148 JOURNAL OF THE ATMOSPHERIC SCIENCES VOLUME 54

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Date: 2016-04-24 12:09:18 Physical quantities Vector calculus Atmospheric thermodynamics Physical oceanography Atmospheric convection Flux Entrainment Surface layer Heat flux Radiative flux Atmospheric entry Energy flux		148 JOURNAL OF THE ATMOSPHERIC SCIENCES VOLUME 54 Add to Reading List Source URL: climate-dynamics.org Download Document from Source Website File Size: 325,32 KB Share Document on Facebook

	Modeling the Atmospheric Boundary Layer Wind Response to Mesoscale Sea Surface Temperature Perturbations Natalie Perlin1, Simon P. de Szoeke2, Dudley B. Chelton2, Roger M. Samelson2, Eric D. Skyllingstad2, and Larry W. O DocID: 1tbqX - View Document
	Oil that is spilled in the ocean floats on the surface of the water. It spreads out quickly to form a thin layer called an oil slick. As the spreading continues, the layer becomes thinner and thinner. It finally becomes DocID: 1sMmj - View Document
	Surface fluxes, temperatures and boundary layer evolution at the building greyzone in London Supervisors: Prof Sue Grimmond (University of Reading), Dr Sylvia Bohnenstengel (Met Office@ Reading), Dr Humphrey Lean (Met Of DocID: 1rY3l - View Document
	Specification for Ocean Surface Vector Stress (OSVS) Preamble/Introduction. Ocean surface vector stress (OSVS) is also the drag at the bottom of the atmosphere and the dynamical forcing at the top of the ocean. OSVS is t DocID: 1reRt - View Document
	KIMBERLITES Kimberlite is an ultrabasic olivine-rich igneous rock called peridotite. Peridotites occur at great depths in the earth in a layer called the mantlemiles below the surface). At this depth the combi DocID: 1reER - View Document