Results 211 to 220 of about 64,779 (261)
A novel approach to micro-fabricated thermoelectric generators with SrTiO<sub>3</sub>. [PDF]
Santander J +11 more
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Uremic Toxins and Hemodiafiltration: From Molecular Mechanisms to Clinical Outcomes. [PDF]
Stuard S +5 more
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Natural convection heat transfer performance of finned heat sinks with different fin materials and geometries. [PDF]
Wani S +4 more
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Identifying key convection-sensitive oceanic regions to weaken the ENSO spring predictability barrier. [PDF]
Mei Z +12 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.
Passman, S. L., Marris, A. W.
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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.
Passman, S. L., Marris, A. W.
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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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Convective Plumes in a Convective Field
Journal of the Atmospheric Sciences, 1970Abstract The theory of isolated turbulent plumes given earlier is used to study a field of plumes. Each plume is immersed in the turbulent downdraft which comprises the return flow. The field of flow is specified by three parameters: the heat flux into the atmosphere at the surface, the depth of the convecting layer, and the intensity of turbulence at ...
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Astrophysics and Space Science, 2003
zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Demarque, Pierre, Robinson, Francis J.
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zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Demarque, Pierre, Robinson, Francis J.
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