MARN 1002 Lecture Notes - Lecture 10: Ocean Acoustic Tomography, Pacific Ocean, Sofar Channel
Document Summary
Implemented in the north pacific ocean, with acoustic transmissions from 1996 through fall. Viscosity of water is low, and decreases with increasing t. Easier for single-cell organism to stay afloat in cold water. In warm water, single-cell organisms need appendages to float. Important in water surface processes and drop formation. Evaporation and precipitation varies in a consistent manner w/ latitude. Total average oceanic salinity is about 35 g/kg. If the concentration of on of the major ions is known, any and all of the concentrations of other salts can be calculated. Na = 10. 76/19. 35 x 5 = 2. 78 g/kg. Trace elements occur in minute or trace amounts. Their concentration is parts per billion (ppb) ( g/kg or lower) Despite their low concentration, some are very important for life thriving in the ocean (iron, zinc, etc. ) Others may be considered pollutants (lead, mercury)