Physical properties of seawater
Effect of Temperature and Salinity on Compressibility
Example 3C: Effect of Temperature and Salinity on Compressibility
As discussed in DPO 3.5.4, seawater is slightly compressible.
Files that may be needed or created in this example:
So now let's demonstrate this with JOA!
Exercise 3C-01: Seawater Properties - Compressibility
- Go back to Exercise 3B-01 where you made the temperature versus salinity plot for the A16_2005_sta085_bottle.joa data.
- Make that plot again, but now using potential temperature (THTA) instead of temperature for the Y-axis, and bottle salinity (SALT) instead of CTD salinity for the x-axis.
- Adjust the plot parameters in the Advanced panel of the Property-Property Plot dialog box until it looks like this:
- Now, when you click OK, you will get this plot:
- Go back to the Property-Property Plot dialog box Advanced page:
- Double-click or control-click on a map plot
- Or type [ctrl/cmd]-R or Edit → Edit: plotname when a map plot is the front-most window.
- Now, experiment with the isopycnal “slider” on the bottom of the Advanced page:
- Try sliding it to 4000 (4000 decibars), while watching the plotted isopycnal lines on the potential temperature versus salinity plot.
- Notice that the numeric isopycnal line label values (these are density-related sigma units as explained in DPO) both increase with increasing pressure (as you slide the slider to the right) and also change their slope.
- Notice how they appear to flatten as pressure increases? Compared to the situation which prevails at sea surface pressure (0 decibars), at 4000 decibars a given change in temperature now has a smaller effect in changing density.
To visualize the deep water at the A16_2007 station 085 bottle data plot, select the deep water portion of your JOA potential temperature versus salinity plot (the part from 0 to 4 °C and salinity 34.5 to 35), i.e.
- Set up the Advanced panel of the Property-Property Plot dialog box like this:
- After you click on OK, you should see this plot:
- Note that the coldest (and deepest) waters have a lower density, expressed as sigma-0, than the warmer (and somewhat shallower)
waters immediately above.
Now try going back and forth between the dialog box and the plot to try different reference pressures for the isopycnals. You will see that the apparent instability (apparent dense water on top of less dense water) in the deep water when 0 decibars was used for the isopycnal reference pressure goes away when an appropriate deep reference pressure (ca. 4000 decibars) is used.
Notice that at A16_2007 station 085, in the deeper layers there is a relative salinity maximum near 2000 meters which, at ca. 3.2 °C, is significantly warmer than the relatively fresh, cold bottom waters underneath.
This particular layering of deep temperature and salinity is characteristic of the Atlantic Ocean, and presents very well the relative layer-to-layer change of temperature and salinity needed to best highlight the importance of using an appropriate reference pressure to examine deep water density. In later exercises, we will contrast the layering in the other oceans.