Ocean Circulation Flashcards
reasons we study the ocean
food, transportation, recreation, influences atomsphereic weather and climate
earth’s five ocean basins
pacific, atlantic, indian, arctic, southern
mid-ocean ridges
longest mountain range in the world
active continental margins
tectonically active zones, subduction zone, small width and sediment input (left side of south america)
passive continental margins
are within plates and low tectonic activity, generally wide, receive large influx of sediment input (right side of south america); not a plate boundary
list the three major layers in the oceans regarding density
surface layer,transition/thermocline, deepzone
surface layer
warmest, 100 m deep. makes up only 2%
transition/thermocline layer
makes up 18%, 1500 m, just above freezing point
deep zone
makes up 80%, temperature is low and constant
seawater
salinity is around 3.5%, salt can be removed by biological organisms, common evaporation and freezing, salinity in oceans is essentially constant
salitinity increases when…
evaporation, chemical weathing from land release elements, volcanic eruption, freezing of sea water
salinity decreases when
fresh water from land/preciptation, plant and animals take elements
ocean surface motion
caused by winds that drag the surface of the water, sun energy, controlled by wind
ocean depth motion
the deep water flow and surface current is quite different, driven by temperature and salinity, controlled by density
when there is high salinity
there is high density and water tends to sink