OS044-0005
Absorption and scattering by active and residual sea foam at millimeter-wave frequencies
Abstract:
Foam emissivity is the basis of passive remote sensing of whitecap fraction W from ocean surface brightness temperature TB. Radiometric W measurements can provide observations of air-sea fluxes of momentum, heat, and mass. Reliable estimates of air-sea fluxes is necessary for accurate representation of the ocean-atmosphere coupling in weather, wave, and climate models. Microwave radiometers (1 to 40 GHz) retrieve W at low spatial resolution, which is acceptable for open ocean where the conditions are relatively homogeneous over expansive areas. However, it is a limiting factor when approaching land or ice. Therefore, radiometric surface observations at higher resolution are necessary to monitor the dynamic and complex environments in coastal zones and polar regions.
To this end, we assess the feasibility of using the surface signal at mmW frequencies (40 to 200 GHz) to detect whitecaps. We need to investigate three aspects to achieve this goal, namely: (1) Evaluate the sensitivity of foam-covered surface signal to the atmospheric signal; (2) Evaluate the performance of existing models in representing the rough sea surface; (3) Develop a model for the emissivity of sea foam at mmW frequencies that accounts for both absorption and scattering. The work presented here focuses on the third aspect, i.e., foam scattering. We will describe our method, present results, and discuss the dependence of foam scattering on radiometric frequency and dimensions of different foam structures.