Surface-based remote sensing of marine boundary-layer cloud properties

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Abstract

Surface-based measurements are used to define some of the important macrophysical and optical properties of marine clouds. These measurements were taken during five different marine field programs. A progression is made from a midlatitude marine stratocumulus regime with an average cloud fraction of 0.7 and a median cloud base of 460 m to the marine tropical regime with an average cloud fraction of 0.2 and a median cloud base of 1050 m. Measurements of the solar transmission coefficient taken during the Atlantic Stratocumulus Transition Experiment (ASTEX) were used in a radiative transfer algorithm to produce values of albedo, absorption, and optical depth. A microwave radiometer provided measurements of the liquid water path (LWP). -from Authors

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White, A. B., Fairall, C. W., & Snider, J. B. (1995). Surface-based remote sensing of marine boundary-layer cloud properties. Journal of the Atmospheric Sciences, 52(16), 2827–2838. https://doi.org/10.1175/1520-0469(1995)052<2827:SBRSOM>2.0.CO;2

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