dew.point.solver

Solver function used in dew.point()

internal

Calculation of physical (e.g. aerodynamic conductance, surface temperature),
and physiological (e.g. canopy conductance, water-use efficiency) ecosystem properties
from eddy covariance data and accompanying meteorological measurements. Calculations
assume the land surface to behave like a 'big-leaf' and return bulk ecosystem/canopy variables.

Juergen Knauer

bigleaf

Physical and Physiological Ecosystem Properties from Eddy
Covariance Data

Thomas Wutzler

Alison Bennett

Soenke Zaehle

Tarek El-Madany

Mirco Migliavacca

dew.point.solver function

<dl><dt>ea</dt>
<dd>Air vapor pressure (kPa)</dd>
<dt>accuracy</dt>
<dd>Accuracy of the result (degC)</dd>
<dt>Esat.formula</dt>
<dd>Optional: formula to be used for the calculation of esat and the slope of esat.
One of <code>"Sonntag_1990"</code> (Default), <code>"Alduchov_1996"</code>, or <code>"Allen_1998"</code>.
See <code>Esat.slope</code>.</dd>
<dt>constants</dt>
<dd>Pa2kPa - conversion pascal (Pa) to kilopascal (kPa)</dd></dl>

Arguments

Solver function for dew point temperature — dew.point.solver

<dl>

<dt>ea</dt>
<dd>Air vapor pressure (kPa)</dd>


<dt>accuracy</dt>
<dd>Accuracy of the result (degC)</dd>


<dt>Esat.formula</dt>
<dd>Optional: formula to be used for the calculation of esat and the slope of esat.
One of <code>"Sonntag_1990"</code> (Default), <code>"Alduchov_1996"</code>, or <code>"Allen_1998"</code>.
See <code>Esat.slope</code>.</dd>


<dt>constants</dt>
<dd>Pa2kPa - conversion pascal (Pa) to kilopascal (kPa)</dd>

</dl>

dew.point.solver: Solver function for dew point temperature

Description

Usage

Arguments