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4 edition of Determination of vertical turbulent diffusivities of heat in a North Florida lake found in the catalog.

Determination of vertical turbulent diffusivities of heat in a North Florida lake

by Jerry Allen Steinberg

  • 153 Want to read
  • 31 Currently reading

Published .
Written in English

    Subjects:
  • Water temperature.,
  • Turbulence.,
  • Diffusion.,
  • Mize, Lake.

  • Edition Notes

    Statementby Jerry A. Steinberg
    The Physical Object
    Paginationix, 206 leaves :
    Number of Pages206
    ID Numbers
    Open LibraryOL24131005M
    OCLC/WorldCa2352398

    J. Lee, J.F. MacArt, M.E. Mueller, Heat release effects on the Reynolds stress budgets in turbulent premixed jet flames at low and high Karlovitz numbers, Combustion and Flame () M.E. Mueller, Physically-derived reduced-order manifold-based modeling for multi-modal turbulent combustion, Combustion and Flame ()   Abstract: Direct numerical simulation of a turbulent channel flow with heat transfer was performed at very low Reynolds numbers. Two different thermal boundary conditions were studied, and temperature was considered as a passive scalar. The computations were carried out with huge computational boxes (up to x 2 x in the streamwise, wall-normal, and spanwise directions, Cited by: 7.

    Artificially initiated turbulent spots in a Blasius boundary layer were investi- gated experimentally using hot-wire anemometers. Electrical discharges generated the spots, which grew in all directions rn they were swept downstream by the mean by: An experimental investigation of pressure drop and heat transfer for water boiling in a vertical-upflow single-tube heat exchanger / (Washington, D.C.: National Aeronautics and Space Administration ; Springfield, VA: For sale by the Clearinghouse for Federal Scientific and Technical Information, ), by James R. Stone, Thomas M. Damman.

    In February , we observed the response of the 40 to 50 m deep northern Adriatic Sea to strong surface forcing by 20 m s−1 winds and W m−2 net upward heat flux resulting from cold bora winds b Cited by: Duplicate Title to Geographic and temporal variations in turbulent heat loss from lakes: A global analysis across 45 lakes User Workarea, Unnamed user with username JiscRouter - [ Manage ] [ Compare & Merge ] [ Acknowledge ]Cited by:


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Determination of vertical turbulent diffusivities of heat in a North Florida lake by Jerry Allen Steinberg Download PDF EPUB FB2

Determination of vertical turbulent diffusivities of heat in a North Florida lake / By. Steinberg, Jerry Allen, Type. Book Material. Published material. Publication info. Notes: Typescript. Vita. Thesis--University of Florida.

Subjects. Full text of "Determination of vertical turbulent diffusivities of heat in a North Florida lake." See other formats. Determination of vertical turbulent diffusivities of heat in a North Florida lake / View Metadata.

By: Steinberg, Jerry Allen, Publication info: Holding Institution: University of Florida, George A. Smathers Libraries. Books by genre: Nonfiction. Nonfiction is a genre which is entirely based on real facts.

It can be full, complete story or just some notes of eyewitness about a concrete action. Determination of Vertical Turbulent Diffusivities of Heat in a North Florida Lake.

Steinberg, Jerry Allen, transition and must be reflected in those heat transfer correlations. Thus, analysing turbulent heat transfers mi-croscales in vertical natural convection boundary layers, we consider in the present report that the local Grashof number must be replaced by the non-dimensional group RaxPrx/(1+Prx) based on the real thermophysical prop-Cited by: 2.

Investigation of turbulent mixing in shallow lakes using temperature microstructure measurements Andreas Lorke Institute of Freshwater Ecology and Inland Fisheries, MueggelseedammD.

Direct determination of the irreversible turbulent flux of salinity in the ocean has not been possible because of the complexity of measuring salinity on the smallest scales over which it mixes.

A microstructure profiler was designed especially for the investigation of the diurnal dynamics of turbulent mixing in shallow lakes. 7 hours observation of these dynamics in a shallow, polymictic lake shows a multitude of different mixing processes acting together on very short time-scales.

Estimated turbulent diffusivities for the surface mixed layer, using the Cox number method, are Cited by: 9. It was found that (1) ∼% of the vertical wind energy flux P 10 (∼39 mW m −2), estimated 10 m above the lake surface, was available for turbulent mixing in the entire lake water body; (2) ∼% of P 10 was dissipated by turbulence in the weakly stratified surface layer (epilimnion ;6 m deep), and ∼% of P 10 reached the Cited by: Determination of vertical turbulent diffusivities of heat in a North Florida lake.

