4 edition of **Turbulence and diffusion in stable environments** found in the catalog.

- 292 Want to read
- 9 Currently reading

Published
**1985**
by Clarendon Press, Oxford University Press in Oxford [Oxfordshire], New York
.

Written in English

- Turbulence -- Congresses.,
- Diffusion -- Congresses.

**Edition Notes**

Includes bibliographies.

Statement | organized by the Institute of Mathematics and Its Applications and held in Cambridge, March 1983 ; edited by J.C.R. Hunt. |

Series | The Institute of Mathematics and Its Applications conference series ;, new ser., 4 |

Contributions | Hunt, Julian C. R., Institute of Mathematics and Its Applications. |

Classifications | |
---|---|

LC Classifications | QA913 .T865 1985 |

The Physical Object | |

Pagination | xv, 319 p. : |

Number of Pages | 319 |

ID Numbers | |

Open Library | OL2540242M |

ISBN 10 | 0198536046 |

LC Control Number | 85021494 |

Anomalous diffusion in rotating stratified turbulence. Pages Numerical studies of viscous effects for particle fluxes to perfectly absorbing spherical surfaces in turbulent environments: biological applications. Pages Particle-Laden Flow Book Subtitle From Geophysical to Kolmogorov Scales Editors. Bernard Geurts;. The same applies to strategy crafting. Constant planning, revisioning, and turbulence can lead to a lack of clarity and priorities for employees. We recommend that in your strategy crafting, you remain intentional over the long term by cycling through periods planning using turbulence and change through chaos and rest through renewal.

It is derived from the full consolidation (Gibson) equation and is implemented in a mixed Lagrangian-Eulerian bed model guaranteeing stable and non-negative solutions, while numeric diffusion remains small. The erosion and deposition of sand and mud is accounted for, whereas internal mixing (e.g., bioturbation) is modeled through diffusion. The only two stable nitrogen isotopes are N 7 14 and N 7 15, which have seven protons each and seven or eight neutrons in their nucleus, respectively. 15 N is the less frequent stable isotope, constituting of % of the global nitrogen pool. Consequently, it is more practical to measure the difference or ratio of two isotopes instead of the Cited by: 7.

Furthermore, the free surface treatment is combined with a Smagorinsky turbulence model and a technique for adaptive time steps to ensure stable simulations. The method is validated by comparing the position of the free surface with an uncoarsened simulation. where p and T are the air pressure and temperature, respectively, L υ and R υ are the latent heat and the gas constant for vapor, respectively, and e s is the saturation vapor pressure.. The turbulent exchange coefficient in radiation fog is small, with a typical range from 10 −2 m 2 s −1 in its early stage to 10 −1 –10 0 m 2 s −1 in its mature stage (Lala et al. ; Roach et al Cited by:

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Get this from a library. Turbulence and diffusion in stable environments: based on the proceedings of a conference on models of turbulence and diffusion in stably stratified regions of the natural environment.

[Julian C R Hunt; Institute of Mathematics and Its Applications.;]. Turbulence and diffusion in stable environments: Ed. Hunt Clarendon Press, Oxford,xv + pp., £ Article (PDF Available) in Applied Mathematical Modelling 10(6)– Nikolaos D.

Katopodes, in Free-Surface Flow, Dispersion. Even if turbulent diffusion were perfectly understood, it would not be sufficient for describing the transport of contaminants in the environment. There is an additional mechanism that affects the distribution of solute mass in space that is commonly identified as originates from the Greek διασπορά and.

Britter, RE () Diffusion and decay in stably-stratified turbulent flows. In: Turbulence and Diffusion in Stable Environments. Clarendon Press, Oxford, Great Britain. Full text not available from this repository. The turbulence in the very stable surface layer may be intermittent, sometimes related to downward bursts from turbulence generated aloft.

Clear air radiative flux divergence, transport by nonlinear gravity waves, drainage flows, and surface heterogeneity (see later) may invalidate assumptions required for Monin–Obukhov similarity theory. Turbulent Diffusion and Pollutant Transport in Shoreline Environments.

When the airplane travels from the stable marine atmosphere into the IBLt. BRITTER, R.E. Diffusion and decay in stably-stratified turbulent flows, in Turbulence and Diffusion in Stable Environments (ed J C R Hunt), 3–14, Clarendon Press, Oxford, UK.

Google Scholar BROW AND, F.K. and HOPFINGER, E.J. The inhibition of vertical turbulence scale by stable stratification, in Turbulence and Diffusion in Stable Cited by: 3. In Turbulence and Diffusion in Stable Environments, Clarendon Press, Oxford. Google Scholar Griffiths, R.

and Hopfinger, E.“The Structure of Mesoscale Turbulence and Horizontal Spreading at Ocean Fronts”, Deep-Sea Research, 31, –Cited by: 3. "Fully developed turbulence" is ubiquitous in both cosmic and natural environments, in engineering applications and in everyday life.

