calc_soilmstress | R Documentation |
Calculates an empirical soil moisture stress factor as a function of relative soil moisture (fraction of field capacity).
calc_soilmstress(soilm, meanalpha = 1, apar_soilm = 0, bpar_soilm = 0.685)
soilm |
Relative soil moisture as a fraction of field capacity (unitless). Defaults to 1.0 (no soil moisture stress). |
meanalpha |
Local annual mean ratio of actual over potential evapotranspiration, measure for average aridity. Defaults to 1.0. |
apar_soilm |
(Optional, used only if |
bpar_soilm |
(Optional, used only if |
The soil moisture stress factor is calculated using a quadratic function that
is 1 above soilm
= 0.6 and has a sensitivity, given by the y-axis cutoff,
(zero soil moisture), determined by average aridity (argument meanalpha
) as:
\beta = q(\theta - \theta*)^2 + 1
for \theta < \theta*
and \beta = 1.0
otherwise. \theta*
is fixed at 0.6.
q
is the sensitivity parameter and is calculated as a linear function of average aridity,
quantified by the local annual mean ratio of actual over potential evapotranspiration, termed
\alpha
:
q=(\beta0-1)/(\theta*-\theta0)^2
\theta0
is 0.0, and
\beta0 = a + b \alpha
a
is given by argument apar
, b
is given by argument bpar
.
A numeric value for \beta
Stocker, B. et al. Geoscientific Model Development Discussions (in prep.)
## Relative reduction (%) in GPP due to soil moisture stress at
## relative soil water content ('soilm') of 0.2:
print((calc_soilmstress(0.2)-1)*100 )
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