hurs2huss | R Documentation |
Relative humidity to specific humidity conversion using surface pressure and temperature
hurs2huss(hurs, ps, tas)
hurs |
Relative humidity grid |
ps |
Surface pressure |
tas |
Near-surface air temperature |
A climate4R CDM grid of specific humidity (in kg/kg)
In principle, the derivation functions will work regardless of the input units, as all units are internally
converted as necessary according to the specific formulae definitions.
However, the units string (see getGridUnits
) must be parseable. In the same vein,
the input units need to be convertible to the required ones. Unit consistency is internally achieved
by the function udConvertGrid
.
J. Bedia, S. Herrera
Gregory, D. (2000), Atmospheric thermodynamics. By Craig F. Bohren and Bruce A. Albrecht. Oxford University Press. xiv + 402 pp. Price £49.50 (hardback). ISBN 019 5099044. Q.J.R. Meteorol. Soc., 126: 2631-2632. doi:10.1002/qj.49712656815
Other derivation:
hurs2tdps()
,
hurs2w()
,
huss2hurs()
,
huss2pvp()
,
ps2psl()
,
psl2ps()
,
rad2cc()
,
tas2ws()
,
tdps2hurs()
Other humidity:
hurs2tdps()
,
hurs2w()
,
huss2hurs()
,
huss2pvp()
,
tas2ws()
,
tdps2hurs()
data("ps.iberia")
data("tas.iberia")
data("huss.iberia")
hurs <- huss2hurs(huss = huss.iberia, ps = ps.iberia, tas = tas.iberia)
huss <- hurs2huss(hurs = hurs, ps = ps.iberia, tas = tas.iberia)
identical(huss$Data, huss.iberia$Data)
# Not identical due to rounding errors:
range(huss$Data - huss.iberia$Data)
## Not run:
require(visualizeR)
spatialPlot(climatology(hurs), rev.colors = TRUE, backdrop.theme = "coastline")
## End(Not run)
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