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NSF North Mississippi GK-8 NSF North Mississippi GK-8 Weather! Weather! Matt Aufman Matt Aufman NSF North Mississippi GK-8 NSF North Mississippi GK-8 November 2005 November 2005

NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Page 1: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

NSF North Mississippi GK-8NSF North Mississippi GK-8

Weather!Weather!

Matt AufmanMatt Aufman

NSF North Mississippi GK-8NSF North Mississippi GK-8

November 2005November 2005

Page 2: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Temperature• You will usually see temperature measured in °F for maps of the United States

• Maps of foreign countries will usually be measured in °C

Page 3: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Relative Humidity• The relative humidity tells us how “full” the air is at the time of measurement.

• For example, 90% relative humidity means that at that moment the air is holding 90% of the maximum amount of water it could.

Page 4: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Cloud Cover Symbols• You will often see the circles drawn on a weather map

Page 5: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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High and Low Pressure Areas

• High pressure causes air to sink

• Usually results in several days of clear sunny skies

• Air rises in low pressure areas and forms water droplets

• Usually results in rain and storms

Page 6: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Air MassesThere are two types of air masses:

1. Continental Polar air masses

2. Maritime Tropical air masses

Page 7: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Fronts

A front is the boundary separating air masses of different densities

Fronts extend both vertically and horizontally in the atmosphere

Page 8: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Fronts: Five Types of Fronts1. Cold Front: The zone where cold air is replacing warmer air

• In U.S., cold fronts usually move from northwest to southeast

• Air gets drier after a cold front moves through

Page 9: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Fronts: Five Types of Fronts2. Warm Front: The zone where warm air is replacing colder air

• In U.S., warm fronts usually move from southwest to northeast

• Air gets more humid after a warm front moves through

Page 10: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Fronts: Five Types of Fronts3. Stationary Front: When either a cold or warm front stops moving

• When the front starts moving again it returns to either being a cold or warm front

Page 11: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Fronts: Five Types of Fronts4. Occluded Front: Formed when a cold front overtakes a warm front

• This occurrence usually results in storms over an area

• In U.S., the colder air usually lies to the west

Page 12: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Fronts: Five Types of Fronts5. Dry Line (Dew Point Front): Boundary separating a dry air mass from a moist air mass

This occurrence can result in tornadoes being formed

Usually found in western part of U.S.

Page 13: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Clouds: Five Types of Clouds1. High-Level Clouds: Usually found at greater than 20,000 ft.

Usually made of ice crystals

Examples include Cirrus, Cirrostratus

Page 14: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Clouds: Five Types of Clouds2. Mid-Level Clouds: Usually found between 6,500 and 20,000 ft.

Usually made of water droplets, but can be made of ice

Example is altocumulus

Page 15: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Clouds: Five Types of Clouds3. Low-Level Clouds: Usually found lower than 6,500 ft.

Low, lumpy clouds that produce weak to moderate precipitation

Examples include Nimbostratus and Stratocumulus

Page 16: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Clouds: Five Types of Clouds4. Vertically developed: These clouds are thick and puffy and extend very far upwards

Examples include Cumulonimbus and Fair Weather Cumulus

Ordinary Cumulus clouds can quickly become Cumulonimbus clouds that start strong thunderstorms

Page 17: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Clouds: Five Types of Clouds5. Other: These are miscellaneous clouds

These clouds do not really fit into any category, and all have different characteristics

Examples include billow clouds, contrails, mammatus, orographic, and pileus

Page 18: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Weather Maps: Pressure & Temperature

Page 19: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Weather Maps: Doppler Radar Maps

Page 20: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Summary Temperature: Usually in °F, need to convert to °C

High pressure areas cause sunny weather; low pressure areas cause rain and storms

Two Types of air masses:

1. Continental Polar

2. Maritime Tropical

Page 21: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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Summary (continued) Five types of fronts:

1. Cold2. Warm3. Stationary4. Occluded5. Dew Point (Dry Line)

Five types of clouds:1. High Level2. Mid Level3. Low Level4. Vertically developed5. Miscellaneous

Page 22: NSF North Mississippi GK-8 Weather! Matt Aufman NSF North Mississippi GK-8 November 2005

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SourcesPalmer, Chad and Evans, David. May 20, 2005. Occluded fronts can

signal weakening of storm. Accessed 28 October 2005. http://www.usatoday.com/weather/tg/wofront/wofront.htm

Palmer, Chad and Kepple, Kevin. May 20, 2005. High-pressure systems

brings sunny days. Accessed 27 October 2005.http://www.usatoday.com/weather/tg/whighp/whighp.htm

Palmer, Chad and Kepple, Kevin. May 20, 2005. How low pressure systems affect weather. Accessed 27 October 2005.

http://www.usatoday.com/weather/tg/wlowpres/wlowpres.htm

Weather World 2010, University of Illinois. No date of publicationgiven. Reading and Interpreting Weather Maps. Accessed

21 October 2005. http://ww2010.atmos.uiuc.edu/(Gh)/guides/maps/home.rxml