Elementary presentations of dynamical systems ideas, probabilistic methods (including the theory of large deviations) and fractal geometry make this a self-contained textbook. Statistics of Reconnection-driven Turbulence Grzegorz Kowal1,2, Diego A. Falceta-Gonçalves2, Alex Lazarian3, and Ethan T.

Vishniac4 1 Núcleo de Astrofísica Teórica, Universidade Cruzeiro do Sul, Rua Galvão Bueno, —Liberdade CEP:São Paulo, SP, Brazil; @d by: Under the premise of stable atmospheric stratification, the Ozmidov scale L O [20,21] can be used as the maximum value of the turbulence scale, and the turbulence kinetic energy dissipation rate and turbulence diffusion coefficient can be correlated: ε = L O 2 N s 3, K = β L O 2 N s, where β is a constant, and N s is the positive buoyancy Author: Yang He, Zheng Sheng, Mingyuan He.

(5) Generally, when the flow is parallel to the x-axis, the diffusion term K x (∂ 2 χ ̅ /∂x 2) is small compared to the transport term u ̅ (∂ χ ̅ /∂x) and is ignored. Likewise, for a continuous infinite line source (for example, a long, straight section of highway) oriented along the y-axis, both the K x and K y terms are usually ignored.

Although values of K z have been Cited by: 8. turbulence on domestic and international environments. Attention is focused on two distinctive sources of turbulence.

The first, external-led turbulence, is generated by globalization dynamics and is mainly played out by transnational actors who are particularly visible in monetary issues and financial volatility. Hunt, Julian C. R [ Book, Government publication: ] At Nat Met Library Turbulence and diffusion in stable environments: based on the proceedings of a conference on models of turbulence and diffusion in stably stratified regions of the natural environment / organized by the Institute of Mathematics and Its Applications.

Numerous previous works have shown that vertical shear in wind speed and wind direction exist in the atmospheric boundary layer. In this work, meteorological forcing mechanisms, such as the Ekman spiral, thermal wind, and inertial oscillation, are discussed as likely drivers of such shears in the statically stable by: B.

Galperin. A laboratory study of anisotropic turbulence and Lagrangian diffusion on a westward jet - and a novel method of analyzing macroturbulence. Naval Research Laboratory, Stennis Space Center, MS, 5 March Galperin, B. An experimental study of anisotropic turbulence and Lagrangian diffusion in an.

In this report, we present several results in the theory of α-models of turbulence with improved accuracy that have been developed in recent α-models considered herein are the Leray-α model, the zeroth Approximate Deconvolution Model (ADM) turbulence model, the modified Leray-α and the Navier–Stokes-α model.

For all of the models from above, the. @article{osti_, title = {HORIZONTAL DIFFUSION FROM AN INSTANTANEOUS POINT-SOURCE DUE TO OCEANIC TURBULENCE.

Technical Report No. 32}, author = {Okubo, A.}, abstractNote = {A discussion is presented of horizontal turbulent diffusion of a patch of a diffusive substance released from an instantaneous point-source in the sea a situation to which a. Representations of the atmospheric boundary layer in global climate models play a role in simulations of past, local closure likens turbulent transport to molecular diffusion, and is usually first or second order.

though it has been applied to statically stable environments. The drift velocities, mobilities, and longitudinal diffusion coefficients of the ion-gas combinations Tl/sup +/ in He, Ne, Ar, and O/sub 2/, Cl/sup -/ in N/sub 2/ and NO/sup +/ in N/sub 2/ were measured at constant room temperature as a function of E/N, where E is the electric field strength and N is the number density of the neutral gas.

The flow in the test section is stable (1σ airspeed = m s −1 at the mid-range speed, 25 m s −1), uniform (1σ airspeed = m s −1 at 25 m s −1), straight (1σ deviation angle = ° at 25 m s −1), low turbulence (axial turbulence intensity = % at 25 m s −1) and quiet ( dB at 25 m s −1).

The datasets resulting Cited by: 5.The purpose of the present chapter is once again to show on concrete new examples that chaos in one-dimensional unimodal mappings, dynamical chaos in systems of ordinary differential equations, diffusion chaos in systems of the equations with partial derivatives and chaos in Hamiltonian and conservative systems are generated by cascades of bifurcations under Cited by: 1.

The nanoparticles produced by iFNP have a hydrophilic core and hydrophobic corona, and are dispersed in organic solvents. However, most nanoparticle applications, particularly biomedical applications, require that the particle be stable in aqueous environments.