Description Usage Arguments Value References
View source: R/wind_functions.R
Calculates the aerodynamic resistance (s/m) over a lake as defined by Calder and Neal (1984, pg. 93) and McJannet et al. (2008, Appendix B, Equation 10), and as presented in McMahon et al. (2013) Equation S11.23.
1 | aero_resist(uz, wind_z, z0, A, lake_z, rho_a = 1.2, ca = 0.001013)
|
uz |
wind speed at wind_z height (m/s) |
wind_z |
height at which |
z0 |
aerodynamic roughness of land cover at measurement site (m) |
A |
surface area of the lake (km^2) |
lake_z |
elevation of lake above mean sea level (m) |
rho_a |
density of the air (kg/m^3), defaults to 1.20 kg/m^3 at 20 deg C |
ca |
specific heat of the air (MJ/kg/K), defaults to 0.001013 MJ/kg/K |
ra |
aerodynamic resistance (s/m) |
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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