MET 1010 Chapter 10 Global Winds
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Complete list of Terms and Definitions for MET 1010 Chapter 10 Global Winds

Terms Definitions
Thermally Direct Cell warm air rises and cold air sinks
Ekman Spiral surface winds drive surface currents, and each layer of water drags the layer below, but the Coriolis Force changes each layer's direction slightly to make a spiral effect
The Hadley Cell a cellular circulation of air in which warm air rises and cold air sinks, so that cold air from the poles moves to the equators at the surface, then rises as it warms and goes back to the poles aloft
Converging surface flows cause low surface pressure, uprising air, heavy precipitation
Ferrel Cell In the three-cell model, 30 degrees to 60 degrees latitude, thermally indirect cell in subpolar low
In the three-cell model, the Hadley cell goes from.... to..... 0 degrees to 30 degrees latitude
Newton's Third Law For every action there is an equal and opposite reaction
Polar Cell In three-cell model, 60-90 degrees latitude, Hadley-type thermally-direct cell in polar high
Jet streams swiftly flowing air currents aloft
Intertropical Convergence Zone (ITCZ) at equator, NE trades meet SE trades and converge, rise, and turns back into Hadley cell
Wind and pressure systems aloft Winds aloft are stronger due to low friction, it is close to a geostrophic system and three-cell model doesn't apply
Diverging surface flows cause high surface pressure, sinking air, dry climate
Trade Winds wind from horse latitudes goes back to the equator, but is directed west by the Coriolis Force, causing Northeasterly winds
Seasonal highs and lows (over continents) Winter: Siberian, Canadian highs; Summer (thermal lows): SE US, Iran
Tropopause Jet Streams Subtropical; Polar- as a result of strong temperature gradients, there are strong westward winds and a meandering pattern that may merge or split, discontinuous
Semi-permanent highs and lows persist throughout the year, correspond to converging/diverging upper air masses (over ocean) (Bermuda, Pacific highs / Icelandic, Aleutian laws)
General Circulation prevailing winds on a global scale
Thermally indirect cell cold air rises and warm air sinks
Horse latitudes weak horizontal winds due to small Pressure Gradient in subtropical highs
Subtropical Highs at equator, high surface pressure resulting from air convergence, cool air sinks and warms to cause clear skies and major deserts
Newton's Third Law applied to the atmosphere The atmosphere exerts a friction on the Earth's surface driving surface currents of the ocean
Is the Single Cell model accurate? No, because it is too simple.
The Single Cell model of general circulation a simplified model that assumes that the earth's surface is uniformly covered in water, no seasonal variations, earth does not rotate
The general circulation of the atmosphere is the result of... uneven heating of the earth's surface and the earth's rotation so that the air circulates in order to balance heat and pressure distribution.
The Three Cell Model of general circulation a simplified model that assumes that the earth is covered entirely in water, there are no seasonal variations, and the earth rotates
gyres circular whirls of ocean currents
Water Upwelling wind along the coast forces warm surface water away from coast so deeper cold water rises to replace it