Results 321 to 330 of about 570,217 (365)

Dimensionless Parameters Define Criteria for Optimal Flow Velocity in Enhancing Chemotactic Response toward Residual Contaminants in Porous Media. [PDF]

Environ Sci Technol
Gao B, Ford RM.
europepmc   +1 more source

The liquid-vapor water generation characteristics of thermo-responsive polymer based on the multi-scale method. [PDF]

iScience
Tian S, Chen C, Huang L, Yao X, She A, Su X.   +5 more
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Exploring the thermal-induced optical nonlinearity of crude oil via spatial self-phase modulation technique. [PDF]

Sci Rep
Golestanifar M, Haddad MA, Hassan AN, Pakravan K.   +3 more
europepmc   +1 more source

Overshooting convection drives winter mixed layer under Antarctic sea ice

Gayen B, Bhadouriya A, Garabato AN, Silvano A.   +3 more
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CONVECTION | Convection in the Ocean

2003
This 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.
openaire   +2 more sources

Solar Convection and Magneto-Convection

1996
We 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, D. J. Bercik, Shantanu Basu, Åke Nordlund   +3 more
openaire   +2 more sources

Convective Plumes in a Convective Field

Journal of the Atmospheric Sciences, 1970
Abstract 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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Convective instability of a free-convection vortex

Journal of Engineering Physics, 1990
The stability of free-convection vortex formations obtained in the laboratory is compared with natural tropical cyclones.
A. A. Solov'ev, A. D. Solodukhin, Oleg G. Martynenko   +2 more
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Conduction and Convection [PDF]

, 1991
As we discussed in Chapter 8, our knowledge of the pore-level fluid mechanics in two-phase flow through porous media is rather incomplete. In this chapter, we discuss thermal dispersion, i.e., convective heat transfer at the pore level, using the available knowledge about the subject. This knowledge is even more inconclusive.
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