IDL contouring routine was used to interpolate the data from pressure to sigma surfaces. Levitus climatology is shown for comparison. The figures show transports on pressure surfaces and transports on sigma surfaces. Levitus climatology is shown for comparison. Transports The transports for the north-south crossections were clculated by integrating velocities from north to south.
Figures show transports on sigma surfaces .
Comparison of transports for calibrated and uncalibrated data. Calibrated data are available for Spring 93 and Fal 92 cruises, from Dave Musgrave. For these cruises the transports in 1500 db deep layer were calculated and compared with similar transports from uncalibrated data. The figures are shown below .