Units of sensible heat flux
[DOC File]Solutions to the Exercises
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This shows that while soil heat flux was a minor component of the daily energy balance, it played a crucial role in how energy was partitioned on a diurnal basis. Negative Hc values indicate that the sensible heat flux away from the canopy (Fig. 5 B) enhanced by cool arial and soil surface conditions.
[DOCX File]CZO Metadata Worksheet
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Table S1: Downward radiation of shortwave (SW), longwave (LW) at the surface, latent heat flux (LH), sensible heat flux (SH), and ground heat flux (G, positive downward into the ground) and outgoing longwave radiation at the top of the atmosphere (all in units of …
[DOC File]Moisture flux - Atmospheric Sciences
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COL9: label=Latent heat flux, Units=W/m2, TimeSupport=30 min, DataType=Average. COL10: label=CO2 concentration, Units=mg/m3, TimeSupport=30 min, DataType=Average. COL11: label=Water vapor concentration, Units=g/m3, TimeSupport=30 min, DataType=Average. Keywords. CO2 flux, sensible heat flux, latent heat flux, boundary layer meteorology. Methods
[DOCX File]American Meteorological Society
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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 was upward, and . (d) The ground was warming because , that is the heat flux into the ground was positive.
[DOC File]Eddy Correlation Flux Measurement System (ECOR) …
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Units that perform a heating function are also included. UNITARY HEAT PUMP. One or more factory-made assemblies that normally include an indoor conditioning coil, compressor(s), and an outdoor refrigerant-to-air coil or refrigerant-to-water heat exchanger. These units provide both heating and cooling functions. VARIABLE AIR VOLUME (VAV) SYSTEM.
[DOC File]Moisture flux
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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]DIURNAL ENERGY BALANCE IN WHEAT FIELD
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Primary Measurements: fc (CO2 flux), lv_e (latent heat flux), h (sensible heat flux), k (momentum flux), ustar (friction velocity); all of these are calculated quantities. The QC limits set in the ingest are appropriate for the measurements (primary and otherwise), although there are times when legitimate values fall outside the QC limits.
[DOC File]GEOS-4 File Specification - NASA
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units: kg m-3 J kg-1 K-1 m s-1 K = J m-2s-1. So . Surface Moisture flux and latent heat flux. Evaporation, E, can be treated similarly. Again we want to use a variable that is conserved unless there are sources or sinks. In the case of water vapor, suych a variable is the specific humidity, q. The eddy correlation method yields. The gradient ...
Heat flux - Wikipedia
Sensible heat flux. The density of sensible energy is (1) We have to be a bit careful in the vertical because of compressional effects that are not relevant to vertical energy exchange. Note that for adiabatic processes, q is conserved and no heat is exchanged.
[DOC File]SECTION 13-100
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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. ... %Convert data into appropriate units. % %Variables %input: ... % shf sensible heat flux % lhf latent heat flux % hf (total ...
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