teos2eos_geo {seacarb} | R Documentation |
Convert temperature and salinity from TEOS-10 to EOS-80
Description
Converts conservative temperature to in situ temperature and absolute salinity to practical salinity (SP). Salinity conversion depends on depth and geographic location.
Usage
teos2eos_geo(SA, CT, P=0, long=1.e20, lat=1.e20)
Arguments
SA |
Absolute salinity in g/kg |
CT |
Conservative temperature in degrees C |
P |
Sea water pressure in dbar |
long |
Longitude in decimal degrees [ 0 ... +360 ] or [ -180 ... +180 ] |
lat |
Latitude in decimal degrees [-90 ... 90] |
Details
Conversion from absolute to practical salinity depends on water density anomaly which is correlated with silicate concentration. This function relies on silicate concentration taken from WOA (World Ocean Atlas) to evaluate the density anomaly.
Value
The function returns a data frame containing the following columns:
T |
In situ temperature (deg C) |
SP |
Practical salinity (psu) |
Author(s)
Jean-Marie Epitalon
References
McDougall T. J., Jackett D. R., Millero F. J., Pawlowicz R. and Barker P. M., 2012. A global algorithm for estimating Absolute Salinity. Ocean Science 8, 1123-1134.
Pawlowicz R., Wright D. G. and Millero F. J., 2011. The effects of biogeochemical processes on oceanic conductivity/salinity/density relationships and the characterization of real seawater. Ocean Science 7, 363-387.
Pawlowicz R., 2013. What every oceanographer needs to know about TEOS-10 (The TEOS-10 Primer). http://www.teos-10.org/
See Also
eos2teos_geo does the reverse, teos2eos_chem, sa2sp_geo, package gsw
Examples
# Calculate in situ temperature and practical salinity of a sample with
# Absolute salinity of 35 g/kg, conservative temperature of 18 deg C,
# depth is 10 dbar and location is 188 degrees East and 4 degrees North.
f <- teos2eos_geo(SA=35, CT=18, P=10, long=188, lat=4)
T <- f$T # in situ temperature
SP <- f$SP # Practical salinity