Marine stratocumulus structure

Abstract

Thirty-three Landsat TM scenes of California stratocumulus cloud fields were acquired as part of the FIRE Marine Stratocumulus Intensive Field Observations in July 1987. They exhibit a wide variety of stratocumulus structures. Analysis has so far focused upon the 7 July scene, in which aircraft from NASA, NCAR, and the British Meteorological Office repeatedly gathered data across a stratocumulus-fair weather cumulus transition. The aircraft soundings validate the cloud base temperature threshold determined by spatial coherence analysis of the TM thermal band. Brightness variations in the stratocumulus region exhibit a − 5 3 power-law decrease of the wavenumber spectra for scales larger than the cloud thickness, about 200 m, changing to a −3 power at smaller scales. Observations by an upward-looking three-channel microwave radiometer on San Nicolas Island also show the − 5 3 power-law in total integrated liquid water, suggesting that the larger-scale TM brightness variations are primarily due to variations in the liquid water. The Kolmogorov 5 3 power suggests that for some purposes liquid water in turbulent stratocumulus clouds may be treated as a passive scalar, simply reflecting variations in vertical velocity. This may be tested using the velocities measured by the aircraft.