HR: 1340h
AN: A33C-1406    [Abstracts]
TI: Satellite retrieved aerosol extinction coefficients for sensor performance in the coastal zone
AU: * Schoemaker, R M
EM: robin.schoemaker@orange.nl
AF: TNO Defence, Security and Safety, Oude Waalsdorperweg 63, The Hague, 2597 AK, Netherlands
AU: van Eijk, A M
EM: lex.vaneijk@tno.nl
AF: TNO Defence, Security and Safety, Oude Waalsdorperweg 63, The Hague, 2597 AK, Netherlands
AB: Littoral characterization and sensor performance assist in optimizing the efficiency and safety of operations in the area. The environmental conditions of the marine boundary layer (MBL) – due to weather and atmospheric effects – change continuously in space and time, which certainly holds for the aerosol make-up. Models have been developed to describe the electro-optical propagation in the boundary layer as a function of meteorological parameters. EOSTAR is such an end-to-end model suite for electro-optical sensor performance in which the Advanced Navy Aerosol Model (ANAM) is embedded for computing the aerosol extinction. While ANAM provides favourable results in open ocean conditions, in coastal zones the model lacks accuracy due to the presence of aerosols from a variety of sources that need to be assessed. In offshore wind conditions continental aerosols of anthropogenic and natural origin mix with marine aerosols produced in the surf zone and by wave breaking further offshore. Radiometers on satellites can be used to retrieve the spatial variation over an extended area determined by the swath width, with a resolution determined by the radiometer pixel size. More accurate information on the aerosol properties in larger coastal domains are required to correctly handle the aerosol influence on transmission characteristics in the coastal zone. Results from in situ measurements off the coast of Italy in April 2007 are presented in this analysis. For one particular day, the satellite retrieved aerosol optical thickness (AOT) is to be compared with hand-held sun photometer measurements for quality assessment. The AOT values are converted into aerosol extinction coefficients for a pre-defined path. For one visible wavelength channel the transmission loss is computed with these coefficients, which is compared with the computed transmission loss for the path in case of a) a single extinction coefficient obtained from measurements and b) a modeled extinction coefficient obtained from ANAM.
DE: 0305 Aerosols and particles (0345, 4801, 4906)
DE: 1640 Remote sensing (1855)
DE: 4801 Aerosols (0305, 4906)
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting