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A Note on the Linearized Form of the Kinematic Bottom Boundary Condition
Publisher: American Meteorological Society
Abstract: The exact kinematic bottom boundary condition is w = u·?h. The linearized form in an incompressible flow is w = ?·(uh at z = 0. Use of the approximate linearized form w = u·?h at z = 0 eliminates the phase shift of the ...
A CENSUS OF CUMULUS-CLOUD HEIGHT VERSUS PRECIPITATION IN THE VICINITY OF PUERTO RICO DURING THE WINTER AND SPRING OF 1953-1954
Publisher: American Meteorological Society
Abstract: The analysis of fifteen cloud-census flights confirms the common existence of warm precipitation from trade-wind cumuli. A probability that over-water clouds of certain vertical developments will contain precipitation is ...
Resolved Order of Scattering for the Solution of Radiative Transfer Equation
Publisher: The American Society of Mechanical Engineers (ASME)
Abstract: The solution of the radiative transfer equation (RTE) becomes complicated when the participating medium is scattering and/or the boundary walls are reflecting. To reduce the complexity, the resolved order of scattering ...
BoBBLE: Ocean–Atmosphere Interaction and Its Impact on the South Asian Monsoon
Publisher: American Meteorological Society
Abstract: AbstractThe Bay of Bengal (BoB) plays a fundamental role in controlling the weather systems that make up the South Asian summer monsoon system. In particular, the southern BoB has cooler sea surface temperatures (SST) that ...