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ENTRAINMENT OF AIR INTO A CUMULUS CLOUD
Publisher: American Meteorological Society
Abstract: A theory of convective clouds is presented, the fundamental hypothesis being that the ascending current in a cloud entrains air from its surroundings. A method is developed for computing the amount of entrainment from a ...
Equatorial Current Observations in the Western Indian Ocean in 1975 and 1976
Publisher: American Meteorological Society
Abstract: Vertical profiles of current, temperature and salinity were taken in the upper ocean from 3°S to 2°N along 55°30?E in the Indian Ocean during February?June in 1975 and 1976. During both years a strong O(80 cm s?1) equatorial ...
Gyres Driven by Combined Wind and Buoyancy Flux
Publisher: American Meteorological Society
Abstract: The combined effects of buoyancy forcing and wind in a gyre-scale steady ocean circulation are modeled using discrete layers with an interfacial flux, not necessarily vertical. The equations for vorticity conservation of ...
Onset of the Southwest Monsoon over the Arabian Sea from Marine Reports of Surface Winds: Structure and Variability
Publisher: American Meteorological Society
Abstract: The time and type of onset of the southwest monsoon over the Arabian Sea is studied using ship reports of surface wind tabulated by 1° squares daily along two densely occupied shipping lanes. It is found that several types ...
Self-sustained Inertial Oscillations
Publisher: American Meteorological Society
Abstract: The authors describe a self-sustaining baroclinic inertial oscillation whose energy source rests in a uniform horizontal temperature gradient. This energy is released through the agency of a stratification-dependent mixing ...
Four Views of a Portion of the North Atlantic Subtropical Gyre
Publisher: American Meteorological Society
Abstract: Data from four cruises to the ??-triangle? centered at 27°N, 32°30?W were smoothed by fitting second-degree polynomials at each of about 30 different density surfaces. The density intervals were ?σp=0.3?, corresponding to ...