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above a given point, usually expressed in millibars (mb) or inches of mercury (in. Hg) |
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Mercury barometer Aneroid barometer |
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– Column of mercury in a glass tube under vacuum – Mercury rises or falls with changes in air pressure |
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Small, sealed chamber partially emptied of air – Chamber connected to a mechanism that is sensitive to changes in the chamber – As air pressure varies, mechanism moves needle on a dial |
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the horizontal motion of air across Earth’s surface |
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wind updrafts and downdrafts |
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Driving Forces within the Atmosphere |
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created because of a pressure difference between high- and low-pressure areas |
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The closer together the lines |
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Because the earth is a sphere and rotates on its axis,.... |
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air moving across the surface appears to curve. |
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Apparent deflection of straight line to the right in the Northern Hemisphere and to the left in Southern Hemisphere |
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The effects of wind friction near the surface extends to a height of about |
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Variables affecting friction: |
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– Surface texture – Wind speed – Time of day and year – Atmospheric conditions |
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friction disrupts equilibrium between pressure gradient and Coriolis forces: |
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Near the surface, friction disrupts equilibrium between pressure gradient and Coriolis forces: |
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Primary high- and low-pressure areas: |
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– Interrupted cells or uneven belts of similar pressure that stretch across the globe |
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Secondary high- and low-pressure areas are smaller than the primary systems |
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– Form within the primary pressure areas – Range from a few hundred to a few thousand kilometers in diameter – Hundreds to thousands of meters high |
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Primary High-Pressure and Low- Pressure Areas |
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Equatorial low-pressure trough |
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Rising warm air creates an equatorial trough, low- pressure belt called the |
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Rising warm air occurs within the |
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Here, trade winds converge near equator |
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Monotony of the weather has given rise to the expression |
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In northern hemisphere, trade winds blow mainly towards the |
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In northern hemisphere, trade winds blow mainly towards the southwest: |
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Utilized by mariners for trade when traveling from Europe to America – Caused Columbus to land in West Indies rather than continental North America |
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Trade winds in the southern hemisphere are important in affecting _____ |
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south-easterly winds blowing towards the northwest diminish |
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Rising air within ____ once aloft, moves towards the poles |
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This northward-moving air, however, must converge aloft cause... |
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energy into outer space, cools, and becomes more dense, causing it to sink in regions known as highs. |
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....masses aloft causes the air to sink at ~30o north and south latitudes to form Subtropical Highs |
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convergence and cooling of air |
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Occur close to 30o north and south latitudes |
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Downwelling air is dry (why?): |
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Worlds largest deserts occur in these zones |
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subtropical highs (gentle winds) |
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Ships sailing to America often languished in these regions due to lack of winds |
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When food supplies diminished.... |
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horses were either eaten or thrown overboard to lighten load – Hence the term “horse latitudes” |
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higher latitudes than the trade winds |
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In northern hemisphere, westerlies mainly blow from the... |
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west towards the northeast |
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In northern hemisphere, westerlies mainly blow from the west towards the northeast: |
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– Utilized by sailors returning to Europe from North America |
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The Bermuda High steers the paths of |
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In winter, two cells dominate around 60o N latitude but weaken or disappear in summer: |
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Aleutian low in the Pacific Ocean – Icelandic low in the Atlantic Ocean |
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Polar atmospheric mass is |
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small and receives little energy from the sun |
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Cold air aloft sinks towards the surface |
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– Descending winds diverge clockwise near the surface in N. hemisphere (counterclockwise in S. hemisphere) – Surface winds moving away from northern polar region are therefore anticyclonic |
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Arctic high less pronounced than Antarctic high: |
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– Arctic high tends to form over continental areas in winter (Canadian and Siberian highs) |
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