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[DOC File]ASEN/ATOC 5225 Thermodynamics of Atmospheres and Oceans
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19. Units for heat flux FB0 are __kg/ms3_____ 20. The equation for ocean surface buoyancy flux (no runoff or sea ice) can be written as. Evaporation modifies buoyancy in two ways, via the latent heat flux and also via the salinity. Compare the thermal vs salinity effects of evaporation on the ocean surface buoyancy flux (e.g. determine their ...
units of sensible heat flux

[DOC File]CHAPTER 3
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When the energy equation (2.3) is not solved, the evaporation outflow rate in Equation (2.2) is computed with the Penman equation which is based on the following simplified energy balance on the water surface: (2.9) where, , and are the net radiation flux, latent heat flux, and sensible heat flux…
latent heat of vaporization calculation

[DOC File]Solutions to the Exercises
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Assume that on average the latent heat of evaporation is . This gives a latent heat flux . Thus according to (4.13) with the assumption that , one can write H = 200-40-122.5 = 37.7 W/m2. (b) The Bowen ratio was (c) The atmosphere was unstable because , which means that the sensible heat flux …
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[DOC File]Atmospheric Sciences
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1. 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.
latent heat formula

[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).
specific latent heat formula

[DOCX File]Yale University
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(1), and distributed the imbalance term to the sensible and latent heat fluxes in proportion to the measured Bowen ratio [Twine et al., 2000]. The sensible and latent heat flux after this adjustment are denoted as . H ' and LE ' . This adjustment was done at half-hourly intervals. In this analysis, we have ignored the canopy heat storage.
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[DOC File]Paper No: 200000
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Equation 10 is essentially identical to the latent heat flux equation presented by Monteith and Unsworth (1990, equation 15.9) except that their formulation was based on the vapor pressure deficit (VPD). The VPD is the saturated air vapor pressure minus the actual vapor pressure. In our formulation we rely only on actual vapor pressures.
latent heat of vaporization formula

[DOC File]CHAPTER 5 ENERGY, MATTER, AND MOMENTUM …
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turbulent flux of sensible heat (also known as the . sensible heat flux (QH)) and the . turbulent flux of latent heat, or . latent heat flux (QE), and is used to drive atmospheric processes between the surface and the atmosphere above this layer. Unlike energy and moisture, the . vertical flux of horizontal momentum. or . shearing stress (τ
how to calculate latent heat

Latent heat flux equation