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Convergent tectonic boundaries
plates collide/move towards each other
Divergent tectonic boundaries
plates move apart from each other = creates new oceanic crust (eg: Mid-Atlantic Ridge)
CTD
instrument used by oceanographers in which measures conductivity, temperature, and depth (pressure) of seawater
Ekman Spiral
the consequence rotation pattern in the upper layers of the ocean
Ekman Layer
total depth of the frictional influence of the wind
Ekman Drift
mean current across the Ekman layer
strongly influenced by the thickness of the mixed layer
largely dependent on the time of year and wind speed
Ekman Transport
the volume of water transported by the Ekman drift
Bathymetry
The study of underwater depth of lake or ocean floors.
Continental shelf
The part of the ocean floor bordering the continents at a depth of 200 m or less below the sea surface.
Continental slope
The part of the ocean floor extending from the edge of the continental shelf to the start of the continental rise. The continental slope has an average gradient of around 4deg.
Abyssal plane
The flat part of the ocean floor that lies between about 4 and 6 km below the sea surface.
Hydrothermal vent
Fissures on the seafloor out of which flows water that has been heated by underlying magma.
Constancy of composition
The principle for seawater that, although the concentration of dissolved salts can vary from place to place, the relative proportions of the ions remains virtually constant.
Stratification
Where water masses with different properties of salinity, oxygenation, density and temperature form layers that act as barriers to water mixing.
Albedo
The reflection coefficient of a surface - the fraction of the amount of incoming radiation that is reflected from a surface. (measure of how much incoming radiation a surface reflects → eg: low albedo (dark surfaces, like the ocean) most of solar radiation is absorbed to heat surface)
Isohalines
Contour line joining points of equal salinity either on maps or in vertical sections.
Wind-mixed layer
Surface water that has been mixed by the wind to create a layer with uniform physical properties. (locations where winds are stronger the mixed layer can be up to 200m thick // after the mixed layer both temp. and salinity decrease = permanent thermocline)
Eddy viscosity
Internal friction between the molecules of a liquid that transfers momentum.
Permanent thermocline
The region beneath the mixed layer where temperature decreases with depth.
Isotherms
Contours of constant temperature.
Gyre
A large-scale circulatory feature of the ocean circulation, usually extending across many thousands of kilometers.
Water mass
A very large volume of water with uniform temperature, salinity and, therefore, density.
Salt rejection
A process that occurs during sea ice formation where salt is pushed from forming ice into the surrounding seawater, increasing the salt concentration there.
Mid-Atlantic Ridge
underwater mountain ranges formed by tectonic plates pulling apart, a peak rising from abyssal planes & North-South suboceanic ridge in the Atlantic Ocean from Iceland to Antarctica