Description Usage Arguments Value References
View source: R/heat_functions.R
Calculates the heat flux for the land surface in question. When using the "FAO" evaporation method, calculates the soil heat flux beneath a dense cover of grass based on Equations 42-46 in Allen et al. (1998). When using the "McJannet" lake evaporation method, calculates the change in heat storage based on water temperature following McJannet et al. (2008) Equation 31 as presented in McMahon et al. S11.33 (2013).
1 2 3 4 5 6 7 8 9 10 |
method |
denotes which evaporation method to use ("FAO", "McJannet", or "Hamon"). |
loc |
a list with location information that includes:
|
lake |
A list with lake data. Defaults to NULL, but for McJannet lake evaporation calculations, should include:
|
weather |
a list with weather data that includes:
|
albedo |
a list with albedos for different surfaces, defaults to:
|
Rn |
Net solar or shortwave radiation (MJ/m^2/timestep) |
rho_w |
density of water (kg/m^3), defaults to 997.9 kg/m^3 at 20 deg C |
cw |
specific heat of water (MJ/kg/K), defaults to 0.00419 |
G |
heat flux (MJ/m^2/hr) |
Allen, R. G., Pereira, L. S., Raes, D., & Smith, M. (1998). Crop evapotranspiration: Guidelines for computing crop water requirements. Rome: FAO. Retrieved from http://www.fao.org/docrep/X0490E/x0490e00.htm.
McMahon, T. A., Peel, M. C., Lowe, L., Srikanthan, R., and McVicar, T. R. (2013). Estimating actual, potential, reference crop and pan evaporation using standard meteorological data: a pragmatic synthesis, Hydrol. Earth Syst. Sci., 17, 1331–1363. https://doi.org/10.5194/hess-17-1331-2013.
McJannet, D. L., Webster, I. T., Stenson, M. P., and Sherman, B.S. (2008). Estimating open water evaporation for the Murray-Darling Basin. A report to the Australian Government from the CSIRO Murray-Darling Basin Sustainable Yields Project, CSIRO, Australia, 50 pp. Retrieved from http://www.clw.csiro.au/publications/waterforahealthycountry/mdbsy/technical/U-OpenWaterEvaporation.pdf.
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