Converts latent heat flux (W/m²) to an evaporation rate in metres per day,
suitable for lake water balance calculations.
Usage
flux_to_evap(Qlh, Lv = 2453000, rho_water = 1000)
Arguments
- Qlh
Numeric. Latent heat flux (W/m²), should be \(\leq 0\).
- Lv
Numeric. Latent heat of vaporisation (J/kg). Default 2453000.
- rho_water
Numeric. Water density (kg/m³). Default 1000.
Value
Numeric. Evaporation rate (m/day), \(\leq 0\).
Details
The conversion is:
$$E = \frac{Q_{lh}}{L_v\,\rho_w} \times 86400$$
Examples
flux_to_evap(-50)
#> [1] -0.001761109