Parameterization of optical properties for hydrated internally mixed aerosol

被引:122
作者
Ghan, Steven J. [1 ]
Zaveri, Rahul A. [1 ]
机构
[1] Pacific NW Natl Lab, Richland, WA 99352 USA
关键词
SULFATE AEROSOLS; BLACK CARBON; FOSSIL-FUEL;
D O I
10.1029/2006JD007927
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] The optical properties of an internally mixed aerosol with a lognormal size distribution can be approximated in terms of analytic functions of the wet surface mode radius with coefficients that can be related to the wet refractive index. The wet radius is calculated from the dry radius and relative humidity using either the Kohler theory or the MOSAIC thermodynamic model. The hydration state of the aerosol in the hysteresis region between the crystallization and deliquescence relative humidities is diagnosed by comparing the aerosol water from the previous time step with the current water content of the hydrated aerosol. The wet refractive index is estimated from the volume fractions and refractive indices of all components of the aerosol, including water, using volume mixing for soluble components and an effective medium approximation for the insoluble components. The parameterization is evaluated by comparing with Mie solutions for ammonium sulfate, black carbon, and a 50: 50 mixture for a wide range in size distributions and relative humidity. Errors are usually less than 20% and are less then 30% for all conditions except when absolute values are small. The parameterization is suitable for any aerosol model that uses lognormal size distributions composed of internal mixtures of multiple aerosol components.
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页数:10
相关论文
共 20 条
[1]  
[Anonymous], ADV AGRON, DOI DOI 10.1016/S0065-2113(08)60142-X
[2]  
Bohren C. F., 1983, Absorption and Scattering of Light By Small Particles, DOI 10.1002/9783527618156
[3]   Cloud susceptibility and the first aerosol indirect forcing: Sensitivity to black carbon and aerosol concentrations [J].
Chuang, CC ;
Penner, JE ;
Prospero, JM ;
Grant, KE ;
Rau, GH ;
Kawamoto, K .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D21) :AAC10-1
[4]   SCATTERING OF ELECTROMAGNETIC-WAVES BY COMPOSITE SPHERICAL-PARTICLES - EXPERIMENT AND EFFECTIVE MEDIUM APPROXIMATIONS [J].
CHYLEK, P ;
SRIVASTAVA, V ;
PINNICK, RG ;
WANG, RT .
APPLIED OPTICS, 1988, 27 (12) :2396-2404
[5]   Evaluation of aerosol direct radiative forcing in MIRAGE [J].
Ghan, S ;
Laulainen, N ;
Easter, R ;
Wagener, R ;
Nemesure, S ;
Chapman, E ;
Zhang, Y ;
Leung, R .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D6) :5295-5316
[6]   Climate response of fossil fuel and biofuel soot, accounting for soot's feedback to snow and sea ice albedo and emissivity [J].
Jacobson, MZ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D21) :D212011-15
[7]   A physically-based treatment of elemental carbon optics: Implications for global direct forcing of aerosols [J].
Jacobson, MZ .
GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (02) :217-220
[8]   Analysis of aerosol interactions with numerical techniques for solving coagulation, nucleation, condensation, dissolution, and reversible chemistry among multiple size distributions [J].
Jacobson, MZ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D19) :AAC2-1
[9]   Global direct radiative forcing due to multicomponent anthropogenic and natural aerosols [J].
Jacobson, MZ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D2) :1551-1568
[10]   Radiative forcing due to sulfate aerosols from simulations with the National Center for Atmospheric Research Community Climate Model, Version 3 [J].
Kiehl, JT ;
Schneider, TL ;
Rasch, PJ ;
Barth, MC ;
Wong, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D1) :1441-1457