Brightness Temperature Sensitivity to Whitecap Fraction at Millimeter Wavelengths

Accurate representation of the ocean-atmosphere coupling in weather, wave and climate models requires reliable estimates of air-sea surface fluxes of momentum, heat and mass. Whitecap fraction (W) usually quantifies the enhancement of the surface fluxes due to wave breaking. Satellite-based passive...

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Bibliographic Details
Published in:Remote sensing (Basel, Switzerland) Switzerland), 2019, Vol.11 (17), p.2036
Main Authors: Bettenhausen, Michael H., Anguelova, Magdalena D.
Format: Article
Language:English
Subjects:
air-sea interaction
Algorithms
Antennas
Atmospheric models
Brightness
Brightness temperature
Climate models
Coastal zone
Environmental conditions
Feasibility studies
Fluxes
Laboratories
Meteorological satellites
microwave
Millimeter waves
millimeter-wave
Ocean models
Ocean surface
Polar environments
radiometer
Radiometers
Remote sensing
Spatial discrimination
Spatial resolution
Surface brightness
Temperature
Unmanned aerial vehicles
Wave breaking
Wavelengths
Weather
whitecap fraction
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Summary:Accurate representation of the ocean-atmosphere coupling in weather, wave and climate models requires reliable estimates of air-sea surface fluxes of momentum, heat and mass. Whitecap fraction (W) usually quantifies the enhancement of the surface fluxes due to wave breaking. Satellite-based passive remote sensing of W from ocean surface brightness temperatures ( T B s) observes open ocean surface fluxes at low spatial resolution. Radiometric surface observations at higher resolution are necessary to monitor the complex environment in the coastal zone and in polar regions. We assess the feasibility of using the millimeter-wave frequencies (89 to 150 GHz) to observe whitecaps. We evaluate the derivative of the T B with respect to W as a measure for the observation of W. We describe the models and data used to evaluate the T B sensitivity to W for different instrumental and environmental conditions. Atmospheric absorption limits the ability to observe the surface at millimeter-wave frequencies. We find that the T B sensitivity to W at 89 GHz may be sufficient to support limited W retrieval from observations at altitudes below 1 km and that the T B sensitivity at 113 and 150 GHz is not sufficient. Clear skies, and low to moderate atmospheric humidity favor whitecap observations.
ISSN:2072-4292
2072-4292
DOI:10.3390/rs11172036