convert_StoR | R Documentation |
Estimates the conductivity ratio from salinity, temperature and pressure.
The equation is valid over ranges of temperature from -2 to 35
^\circ
C, pressure of 0 - 1000 bar and salinity 2-42
in the world ocean.
convert_StoR(S = 35, t = 25, p = max(0, P-1.013253), P = 1.013253)
S |
(practical) Salinity, -, |
t |
Temperature, |
P |
True Pressure, bar, |
p |
Gauge (or applied) pressure, the pressure referenced against the local atmospheric pressure, bar. |
The conductivity ratio (-), this is the conductivity at (S, t, p), divided by the conductivity at S = 35, t = 15, p = 0.
Pressure here is true pressure, 1 bar (at sea surface), in contrast to hydrostatic pressure in dbar of original formula.
The conductivity ratio for Salinity = 40, t = 40, p
=
1000 is 1.888091.
Karline Soetaert <karline.soetaert@nioz.nl>
Fofonoff NP and Millard RC Jr, 1983. Algorithms for computation of
fundamental properties of seawater. UNESCO technical papers in marine
science, 44, 53 pp.
http://unesdoc.unesco.org/images/0005/000598/059832EB.pdf
convert_AStoPS
, convert_PStoAS
,
convert_RtoS
,
convert_StoCl
,
convert_p
, convert_T
,
convert_StoR(S = 40, t = 40, p = 1000)
convert_StoR(S = 35, t = 15, p = 0)
# Check values:
convert_StoR(S = 25, t = 10, p = 0) # 0.654990
convert_StoR(S = 25, t = 10, p = 100) # 0.662975
convert_StoR(S = 25, t = 10, p = 1000) # 0.712912
convert_StoR(S = 35, t = 10, p = 100) # 0.897778
convert_StoR(S = 40, t = 10, p = 100) # 1.011334
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