ENV100Y5 Chapter Notes -Wave Power, Deep Sea, Pycnocline

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ENV100Y5 Full Course Notes
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Water density increases as salinity rises and as temperature falls. These relationships give rise to different layers of water; heavier (colder and saltier) water sinks, and lighter (warmer and less salty) water remains nearer the surface. Waters of the surface zone are heated by sunlight each day and are stirred by wind such that the proper-ties are fairly uniform throughout the zone. Thermocline- a zone in which temperature decreases rapidly with depth, toward the much colder deep layer (below the zone of warm, salty surface water) Salinity of the water also changes, increasing with depth along the halocline. The density of the water also changes rapidly with depth, increasing along the pycnocline. Cline- zone of rapid transition (transitional zone 18% of the ocean) 2% is surface zone and 80% is deep zone. Colder, saltier water is denser and will sink towards to deep zone.

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