Presentation on theme: "Atmospheric Pressure The Earth's land surface is actually located at the bottom of a vast ocean of air. Like the water in the ocean, the air in the atmosphere."— Presentation transcript:
2Atmospheric PressureThe Earth's land surface is actually located at the bottom of a vast ocean of air.Like the water in the ocean, the air in the atmosphere is constantly pressing on the solid or liquid surface beneath it.
3Atmospheric PressureAtmospheric pressure. This figure depicts atmospheric pressure as the weight of a column of air. (a) Metric system. The weight of a column of air 1 cm on a side is balanced by the weight of a mass of about 1kg. (b) English system. The weight of a column of air 1 in. on a side is balanced by a weight of about 15 pounds.
4Air Pressure Changes With Altitude Because atmospheric pressure decreases rapidly with altitude near the surface, a small change in elevation will often produce a significant change in air pressure.
5Air Pressure Changes With Altitude Atmospheric pressure decreases with increasing altitude above the Earth's surface.
6WindWind is caused by differences in atmospheric pressure from place to place. Air tends to move from high to low pressure until the air pressures are equal.For example, pressure was higher over Wichita than Columbus, a pressure gradient force would push air from Wichita to Columbus.
7WindIsobars and a pressure gradient. High pressure is centered at Wichita, and low pressure is centered at Columbus.
8The Coriolis EffectAn object in motion on the Earth's surface always appears to be deflected away from its course. This effect is a result of the Earth's rotation, and is called the Coriolis effect.*See movies on the Coriolis Effect in the geodiscoveries section of your text’s website.
9The Coriolis EffectCoriolis effect direction and strength. The Coriolis effect acts to deflect the paths of winds or ocean currents to the right in the northern hemisphere and to the left in the southern hemisphere as viewed from the starting point.=
10Surface Winds on an Ideal Earth A parcel of air in motion near the surface is subjected to three influences: the pressure gradient that propels the parcel toward low pressure; the Coriolis effect that deflects the parcel, and the frictional forces of the ground surface that slow the parcel down.
11Surface Winds on an Ideal Earth Global surface winds on an ideal Earth. This schematic diagram of global surface winds and pressures shows the features of an ideal Earth, without the disrupting effect of oceans and continents and the variation of the seasons. Surface winds are shown on the disk of the Earth, while the cross section at the right shows winds aloft.
12Global Atmospheric Circulation Wind and air pressure follow both global and local patterns. These patterns are affected by the level of the atmosphere, the hemisphere and the season in which they occur.*See movie on Global Atmospheric Circulation in the geodiscoveries section of your text’s website.
13Rossby WavesThe smooth westward flow of the upper-air westerlies frequently forms undulations, called Rossby waves.
14Rossby WavesDevelopment of upper-air Rossby waves in the westerlies of the northern hemisphere.
15Ocean CurrentsJust as there is a circulation pattern to the atmosphere, so there is a circulation pattern to the oceans.
16Ocean CurrentsJanuary ocean currents. Surface drifts and currents of the oceans in January.
17El NiñoAt intervals of about three to eight years, a remarkable disturbance of ocean and atmosphere occurs. This phenomenon is called El Niño.*See movie on El Niño in the geodiscoveries section of your text’s website.
18El NiñoMaps of pressures in the tropical Pacific and eastern Indian Ocean in November during normal and El Niño years. In normal year (a), low pressure dominates in Malaysia and northern Australia. In an El Niño year (b), low pressure moves eastward to the central part of the western Pacific and sea-surface temperatures become warmer in the eastern Central Pacific.