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air pressure
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Meteorology

WCHS Meteorology Chapter 19

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air pressure is exerted in all directions; pressure pushing down on an object exactly balances the air pressure pushing up on the object
barometer is a device used for measuring air pressure; when air pressure increases, the mercury in tube rises, when it decreases, the the mercury falls; invented by Torricelli in 1643
Wind is the result of horizontal differences in air pressure, air flow from areas of higher presure to areas of lower pressure
pressure differences the unequal heating of earth's surface; solar rediation is the ultimate energy source for most wind
wind control three factors combined; pressure differences, the Coriolis effect and friction
pressure gradient the amount of pressure change occurring over a given distance; closely spaced isobars indicate a steep pressure graidient and high winds, widely space isobars indicate weak pressure and light winds
Coriolis effect describes how earth's rotation affects moving objects; all reee-moving objects or fluids, including the widn are deflected to the right of their path of motion in the Norhtern Hemisphere, and to the left in the sourthern hempsphere
jet streams fast-moving rivers of air that travel between 120 and 240 kilometers per hour in a west to east direction
cyclones centers of low pressure; pressure decreases from outer isobars toward the center
anticyclone Centers of high pressure; isoubars increase from the outside toward the center
friction causes a net flow of air inward around a cyclone and a net flow of air outward around an anticyclone
pressure gradient & Coriolis effect applied to pressure centers in the Northern Hemisphere, winds blow counterclockwise around a low, and clockwise around a high.
trade winds two belts of winds that blow almost constantly from easterly directions; travels toward the equator; are located on the north and south sides of the subtropical highs
westerlies travels toward the poles; the dominant west-to-east motion of the atmosphere that characterizes the regions on the poleward side of the subtropical highs
polar easterlies winds that blow form the polar high towards the subpolar low
polar front the stormy frontal zone separating cold air masses of polar origin from warm air masses of tropical origin
monsooms seasonal reversal of wind direction associated with large continents, especially Asia; in winter, the wind blows from land to sea; in summer, the wind blows from sea to land
local winds caused either by topogrpahic effects or by variations in surface compostiion, land and water, in the immediate area
prevailing wind a wind that consistently blows from one direction more than from another
anemometer measuring instrument commonly used to measure wind speed
El Nino at irregular intervals of 3-7 years, warm countercurrents become unusually strong and replace normally cold offshore waters with warm equatorial waters
La Nina opposite of El Nino, once thought to be normal conditions, now considered to be an important atmospheric phenomenon; when surface temperatures in eastern Pacific are colder thatn average
Created by: dmoudy
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