International audienceThe vertical and horizontal transport of aerosols generated over the surf zone is discussed. Experimental data were collected during the second campaign of the Surf Zone Aerosol Experiment that took place in Duck NC (USA) in November 2007. The Empirical Orthogonal Function (EOF) method was used to analyze the vertical concentration gradients, and allowed separating the surf aerosols from aerosols advected from elsewhere. The numerical Marine Aerosol Concentration Model (MACMod) supported the analysis by confirming that the concentration gradients are more pronounced under stable conditions and that aerosol plumes are then more confined to the surface. The model also confirmed the experimental observations made during t...
The aerosol produced by waves breaking in the surf zone is important for a variety of processes, suc...
The work performed in 1992 in the framework of the EUROTRAC subproject ASE was mainly focused on thr...
Results are presented from measurements in the lower 15 m of the marine atmospheric surface layer. T...
International audienceThe vertical and horizontal transport of aerosols generated over the surf zone...
International audienceSea-salt aerosol concentrations in the coastal zone are assessed with the nume...
International audienceMarine aerosols constitute one of the most significant part to the global aero...
International audienceTo assess the properties of aerosol particles generated over the surf zone, tw...
quantitative source function for sea spray aerosol produced by waves breaking in the surf zone was d...
The first results are presented from a quantitative model describing the aerosol production in the s...
The Coastal Aerosol Transport (CAT) model was developed to study the evolution of aerosol particle s...
Improving the United States' electromagnetic (EM) and electro-optical (EO) prediction capabilities i...
Production mechanisms of aerosol chemical species, in terms of primary and secondary processes, were...
The aerosol production in the surfzone, as determined from measurements, at two sites along the Cali...
An extensive data set of aerosol vertical concentration profiles (height range 0.5-15 meters, diamet...
Sea spray aerosol is a product of wave breaking. A very strong source of this aerosol is the surf zo...
The aerosol produced by waves breaking in the surf zone is important for a variety of processes, suc...
The work performed in 1992 in the framework of the EUROTRAC subproject ASE was mainly focused on thr...
Results are presented from measurements in the lower 15 m of the marine atmospheric surface layer. T...
International audienceThe vertical and horizontal transport of aerosols generated over the surf zone...
International audienceSea-salt aerosol concentrations in the coastal zone are assessed with the nume...
International audienceMarine aerosols constitute one of the most significant part to the global aero...
International audienceTo assess the properties of aerosol particles generated over the surf zone, tw...
quantitative source function for sea spray aerosol produced by waves breaking in the surf zone was d...
The first results are presented from a quantitative model describing the aerosol production in the s...
The Coastal Aerosol Transport (CAT) model was developed to study the evolution of aerosol particle s...
Improving the United States' electromagnetic (EM) and electro-optical (EO) prediction capabilities i...
Production mechanisms of aerosol chemical species, in terms of primary and secondary processes, were...
The aerosol production in the surfzone, as determined from measurements, at two sites along the Cali...
An extensive data set of aerosol vertical concentration profiles (height range 0.5-15 meters, diamet...
Sea spray aerosol is a product of wave breaking. A very strong source of this aerosol is the surf zo...
The aerosol produced by waves breaking in the surf zone is important for a variety of processes, suc...
The work performed in 1992 in the framework of the EUROTRAC subproject ASE was mainly focused on thr...
Results are presented from measurements in the lower 15 m of the marine atmospheric surface layer. T...