Compute \(\sigma_\theta\), the potential density of seawater (minus 1000 kg/m\(^3\)), referenced to 2000db pressure.
swSigma2(salinity, temperature = NULL, pressure = NULL,
longitude = NULL, latitude = NULL, eos = getOption("oceEOS",
default = "gsw"))
either practical salinity (in which case temperature
and pressure
must be provided) or an oce
object, in
which case salinity
, temperature
(in the ITS-90 scale; see
next item), etc. are inferred from the object.
in-situ temperature [\(^\circ\)C], defined
on the ITS-90 scale. This scale is used by GSW-style calculation (as
requested by setting eos="gsw"
), and is the value contained within
ctd
objects (and probably most other objects created with data
acquired in the past decade or two). Since the UNESCO-style calculation is
based on IPTS-68, the temperature is converted within the present function,
using T68fromT90
.
pressure [dbar]
longitude of observation (only used if eos="gsw"
;
see ‘Details’).
latitude of observation (only used if eos="gsw"
; see
‘Details’).
equation of state, either "unesco"
[1,2] or "gsw"
[3,4].
Potential density anomaly [kg/m\(^3\)].
Definition: \(\sigma_1=\sigma_\theta=\rho(S,\theta(S,t,p),1000\) - 2000 kg/m\(^3\).
See citations provided in the swRho
documentation.
Other functions that calculate seawater properties: T68fromT90
,
T90fromT48
, T90fromT68
,
swAbsoluteSalinity
,
swAlphaOverBeta
, swAlpha
,
swBeta
, swCSTp
,
swConservativeTemperature
,
swDepth
, swDynamicHeight
,
swLapseRate
, swN2
,
swPressure
, swRho
,
swRrho
, swSCTp
,
swSTrho
, swSigma0
,
swSigma1
, swSigma3
,
swSigma4
, swSigmaTheta
,
swSigmaT
, swSigma
,
swSoundAbsorption
,
swSoundSpeed
, swSpecificHeat
,
swSpice
, swTFreeze
,
swTSrho
,
swThermalConductivity
,
swTheta
, swViscosity
,
swZ