Oceans Flashcards
Percent of earth covered by oceans (area)
75%
Volume of water on earth in oceans
- 2% of all water on earth
8. 4 million liters available per person
Salinity
?The proportion of dissolved salts to pure water, usually expressed in parts per thousand (%)
Most comment salt in ocean
NaCl
Why ocean now thought to be salty
?As rainwater passes through soil and percolates through rocks, it dissolves some of the minerals, a process called weathering. This is the water we drink, and of course, we cannot taste the salt because its concentration is too low. Eventually, this water with its small load of dissolved minerals or salts reaches a stream and flows into lakes and the ocean. The annual addition of dissolved salts by rivers is only a tiny fraction of the total salt in the ocean. The dissolved salts carried by all the world’s rivers would equal the salt in the ocean in about 200 to 300 million years.
Why salinity varies from place to place
? Vertical motion in the ocean are due to density differences do you two different temperature horizontal difference at the surface due to wind direction
Whether relative percent of salts varies
?Seawater is denser than both fresh water and pure water (density 1.0 kg/L at 4 °C (39 °F)) because the dissolved salts increase the mass by a larger proportion than the volume. The freezing point of seawater decreases as salt concentration increases. At typical salinity, it freezes at about −2 °C
Factors affecting density of water
Temperature ( cold water is more dense than hot)
Currents
?An ocean current is any more or less permanent or continuous, directed movement of ocean water that flows in one of the Earth’s oceans. The currents are generated from the forces acting upon the water like the earth’s rotation, the wind, the temperature and salinity differences and the gravitation of the moon.
Gulf stream and resulting temperatures in North Europe
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Black smokers, Life at vents, where they get their energy
?Hydrothermal vents are often associated with undersea volcanoes. This is because the vents are created and sustained by the heat of volcanic activity at tectonic plate boundaries, found throughout the globe.
At these locations, seawater seeps through cracks in the seafloor and is heated by molten rock. This causes chemical reactions between the two, and the altered seawater becomes hydrothermal fluid. This hot fluid then jets back into the ocean, forming a hydrothermal vent.
Despite the seemingly harsh volcanic environment, these vents are actually home to a variety of life. Microbes, such as bacteria and archaea, live here – harvesting chemical energy from the hydrothermal fluid. These microbes form the base of a unique foodchain that includes tubeworms, shrimp, and even crabs that live in communities around the vents.
Sonar, how it works
Sonar (originally an acronym for SOund Navigation And Ranging) is a technique that uses sound propagation (usually underwater, as in submarine navigation) to navigate, communicate with or detect objects on or under the surface of the water, such as other vessels. Two types of technology share the name “sonar”: passive sonar is essentially listening for the sound made by vessels; active sonar is emitting pulses of sounds and listening for echoes.
Structures on Seafloor
?Part of the Earth’s outer surface that is comprised of the ocean floor, mid-oceanic ridges, continental rise, and continental slope. The ocean basins are filled with saline water that makes up the oceans. Flat plain found at the bottom of the ocean. The ocean floor represents the surface of the oceanic crust.
Trenches
?a long, narrow, deep depression in the ocean floor, typically one running parallel to a plate boundary and marking a subduction zone.
plural noun: ocean trenches
Mid ocean ridges
? A mid-ocean ridge or mid-oceanic ridge is an underwater mountain range, formed by plate tectonics. This uplifting of the ocean floor occurs when convection currents rise in the mantle beneath the oceanic crust and create magma where two tectonic plates meet at a divergent boundary.