Thomas
dc.contributor.authorWestphal, Douglas L.
dc.contributor.authorGoroch, Andreas K.
dc.contributor.authorPietras, Christophe
dc.contributor.authorSlutsker, Ilya
dc.date.accessioned2024-04-29T17:00:39Z
dc.date.available2024-04-29T17:00:39Z
dc.description.abstractAerosol optical depth measurements over Bahrain acquired through the ground-based Aerosol Robotic Network are analyzed. Optical depths obtained from ground-based sun/sky radiometers showed a pronounced temporal trend, with a maximum dust aerosol loading observed during the March to July period. The aerosol optical depth probability distribution is rather narrow with a modal value of about 0.25. The Angstrom parameter frequency distribution has two peaks. One peak around 0.7 characterizes a situation when dust aerosol is more dominant, the second peak around 1.2 corresponds to relatively dust-free cases. The correlation between aerosol optical depth and water vapor content in the total atmospheric column is strong (correlation coefficient of 0.82) when dust aerosol is almost absent (Angstrom parameter is greater than 0.7), suggesting possible hygroscopic growth of fine mode particles or source region correlation, and much weaker (correlation coefficient of 0.45) in the presence of dust (Angstrom parameter is less than 0.7). Diurnal variations of the aerosol optical depth and precipitable water were insignificant. Angstrom parameter diurnal variability (~20-25%) is evident during the April-May period, when dust dominated the atmospheric optical conditions. Variations in the aerosol volume size distributions retrieved from spectral sun and sky radiance data are mainly associated with the changes in the concentration of the coarse aerosol fraction (variation coefficient of 61%). Geometric mean radii for the fine and coarse aerosol fractions are 0.14 µm (s.d.=0.02) and 2.57 µm (s.d.=0.27), respectively. The geometric standard deviation of each fraction is 0.41 and 0.73 respectively. In dust-free conditions the single-scattering albedo (SSA) decreases with wavelength, while in the presence of dust the SSA either stays neutral or increases slightly with wavelength. The changes in the Angstrom parameter derived from ground-based nephelometer and co-located sunphotometer during the initial checkout period were quite similar.
dc.description.sponsorshipThe authors thank Dr. Robert Curran of NASA Headquarters and Dr. Michael King of the EOS Project Science Office for their support. The support of the Office of Naval Research and Naval Research Laboratory through programs PE-0602435N and PE-06-1153 is gratefully acknowledged. The authors would like to thank R.Fraser and R.Ferek for fruitful discussions of certain issues. The authors would also like to acknowledge the constructive criticism of anonymous reviewers.
dc.description.urihttps://gacp.giss.nasa.gov/publications/special/smirnov01.pdf
dc.format.extent41 pages
dc.genrejournal articles
dc.genrepreprints
dc.identifierdoi:10.13016/m2lalr-a3py
dc.identifier.urihttp://hdl.handle.net/11603/33350
dc.language.isoen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.titleAtmospheric Aerosol Optical Properties in the Persian Gulf Region
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0001-9801-1610

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