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