hydrology_snowMelt | R Documentation |
High-level functions to define water inputs into the soil of a stand:
Function hydrology_waterInputs
performs canopy water interception and snow accumulation/melt.
Function hydrology_snowMelt
estimates snow melt using a simple energy balance, according to Kergoat (1998).
hydrology_snowMelt(tday, rad, LgroundSWR, elevation)
hydrology_waterInputs(
x,
prec,
rainfallIntensity,
pet,
tday,
rad,
elevation,
Cm,
LgroundPAR,
LgroundSWR,
modifyInput = TRUE
)
tday |
Average day temperature (ºC). |
rad |
Solar radiation (in MJ/m2/day). |
LgroundSWR |
Percentage of short-wave radiation (SWR) reaching the ground. |
elevation |
Altitude above sea level (m). |
x |
An object of class |
prec |
Precipitation for the given day (mm) |
rainfallIntensity |
Rainfall intensity rate (mm/h). |
pet |
Potential evapotranspiration for the given day (mm) |
Cm |
Canopy water storage capacity. |
LgroundPAR |
Percentage of photosynthetically-active radiation (PAR) reaching the ground. |
modifyInput |
Boolean flag to indicate that the input |
The function simulates different vertical hydrological processes, which are described separately in other functions.
If modifyInput = TRUE
the function will modify the x
object (including both soil moisture and
the snowpack on its surface) as a result of simulating hydrological processes.
Function hydrology_waterInputs
returns a named vector with the following elements, all in mm:
Rain |
Precipitation as rainfall. |
Snow |
Precipitation as snow. |
Interception |
Rainfall water intercepted by the canopy and evaporated. |
Snowmelt |
Snow melted during the day, and added to the water infiltrated. |
NetRain |
Rainfall reaching the ground. |
Miquel De Cáceres Ainsa, CREAF
Kergoat L. (1998). A model for hydrological equilibrium of leaf area index on a global scale. Journal of Hydrology 212–213: 268–286.
spwb_day
, hydrology_rainInterception
, hydrology_soilEvaporation
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