Sensible heat flux calculation
[DOC File]GEOS-4 File Specification - NASA
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Latent heat flux at surface W m-2 HFLUX. Sensible heat flux at surface W m-2 LWI. Surface types 0=water, 1=land, 2=ice QV10M. Specific humidity at 10 m above displacement height kg kg-1 QV2M. Specific humidity at 2 m above displacement height kg kg-1 SLP. Sea level pressure Pa T10M. Temperature at 10 m above displacement height K T2M
[DOCX File]User’s Guide
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is available energy partitioned between sensible heat and latent heat fluxes on land surface. VPD = e. sat – e . is the air vapor pressure deficit. All inputs have been previously defined except for surface resistance . r. s, which is an effective resistance accounting for evaporation from the soil surface and transpiration from the plant canopy.
[DOC File]3
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In the calculation of surface heat flux combined with LES, FDS uses ad-hoc correlations of both natural and forced convection. This approximation will have a major effect on the prediction of heat flux to the walls and targets which are important parameters to the fire analysis. For more information on this model, visit www.nist.gov.
[DOC File]THE NCEP LAND-SURFACE MODEL (LSM)
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H sensible heat flux (W/m2) LE latent energy flux (W/m2) CO2 CO2 flux (mg CO2/m2/s) ** LW_in downwelling longwave from sky (W/m2) sm_5 soil volumetric water content at 5 cm zone (after November 19 1997) sm_20 soil volumetric water content at 20 cm zone (after November 19 1997)
[DOC File]Improving spatial resolution of integrated ET seasonal for ...
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The Sensible Heat flux (H) is a convection flux through the atmosphere layers, coming from the surface skin boundary layer with the topmost soil/vegetation layer. (W/m2) Equation 4 The energy necessary to vaporize water under given atmospheric conditions is especially ruled by …
[DOC File]Practical 4: Measuring the wind profile in the surface layer
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, from which surface sensible heat flux H may be estimated. Software: Excel together with (1) the logpro.xls spreadsheet for reading the anemometer data and (2) the met-mast.xls spreadsheet for reading the data from the Penman mast and applying the Penman-Monteith equation to estimate the variables in the surface energy balance (see Atmospheric ...
[DOC File]Remote Sensing of the Oceans - Stanford University
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2) The equation for sensible heat flux between the ocean and atmosphere is: Sensible heat flux = rho*Cp*Cs*U10(Ts-Ta) Where. rho. is the air density (1.5 kg m-3) Cp. is the specific heat capacity of air (1030 J kg-1 K-1) Cs. is the sensible heat transfer coefficient (1e-3) U10. is the wind speed at 10 above sea level (10 m s-1)
[DOC File]GEOS-4 File Specification
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Latent heat flux at surface W m-2 HFLUX. Sensible heat flux at surface W m-2 LWI. Surface types 0=water, 1=land, 2=ice QV10M. Specific humidity at 10 m above displacement height kg kg-1 QV2M. Specific humidity at 2 m above displacement height kg kg-1 SLP. Sea level pressure Pa T10M. Temperature at 10 m above displacement height K T2M
[DOC File]Iowa State University
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2D forecast fields include:Ground temperature (K)PBL height (m)Surface sensible heat flux (W/m2)Surface latent heat flux (W/m2)Frictional velocity (m/s)2 m temperature (K)10 m u component of wind (m/sec)10 m v component of wind (m/sec)Monin-Obukov length (m) Figure 4 [5] provides a visual indication of what physical weather models provide. Fig ...
[DOC File]Solutions to the Exercises
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When the flux is only 0.4 m y-1, the residence time is 46 days. 1.2 An energy flux in equivalent mm y-1 of evaporation is (3600*24*365*10-6/2.5) = 12.6 times that flux expressed in W m-2. Hence for net radiation this is 1,312 mm/y, for evaporation 1,009 mm/y, and for sensible (turbulent) heat flux 240 mm/y. Chapter 2
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