swAlphaOverBeta: Ratio of seawater thermal expansion coefficient to haline...

In oce: Analysis of Oceanographic Data

Ratio of seawater thermal expansion coefficient to haline contraction coefficient

Description

Compute \alpha/\beta using McDougall's (1987) algorithm.

Usage

swAlphaOverBeta(
  salinity,
  temperature = NULL,
  pressure = NULL,
  longitude = NULL,
  latitude = NULL,
  eos = getOption("oceEOS", default = "gsw")
)

Arguments

salinity	either practical salinity (in which case temperature and pressure must be provided) or an oce object (in which case salinity, etc. are inferred from the object).
temperature	in-situ temperature (^\circC)
pressure	pressure (dbar)
longitude	longitude of observation (only used if eos="gsw"; see “Details”).
latitude	latitude of observation (only used if eos="gsw"; see “Details”).
eos	equation of state, either "unesco" or "gsw".

Value

Value in psu/^\circC.

Author(s)

Dan Kelley

References

The eos="unesco" formulae are based on the UNESCO equation of state, but are formulated empirically by Trevor J. McDougall, 1987, Neutral Surfaces, Journal of Physical Oceanography, volume 17, pages 1950-1964. The eos="gsw" formulae come from GSW; see references in the swRho() documentation.

See Also

Other functions that calculate seawater properties: T68fromT90(), T90fromT48(), T90fromT68(), computableWaterProperties(), locationForGsw(), swAbsoluteSalinity(), swAlpha(), swBeta(), swCSTp(), swConservativeTemperature(), swDepth(), swDynamicHeight(), swLapseRate(), swN2(), swPressure(), swRho(), swRrho(), swSCTp(), swSR(), swSTrho(), swSigma0(), swSigma1(), swSigma2(), swSigma3(), swSigma4(), swSigmaTheta(), swSigmaT(), swSigma(), swSoundAbsorption(), swSoundSpeed(), swSpecificHeat(), swSpice(), swSstar(), swTFreeze(), swTSrho(), swThermalConductivity(), swTheta(), swViscosity(), swZ()

Examples

swAlphaOverBeta(40, 10, 4000, eos="unesco") # 0.3476

oce documentation built on July 9, 2023, 5:18 p.m.