Results 301 to 310 of about 536,823 (347)
Haemodiafiltration versus high-flux haemodialysis-a Consensus Statement from the EuDial Working Group of the ERA. [PDF]
Battaglia Y +16 more
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Mixed convection in thermo-gravitational column: a continuous species separation. [PDF]
Sioud K +4 more
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Projected population exposure to dangerous heat stress around Lake Victoria under a high-end climate change scenario. [PDF]
Ramon D +8 more
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ATMOSPHERE-OCEAN, 2022
Convective parameterization is the long-lasting bottleneck of global climate modelling and one of the most difficult problems in atmospheric sciences. Uncertainty in convective parameterization is the leading cause of the widespread climate sensitivity ...
Jialin Lin +8 more
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Convective parameterization is the long-lasting bottleneck of global climate modelling and one of the most difficult problems in atmospheric sciences. Uncertainty in convective parameterization is the leading cause of the widespread climate sensitivity ...
Jialin Lin +8 more
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CONVECTION | Convection in the Ocean
2003This authoritative resource covers all aspects of atmospheric sciences―including both theory and applications. Nearly 350 articles and over 1,900 figures and photographs are presented, many in full-color. The Encyclopediais an ideal resource for academia, government, and industry in the fields of atmospheric, ocean, and environmental sciences.
Soloviev, Alexander, Klinger, B.
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International Journal of Heat and Mass Transfer, 1994
zbMATH Open Web Interface contents unavailable due to conflicting licenses.
L. S. Yao, S. Ghosh Moulic
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zbMATH Open Web Interface contents unavailable due to conflicting licenses.
L. S. Yao, S. Ghosh Moulic
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Solar Convection and Magneto-Convection
1996We explore the general properties of convection in a solar surface layer. Our three-dimensional simulations use a tabulated equation of state that includes excitation and ionization of hydrogen and other abundant atoms, and the formation of H2 molecules. The radiative energy exchange is determined by solving the radiative transfer equation.
Robert F. Stein +3 more
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ZAMM - Journal of Applied Mathematics and Mechanics / Zeitschrift für Angewandte Mathematik und Mechanik, 1973
AbstractThe paper is a study of motions for which the stretching tensor is convected without diffusion. It is shown that the diffusion of the stretching tensor vanishes if and only if the right Cauchy‐Green tensor is equal to its value for a rigid motion plus twice the product of the initial stretching with the elapsed time.
S. L. Passman, A. W. Marris
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AbstractThe paper is a study of motions for which the stretching tensor is convected without diffusion. It is shown that the diffusion of the stretching tensor vanishes if and only if the right Cauchy‐Green tensor is equal to its value for a rigid motion plus twice the product of the initial stretching with the elapsed time.
S. L. Passman, A. W. Marris
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Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences, 1987
Thermal convection in a fluid layer is an example of a dynamical system governed by partial differential equations. As the relevant control parameter (the Rayleigh number) is increased, successive bifurcations may lead to chaos and the nature of the transition depends on the spatial structure of the flow.
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Thermal convection in a fluid layer is an example of a dynamical system governed by partial differential equations. As the relevant control parameter (the Rayleigh number) is increased, successive bifurcations may lead to chaos and the nature of the transition depends on the spatial structure of the flow.
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