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oce (version 0.9-18)

swAlphaOverBeta: 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=300, latitude=30, eos=getOption("oceEOS", default="gsw"))

Arguments

salinity
either practial 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 [$^\circ$C]
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/$^\circ$C.

Details

If the first argument is a ctd object, then salinity, temperature and pressure values are extracted from it, and used for the calculation.

References

The eos="unesco" formulae are based on the UNESCO equation of state, but are formulaed 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.

Examples

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

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