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Ocean current - Wikipedia ... Ocean current
Fish or cut bait
The offspring remain in the fresh water until they are ready to migrate to the ocean as smolts. In a few years, the surviving adults return, climb the fish ladder, and reach their spawning ground to continue the life cycle. [10]: 3 Of the millions of young fish born, only a relative few survive to adulthood. Causes of death include natural ...
At 150 metres (500 ft) below the surface, water has flowed as fast as 0.40 metres per second (1.3 ft/s), showing mixing up to 1,000 times the normal rate in the deep ocean. The flow is hydraulically-controlled, which means it flows smoothly over a shallow ridge just off Cape Flattery then on the other side forms a turbulent breaking undersea ...
Slack tide or slack water is the short period in a body of tidal water when the water is completely unstressed, and there is no movement either way in the tidal stream. It occurs before the direction of the tidal stream reverses. [1] Slack water can be estimated using a tidal atlas or the tidal diamond information on a nautical chart. [2]
The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater, [1] which may be fresh, saline, or brackish, depending on the locality. It can also be simply explained as the depth below which the ground is saturated.
The water transport in the Gulf Stream gradually increases from 30 Sv in the Florida Current to a maximum of 150 Sv south of Newfoundland at 55° W longitude. [4] The Antarctic Circumpolar Current, at approximately 125 Sv, is the largest ocean current. [5] The entire global input of fresh water from rivers to the ocean is approximately 1.2 Sv. [6]
Body of water