Water temperature; Turbulence; Diffusion. o c o I- 3 a. 1 1 ^ o a b â o g O o HI a fJ 11 o u t-1 ^55 I 9 w O CO (Jj -J Q Z ' z 2 < t CO o o < o o < f- <. Determination of vertical turbulent diffusivities of heat in a North Florida lake.

Water temperature; Turbulence; Diffusion. FIGURE PHOTOGRAPH OF SYSTEM CIRCUIT CABINET. FIGURE PHOTOGRAPH OF RECORDER CABINET. We report on our direct numerical simulation of an incompressible, nominally zero-pressure-gradient flat-plate boundary layer from momentum thickness Reynolds number 80– Heat transfer between the constant-temperature solid surface and the free-stream is also simulated with molecular Prandtl number Pr=1.

Skin-friction coefficient and other boundary layer parameters follow Cited by: The governing differential equations for turbulent kinetic energy k and its dissipation rate e are: Turbulent flow and heat transfer in pipes Kinetic energy of turbulence, Dissipation rate, 13 1,) + / + r^ where r ^ Fz^M ^M 'm rT r 2/ 1,i 1 6 1 +0 06 ^ * 6 /»«(2 7) -° The expression for /¿ e f f is + CMpk / by: The fluid flow and heat transfer characteristics in the turbulent combined-convection boundary layer in air along a vertical heated plate were experimentally investigated with normal hot and cold wires, paying close attention to freestream conditions.

The results of the Cited by:   Turbulent fluxes of sensible and latent heat were measured with the helicopter-borne turbulence probe Helipod over a heterogeneous landscape around the Meteorological Observatory Lindenberg during the STINHO-2 and LITFASS field experiments. Besides the determination of area-averaged heat fluxes, the analysis focused on different aspects of the response of the turbulent Cited by: AN EXPERIMENTAL INVESTIGATION OF TURBULENT NATURAL CONVECTION IN AIR AT LOW PRESSURE ALONG A VERTICAL HEATED FLAT PLATE CHARLES Y.

WARNER* and VRDAT S. ARPACIt (Received 19 April and in revised form 7 August ) Abstract-An experimental investigation of turbulent natural convection in air is described. For example, at low values of ε/νN 2, where ε is the dissipation of turbulent kinetic energy and ν is the kinematic viscosity, eddy diffusivities depend on the Schmidt number Sc = ν/D Φ (Barry et al.

), where D Φ is the molecular diffusivity of the scalar Φ, and at high values of ε/νN 2, effects of molecular diffusivity disappear Cited by: T1 - Temperature stratification and mixing dynamics in a shallow lake with submersed macrophytes.

AU - Herb, William R. AU - Stefan, Heinz G. PY - /1/1. Y1 - /1/1. N2 - This paper describes an investigation of temperature stratification and vertical mixing in lacustrine macrophyte by: produce peak heat fluxes that are comparable in magni-tudetothoseofwildfires,butthesmallerscaleofthefires and the shorter duration of heating generally limit the overall quantity of heat output (Heilman et al.

In this study, we examine whether the sensitivity of mean and turbulent flow in the PBL and roughnessCited by: 4. model of turbulent dissolution of a vertical wall. The model is based on the empirical observation that turbulent heat transfer on a vertical wall is independent of height at very high Rayleigh numbers.

Our model predicts the dissolving velocity, V, given by V =g g(rf ri)D2 µ 1=3 C f Ci Cf Cs =gV (1) and the interface temperature and.

THE TURBULENT. BOUNDARY LAYER: EXPERIMENTAL HEAT TRANSFER WITH STRONG FAVORABLE PRESSURE GRADIENTS AND BLOWING. By. D. W. Kearney, R.

J. Moffat and W. M. Kays. Report No. HTMT Prepared Under Grant NASA JGi" for The National Aeronautics and Space Administration (ACCESSION NUMBER) T RU) DE) V 0 ' (NASA c1OR TMX .Uniform Heat Flux: When a flat plate is subjected to uniform heat flux instead of uniform temperature, the local Nusselt number is given by These relations give values that are 36 percent higher for laminar flow and 4 percent higher for turbulent flow relative to the isothermal plate Size: KB.This book grew out of the need for a comprehensive treatment of the diverse elements of geophysical fluid flow at the microscale.

Kantha and Clayson have arranged a logial exposition of the various mixing processes operating within and between the oceans and its .