Atmospheric Pressure Force exerted by the weight of the air above

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Presentation transcript:

Atmospheric Pressure Force exerted by the weight of the air above Weight of the air at sea level 14.7 pounds per square inch 1 kilogram per square centimeter

Atmospheric Pressure Decreases with increasing altitude Units of measurement Millibar (mb) – standard sea-level pressure is 1013.2 mb

Sea-Level Pressure

Atmospheric Pressure Units of measurement Inches of mercury – standard sea-level pressure is 29.92 inches of mercury

Atmospheric Pressure Instruments for measuring Mercury barometer Invented by Torricelli in 1643 Uses a glass tube filled with mercury barometer Aneroid barometer “Without liquid” Uses an expanding chamber Barograph (continuously records the air pressure)

A Mercury Barometer

Aneroid Barometer

Aneroid Barograph

Wind Horizontal movement of air Out of areas of high pressure Into areas of low pressure

Wind Controls of wind Pressure gradient force Isobars – lines of equal air pressure Pressure gradient – pressure change over distance

Weather Map with Isobars

Wind Controls of wind Coriolis effect Friction Apparent deflection in the wind direction due to Earth’s rotation Deflection is to the right in the Northern Hemisphere and to the left in the Southern Hemisphere Friction Only important near the surface Acts to slow the air’s movement

The Coriolis Effect

Wind Upper air winds Generally blow parallel to isobars – called geostrophic winds Lack of friction with surface allows higher speeds Jet stream “River” of air High altitude High velocity (120–240) kilometers per hour

The Geostrophic Wind

Effects of Friction on Wind

Cyclones and Anticyclones Associated with rising air Center of low pressure Often bring clouds and precipitation Anticyclone Associated with sinking air A center of high pressure Pressure increases toward the center

Cyclonic and Anticyclonic Winds

Cyclones and Anticyclones A center of low pressure Pressure decreases toward the center Winds associated with a cyclone In the Northern Hemisphere Inward (convergence) Counterclockwise In the Southern Hemisphere Clockwise

Cyclones and Anticyclones Winds associated with an anticyclone In the Northern Hemisphere Outward (divergence) Clockwise In the Southern Hemisphere Counterclockwise Associated with subsiding air Usually bring “fair” weather

Airflow Associated with Surface Cyclones and Anticyclones