Chapter 6 - Atmosphere-Ocean-Cryosphere Interactions Flashcards
Albedo
The proportion of incident light reflected by the surface of a celestial body.
What are the three main factors responsible for oceanic movement?
1) winds moving over the top surface.
2) spatial variations in the density of water
3) the Coriolis Effect
SST
Sea-Surface Temperature
PDO
Pacific Decodal Oscillations
PDO Cool Phase
Cooler SST in eastern Pacific to the North, near Alaska
Warmer SST in eastern Pacific mid-north
PDO Warm Phase
Opposite of PDO cool phase
Shifts in PDO are accompanied by what changes?
1) changes in wind direction
2) changes in air pressure
Differences in _____ of water, which is largely a function of temperature and salinity, can set water in motion. Once the water is in motion, its path is deflected by the _____ _____.
density, Coriolis Effect
Wind blowing across a body of water causes water motion via …
1) waves, on the small scale
2) water currents, in the global scale
Null Point
At about 100m below the surface, the effects of wind on the surface vanish (due to viscosity)
Coriolis Effect
The tendency to rotate due to decreasing linear velocity while traveling away from the equator.
Apparent deflection to the right ..CW?.. when North of Equator
Ekman Spiral
….
Horse Latitudes
….
Doldrums
….
Gyres
Interacting circular motions that approximate the direction of near surface currents
Indian Ocean currents
1) the warm Mozambique current flowing south, east of Africa
2) the cool Western Australian current flowing north
3) the warm, lateral current from the Pacific
4) ineractions with the cold Antarctic Circumpolar Current
Western Pacific currents
Kuroshio Current
North Pacific Current
East Australian Current
West Wind Drift
Northern Atlatic Currents
Gulf Stream
North Atlantic Drift
Canary Current
Southern Atlantic Currents
Benguela Current
Brazil Current
Antarctic Circumpolar Current
Northern Pacific Currents
California Current
Alaska Current
Bering Current