Robust optical features of fine mode size distributions: Application to the Québec smoke event of 2002
dc.contributor.author | O'Neill, N. T. | |
dc.contributor.author | Thulasiraman, S. | |
dc.contributor.author | Eck, Thomas | |
dc.contributor.author | Reid, J. S. | |
dc.date.accessioned | 2024-04-29T17:02:04Z | |
dc.date.available | 2024-04-29T17:02:04Z | |
dc.date.issued | 2005-06-08 | |
dc.description.abstract | Simple relationships involving the fundamental parameters of fine mode aerosol optical depth (τf), Angstrom exponent (αf) and its derivative (αf′) as near-monotonic functions of the effective van de Hulst parameter (ρeff,f = 2 (2 π reff,f/λ) ∣m − 1∣) were derived for the conceptual case of a log-translatable particle size distribution (LTPSD). This notion is useful in the interpretation of real sunphotometer data; the fine mode size distribution often approximates a LTPSD while departures from this behavior become more readily understood once one understands the first order optics. The near dependency of the fine mode optical parameters on ρeff,f was also exploited to obtain an explicit expression for ρeff,f as a function of αf and αf′. The relationships were applied to a representative case study to demonstrate their general applicability and then to the specific case of the July 2002 Québec smoke event. A number of illustrations were given where the coherency of the derived relations indicated that the LTPSD concept was often a good approximation to reality. The analysis of the Québec-smoke extinction data showed the existence of a weak but systematic dependence of the Angstrom exponents on smoke trajectory time and by inference a steady growth in particle size with time. The variation of reff,f (derived from AERONET inversions) was however observed to be inconsistent with this dependence unless one redefined this parameter in terms of the clearly delineated peak of the asymmetric fine mode particle size distribution (PSD). This definition led to a re-computed temporal rate of increase in reff,f which was coherent with the variation of the Angstrom parameters and which was coherent with a simple coagulative model based on conservation of volume. It was demonstrated that trajectory time was essentially a proxy variable for reff,f and more fundamentally ρeff,f (as predicted by the LTPSD relations). A similar proxy argument could be applied to the dependence of the Angstrom exponent on optical depth but such arguments are tempered by the relative variations of fine-mode abundance (Af) and particle size (by the value of the parameter γ = dlogAf/dlogreff,f). | |
dc.description.sponsorship | The authors would like to thank the National Aeronautics and Space Administration (NASA), the National Sciences and Engineering Research Council of Canada (NSERC) and the Canadian Foundation for Climate and Atmospheric Sciences (CFCAS) for their financial support. The lead author is especially indebted to Brent Holben at GSFC/NASA as well as Bob Curran at GEST/UMBC (Goddard Earth Sciences and Technology Center at the University of Maryland at Baltimore County) for providing a senior visiting research position. Valuable in-kind support was obtained from the Meteorological Services of Canada (MSC) and the AERONET project. The contributions of Jim Freemantle, the AEROCAN coordinator and Egbert technical manager, Ilya Slutsker and David Gilles of the AERONET group and Alain Royer the co-PI of the AEROCAN network are gratefully acknowledged. Acknowledgments are also due to the PIs at the different AERONET sites employed in this study; Glen Lesins at Halifax, NS, Jay Herman, Maria Tzortziou, and Gordon Labow at SERC (Smithsonian Environmental Research Center) in Edgewater, MD, and Brent Holben the PI at CCNY (City College of New York) NY, COVE (CERES Ocean Validation Experiment) near Virginia Beach, VA, Howland, ME, MDSC (Maryland Science Center), Wallop’s Island VA, Norfolk, VA, and GSFC, MD. Finally, we would like to gratefully acknowledge the constructive criticisms of one reviewer concerning the importance of NO2 absorption to the derived optical statistics. | |
dc.description.uri | https://onlinelibrary.wiley.com/doi/abs/10.1029/2004JD005157 | |
dc.format.extent | 21 pages | |
dc.genre | journal articles | |
dc.identifier | doi:10.13016/m2dlh1-0zhk | |
dc.identifier.citation | O’Neill, N. T., S. Thulasiraman, T. F. Eck, and J. S. Reid. “Robust Optical Features of Fine Mode Size Distributions: Application to the Québec Smoke Event of 2002.” Journal of Geophysical Research: Atmospheres 110, no. D11 (2005). https://doi.org/10.1029/2004JD005157. | |
dc.identifier.uri | https://doi.org/10.1029/2004JD005157 | |
dc.identifier.uri | http://hdl.handle.net/11603/33494 | |
dc.language.iso | en_US | |
dc.publisher | AGU | |
dc.relation.isAvailableAt | The University of Maryland, Baltimore County (UMBC) | |
dc.relation.ispartof | UMBC GESTAR II | |
dc.relation.ispartof | UMBC Faculty collection | |
dc.rights | This 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.rights | Public Domain | |
dc.rights.uri | https://creativecommons.org/publicdomain/mark/1.0/ | |
dc.title | Robust optical features of fine mode size distributions: Application to the Québec smoke event of 2002 | |
dc.type | Text | |
dcterms.creator | https://orcid.org/0000-0001-9801-1610 |
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