Using the simplified linear approximating to the equation of state of seawater with respect to standard seawater (with average density po= 1027 kg/m3, in-situ temperature To= 10°C and salinity So= 35) given below: Pstr - Po= [-a . (T-To)+b . (S-So) + k . p] with constant coefficients a = 0.15 kg/m³ per degree Çelcius: b = 0.78 kg/m³ per part per k= 4.5 x10³ kg/m³ per decibar thousand salinity; calculate the in situ density (pstp) values at the four levels measured with a CTD station with the following properties:

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3)
Using the simplified linear approximating to the equation of state of seawater with
respect to standard seawater (with average density po= 1027 kg/m3, in-situ temperature
To= 10°C and salinity So= 35) given below:
Pstr - Po= [-a . (T-To) + b . (S-So) + k .
p]
with constant coefficients
a = 0.15 kg/m³ per degree Celcius:
b = 0.78 kg/m per part per thousand salinity;
k = 4.5 x10-3 kg/m³ per decibar
calculate the in situ density (Pstp) values at the four levels measured with a CTD station
with the following properties:
Pstr
p = 50 db, T= 27.06 °C, S = 34.992?
p = 500 db, T = 6.54 °C, S = 34.271?
р 3 2,500 db, Т %3D1.76 °C, S%3D 34.663?
p = 4,500 db, T = 1.45 °C, S = 34.696?
Transcribed Image Text:3) Using the simplified linear approximating to the equation of state of seawater with respect to standard seawater (with average density po= 1027 kg/m3, in-situ temperature To= 10°C and salinity So= 35) given below: Pstr - Po= [-a . (T-To) + b . (S-So) + k . p] with constant coefficients a = 0.15 kg/m³ per degree Celcius: b = 0.78 kg/m per part per thousand salinity; k = 4.5 x10-3 kg/m³ per decibar calculate the in situ density (Pstp) values at the four levels measured with a CTD station with the following properties: Pstr p = 50 db, T= 27.06 °C, S = 34.992? p = 500 db, T = 6.54 °C, S = 34.271? р 3 2,500 db, Т %3D1.76 °C, S%3D 34.663? p = 4,500 db, T = 1.45 °C, S = 34.696?
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