The Advanced Navy Aerosol Model (ANAM): validation of small-particle modes

The image quality of electro-optical sensors in the (lower-altitude marine) atmosphere is limited by aerosols, which cause contrast reduction due to transmission losses and impact on the thermal signature of objects by scattering solar radiation. The Advanced Navy Aerosol Model (ANAM) aims at providing a quantitative estimate of the aerosol effects on the basis of standard meteorological parameters such as wind speed and relative humidity. For application in coastal regions, the ANAM includes non-marine aerosols that are governed by an ill-defined tuning parameter: the air mass parameter (AMP). The present paper proposes a new parameterization for assessing the effect of these non-marine particles on the propagation. The new parameterization utilizes the Ångström coefficient, which can be experimentally obtained with a sun photometer, and introduces new types of aerosols in ANAM. The new parameterization was tested against experimental validation data acquired at Porquerolles Island at the French Riviera. The limited test data suggested that the new parameterization is only partially efficient in capturing the aerosol signature of the coastal environment. Nevertheless, the new Ångström coefficient algorithm avoids using the ill-defined AMP, and may thus be useful to the ANAM community.

[1]  J. Kusmierczyk-Michulec,et al.  Angström coefficient as an indicator of the atmospheric aerosol type for a well-mixed atmospheric boundary layer: Part 1: Model development , 2009 .

[2]  Stuart G. Gathman,et al.  Optical Properties Of The Marine Aerosol As Predicted By The Navy Aerosol Model , 1983 .

[3]  Gerrit de Leeuw,et al.  Modeling aerosol extinction in a coastal environment , 1992 .

[4]  Jolanta Kusmierczyk-Michulec,et al.  Ångström coefficient as a tracer of the continental aerosols , 2007, SPIE Optical Engineering + Applications.

[5]  G. Tedeschi,et al.  Sea‐spray aerosol particles generated in the surf zone , 2011 .

[6]  Frédéric Bouchara,et al.  Development of the Mediterranean extinction code (MEDEX) , 2003 .

[7]  Alexander M. J. van Eijk,et al.  The Ångström coefficient as an indicator of non-marine particles in ANAM (Advanced Navy Aerosol Model) , 2009, Optical Engineering + Applications.

[8]  A. Sorooshian,et al.  An aerosol climatology for a rapidly growing arid region (southern Arizona): Major aerosol species and remotely sensed aerosol properties. , 2011, Journal of geophysical research. Atmospheres : JGR.

[9]  Gerrit de Leeuw,et al.  Modeling aerosol particle size distributions over the North Sea , 1992 .

[10]  A. M. J. van Eijk,et al.  Improvements in the Advanced Navy Aerosol Model (ANAM) , 2006, SPIE Optics + Photonics.

[11]  C. O'Dowd,et al.  Marine aerosol production: a review of the current knowledge , 2007, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[12]  A. Smirnov,et al.  AERONET-a federated instrument network and data archive for aerosol Characterization , 1998 .

[13]  Anders Ångström,et al.  On the Atmospheric Transmission of Sun Radiation and on Dust in the Air , 1929 .

[14]  Gerrit de Leeuw,et al.  Near-surface aerosol transmission in the marine environment , 2003, SPIE Remote Sensing.

[15]  I. Tang Chemical and size effects of hygroscopic aerosols on light scattering coefficients , 1996 .