Download - Air Pressure/Winds

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Page 1: Air Pressure/Winds

Air Pressure/Winds• Air Pressure –weight of the atmosphere

pushing down on Earth (we don’t feel it because air is pushing on all sides, not just down from the top.)

• •Barometer–tool that measures air pressure.• –Use millibarsto show pressure on maps = they makeisobars when connected.

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Connect the same numbers to draw in the isobars.

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So why does air pressure change?

• Elevation – in general, the higher the elevation, the lower the pressure (less pressure to push down on, since you are higher)

• Temperature warm air lowers pressure (it rises and particles move farther apart), and may get rain . Cool air gives increase in pressure, and weather is clearer .

• Humidity – the more water vapor air contains, the lighter the air is = so low pressure. (Remember: warmer air can hold more water vapor and is low pressure)

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Reading Pressure on a Map• Isobars = lines showing air having the same pressure.• High pressure area (or a High ) –Rotates clockwise .• Low pressure area (or a Low ) –Rotates counterclockwise .• Pressure gradient = • –Lines close together show that pressure is quickly changing (and we will have strong winds).Lines further apart shows weakpressure gradient (and we will have weak winds).

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Winds Blow Because…• Air flows from an area of High pressure to an area of Low

Pressure H to

L

• Coriolis Effect -the apparent curve of a moving object due to the Earth’s rotation

–Causes curve to the right in the Northern Hemisphere –Causes curve to the left in the Southern Hemisphere • Jet Stream – fast moving winds near the top of the

troposphere (winds 120-240 kph) –In the US the jet streams supplies energy to storms and directs their paths.• Anemometer–tool that measures wind speed .

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Global Wind Patterns• Doldrums or Intertropical Convergence Zone (ITCZ) –Low

pressure in tropics –Hot, humid, little to no wind, rain is common.• Subtropical highs or Horse Latitudes –between 20-35

degrees –Deserts –because sinking cooler air with no precipitation is near.• Tradewinds–between 35-60 degrees latitude –Warm, steady, winds• Polar highs –High pressure above 60 degrees latitude (in

the poles) –Where cold air sinks at the poles, usually easterly surface winds.

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Questions

• Which global wind pattern do we live in?The westerlies

• How are the winds named?from the direction they came from

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Global Wind Patterns

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Effects of seasons on winds…

• With a change in air pressure the direction of winds changes

• So winds change direction with the seasons . –Monsoons• Occur southern Asia• Heavy rains

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Local Winds: Land Breeze –vs- Sea Breeze

• Sea Breeze - occurs during the day • Coastal land is warmer than water, causing decrease in pressure

over land • So breeze flows from High to Low/from Sea to Land . (cool breeze from sea blows inland)

• Land Breeze – Occurs at night • Air over land is colder than air over water, causing decrease in pressure over the water. • So, breeze flows from High to Low/from Land to Sea__ (cool

breeze from land blows to sea)


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