meteorology 12.1 the causes of weather. weather meteorology is the study of atmospheric phenomena...
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Meteorology
12.1 The Causes of Weather12.1 The Causes of Weather
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Weather
MeteorologyMeteorology is the study of atmospheric is the study of atmospheric phenomenaphenomena
WeatherWeather is the current state of the is the current state of the atmosphere. atmosphere. This is usually measured in minutes, days This is usually measured in minutes, days
and weeksand weeks
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Climate ClimateClimate is the weather is the weather
for a long period of time for a long period of time for a given location.for a given location.
Usually averaged over Usually averaged over 30 or more years. 30 or more years.
Ex. Ex. The climate is hot The climate is hot and humid in Miami, but and humid in Miami, but it is snowing there todayit is snowing there today..
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Air Masses
An An air massair mass is a large is a large body of air that takes body of air that takes on the characteristics on the characteristics of the area over which of the area over which it forms.it forms.
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Types of Air Masses
MoistureMoisture Maritime vs. Maritime vs.
Continental:Continental: Maritime air masses Maritime air masses
form over water- form over water- have more moisturehave more moisture
Continental air Continental air masses form over masses form over land- they are drierland- they are drier
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Types of Air Masses TemperatureTemperature Tropical vs. PolarTropical vs. Polar
Tropical air masses Tropical air masses form closer to the form closer to the equator- warmequator- warm
Polar air masses Polar air masses form closer to the form closer to the poles- coldpoles- cold
Arctic air masses are Arctic air masses are extremely coldextremely cold
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Source Regions
Combine Moisture and Temperature titles Combine Moisture and Temperature titles to name air masses. to name air masses. Name them after the regions where they Name them after the regions where they
form.form. Continental Tropical(cT) will form over Continental Tropical(cT) will form over
land near the equator. Ex. Brazil, Mexicoland near the equator. Ex. Brazil, Mexico Maritime Tropical(cM) will form over Maritime Tropical(cM) will form over
water near the equator. Ex. Gulf of Mexicowater near the equator. Ex. Gulf of Mexico
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Examples:
Continental Polar(cP)Continental Polar(cP) Continental Tropical(cT)Continental Tropical(cT) Maritime Polar(mP)Maritime Polar(mP) Maritime Tropical(mT)Maritime Tropical(mT) Arctic(A)Arctic(A)
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Coriolis Effect The Earth spins on its axis. This causes air The Earth spins on its axis. This causes air
particles to deflect to the left in the N. particles to deflect to the left in the N. Hemisphere & to the right in the S. Hemisphere & to the right in the S. HemisphereHemisphere
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RR
L
L
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Wind Systems Three wind Three wind
zones in each zones in each HemisphereHemisphere Trade Trade
WindsWinds Prevailing Prevailing
WesterliesWesterlies Polar Polar
EasterliesEasterlies
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Wind Zones•The trade winds occur from the equator to 30ºN and 30ºS. The winds at the equator are called the doldrums and the ones at the 30º mark are called the horse latitudes.
•The prevailing westerlies are between 30ºN and S up to 60ºN and S in a pattern opposite of the trade winds. They are responsible for moving most weather across the US and Canada.
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•The polar easterlies are between 60ºN and S and the poles. (90ºN and S)
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Jet Stream A stream of air A stream of air
that circulates the that circulates the globe. Caused by globe. Caused by differences in differences in pressure between pressure between the wind systems. the wind systems. Trade and Trade and
WesterliesWesterlies Westerlies and Westerlies and
EasterliesEasterlies
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Fronts A A frontfront is the narrow region is the narrow region
separating two air masses of separating two air masses of different densities. These different densities. These differences are due to differences are due to differences in temperature, differences in temperature, humidity, and pressure. humidity, and pressure. ColdCold WarmWarm StationaryStationary OccludedOccluded
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Cold Front – Cold dense air displaces warm air and forces the warm air up along a steep front
-Thunderstorms often occur along the front
Page 308- 309 in RED BOOK!
On a weather map: solid blue line with blue triangles that point in direction of the front’s motion
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Cold Fronts Cold Fronts occur when a cold air mass Cold Fronts occur when a cold air mass
runs into a warm air mass, forcing the warm runs into a warm air mass, forcing the warm mass to rise.(notice cloud types!)mass to rise.(notice cloud types!)
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Warm Front – Advancing warm air displaces cold air
- Extensive cloudiness and precipitation
On a map: solid red line with regularly spaced, solid red semicircles pointing in the direction of the front's motion.
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Warm Fronts When warm masses run into cold masses When warm masses run into cold masses
and slowly displaces it. (notice clouds!)and slowly displaces it. (notice clouds!)
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Stationary Front – Two air masses meet and neither advances; air masses “stall”
- Light wind and precipitation
On a map: combination of short segments of cold and warm front symbols
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Stationary Fronts Stationary Fronts occur when front run in Stationary Fronts occur when front run in
parallel opposite directionsparallel opposite directions
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Occluded Front – Cold air mass moves so rapidly that it overtakes a warm front
- Strong winds, heavy precipitation
On a map: alternating purple triangles and semicircles that point toward the direction of motion.
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Occluded Occluded Fronts occur when two cold Occluded Fronts occur when two cold
fronts “pinch” a warm front up. fronts “pinch” a warm front up.
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Front Video
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High Pressure Systems High Pressure Systems- High Pressure Systems-
Air sinks, then hits the Air sinks, then hits the Earth’s surface and Earth’s surface and spreads out. spreads out. Wind blows away from Wind blows away from
high pressure.high pressure. Clockwise in N. Clockwise in N.
HemisphereHemisphere Associated with fair Associated with fair
weatherweather
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Low Pressure System
Low Pressure System- Air rises, must be Low Pressure System- Air rises, must be replaced.replaced. Wind blows toward center of low Wind blows toward center of low
pressurepressure Counter-Clockwise in N. HemisphereCounter-Clockwise in N. Hemisphere Associated with clouds and precipitationAssociated with clouds and precipitation
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