cal_ActualVapourPressure_from_dewPoint

As the dewpint temperature is the temperature to which the air
 needs to be cooled to make the air saturated, the actual vapour pressure
 is the saturation vapour pressure at the dewpoint temperature.

Supports the calculation of meteorological characteristics in
evapotranspiration research and reference crop evapotranspiration, and offers
three models to simulate crop evapotranspiration and soil water balance in
the field, including single crop coefficient and dual crop coefficient,
as well as the Shuttleworth-Wallace model. These calculations main refer to
Allen et al.(1998, ISBN:92-5-104219-5), Teh (2006, ISBN:1-58-112-998-X), and
Liu et al.(2006) <doi:10.1016/j.agwat.2006.01.018>.

Minguo Liu

simET

Tools for Simulation of Evapotranspiration of Field Crops and
Soil Water Balance

Huimin Yang

cal_ActualVapourPressure_from_dewPoint function

<dl><dt>Tdew</dt>
<dd>dew point temperature(degrees Celsius).</dd></dl>

Arguments

Actual vapour pressure derived from dewpoint temperature — cal_ActualVapourPressure_from_dewPoint

<dl>

<dt>Tdew</dt>
<dd>dew point temperature(degrees Celsius).</dd>

</dl>

cal_ActualVapourPressure_from_dewPoint: Actual vapour pressure derived from dewpoint temperature

Description

Usage

Value

Arguments

References