1. When dense water masses are first formed, they are not stably stratified. 2. Capelin distribution and migration is linked with ocean currents and water masses . 3. The lower waters mass of NADW form from overflow of the Greenland-Iceland-Scotland Ridge. 4. When these turbulent eddies of different water masses interact, they will mix together. 5. That fresher-water mass , fortunately, was small enough to disperse in a short time. 6. The common thresher is migratory, moving to higher latitudes following warm water masses . 7. The water mass in Lake Tanganyika is huge and very stable. 8. It may be easier to see what happens by considering the non-water mass . 9. The world's oceans are made up of many different water masses . 10. In the depth range of is a water mass referred to as Atlantic Water.
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