How to calculate latent heat flux

    • [DOC File]Wind Stress and Ekman Mass Tranport

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      The raw SAIL data was divided into hourly segments. The bulk formulas from Smith’s (1988) paper “Coefficients of sea surface wind stress, heat flux, and wind profiles as a function of wind speed and temperature” were used to calculate the momentum and heat fluxes. A program written by Guest (1997) carried out these surface flux calculations.

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    • [DOC File]Problem set #1

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      Heat pump cost = (2498 kWh)($0.08/kWh) = $200. Operating costs are lower for a heat pump, capital costs are higher. 2. (1.491) Liquid oxygen, which has a boiling point of 90oK and a latent heat of vaporization of 214 kJ/kg, is stored in a spherical container whose outer surface is of 500-mm diameter and at a temperature of (10oC.

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    • Simple Correlation Equations of Heat Transfer Coefficient ...

      The formulae obtained can be used to calculate the mean heat transfer coefficients, (h-corr) and heat flux. ... eff Effective latent heat of vaporization (kJ/kg) ... Heat flux in both the sub ...

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    • [DOC File]Atmospheric Sciences

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      Sensible heat flux. Follow the steps below to determine the surface sensible heat flux by calculating the daytime heating of the planetary boundary layer (PBL) Below are three figures. The first two show recent radiosonde profiles at 5 am and 5 pm in Tucson. The third figure shows the two figures superimposed on top of one another to show the ...

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    • [DOC File]ASEN/ATOC 5225 Thermodynamics of Atmospheres and Oceans

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      5. The surface latent heat flux will (increase, decrease, remain the same) if the ocean salinity increases. decrease. 6. The surface latent heat flux will (increase, decrease, remain the same) if the sea surface temperature increases. increase. 7. A crude estimate of the surface moisture flux, Ė, over a large homogeneous body of water is given by,

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    • [DOCX File]Prospectus Outline - Florida State University

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      The main driver of TC genesis and intensity change is the release of latent heat in clouds where the source of moist entropy flux comes from the thermodynamic disequilibrium at the ocean-atmosphere interface (Charney and Eliassen 1964; Kuo 1965; Emanuel 1986).

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    • [DOC File]Iowa Environmental Mesonet

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      This likely resulted in the excessively large latent heat flux values that the NARR model produced. Figure N: 18 UTC average latent heat flux comparison between nstl11, (over a corn field) nstl10 (over a soy bean field), and the NARR model for the months of May through December, 2006. D. …

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    • [DOC File]DIURNAL ENERGY BALANCE IN WHEAT FIELD

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      The latent heat flux was then calculated as LE = (Rn - G) /(1 + () (3) This equation has been used over different kinds of plants where extremely dry conditions are not used.

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    • [DOC File]CHE 303 (Winter 2000)

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      4) Calculate the heat transfer rate per unit thickness normal to the page from the bottom half of the right surface to the fluid. _____ III. The outer surface of a hollow sphere of radius r2 is subjected to a uniform heat flux . The inner surface at r1 is held at a constant temperature Ts,1.

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