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Chapter 12.1. The causes of weather. Meteorology. Study of atmospheric phenomena Weather- day to day variations Climate- average weather over a long period of time. How is solar radiation is distributed around the planet? Sun feels hotter in the tropics. Why?

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Chapter 12 1

Chapter 12.1

The causes of weather


Meteorology
Meteorology

  • Study of atmospheric phenomena

  • Weather- day to day variations

  • Climate- average weather over a long period of time




Air masses
Air Masses Earth’s heat energy—the continual motion of air and water reallocates

  • Large body of air classified according to its source region

    • warm and dry continental tropical (cT)

    • warm and humid maritime tropical (mT)

    • cold and dry continental polar (cP)

    • cold and humid maritime polar (mP)

    • arctic (A)


Air mass modification
Air Mass Modification Earth’s heat energy—the continual motion of air and water reallocates

  • Heat transfers from one area to another establishing a heat balance.

  • As an air mass moves, it acquires some of the characteristics of the new surface beneath it.


Section assessment

The Causes of Weather Earth’s heat energy—the continual motion of air and water reallocates

Section Assessment

1. Match the following terms with their definitions.

___ meteorology

___ weather

___ climate

___ air mass

___ air mass modification

A. the current state of the atmosphere

B. the study of atmospheric phenomena

C. the average weather over a long period of time

D. the exchange of heat or moisture with the surface over which an air mass travels

E. a large body of air that takes on the characteristics of an area over which it forms

B

A

C

E

D


Section assessment1

The Causes of Weather Earth’s heat energy—the continual motion of air and water reallocates

Section Assessment

  • Identify the winter characteristics of each air mass.

    ___ A

    ___ cP

    ___ cT

    ___ mP

    ___ mT

A. warm, humid

B. bitter cold, dry

C. cold, humid

D. mild, humid

E. warm, dry

F. very cold, dry

B

F

E

C

A


Chapter 12 2

Chapter 12.2 Earth’s heat energy—the continual motion of air and water reallocates

Weather SYstems


Coriolis effect
Coriolis Earth’s heat energy—the continual motion of air and water reallocates Effect

  • Particles of air are deflected to the right in the N. hem. and to the left in the S hem. (due to Earth’s rotation)

  • The Coriolis effect & heat imbalances create distinct global wind systems that mix colder and warmer air masses.


Global wind systems
Global Wind Systems Earth’s heat energy—the continual motion of air and water reallocates

  • Trade winds- flow at 30° N and S latitude, where air sinks, warms, and returns to the equator in a westerly direction.


Other wind zones
Other Wind Zones Earth’s heat energy—the continual motion of air and water reallocates

  • The prevailing westerlies, the second major wind zone, flows between 30° and 60° N and S latitude in a circulation pattern opposite that of the trade winds. (US, Canada)

  • The polar easterlies, the third major wind zone, lies between 60° latitude and the poles. (cold)


Jet streams
Jet Streams Earth’s heat energy—the continual motion of air and water reallocates

  • Narrow bands of high-altitude, westerly winds that flow at speeds up to 185 km/h at high elevations of 10.7 km to 12.2 km.

  • They are the strongest core of westerly winds.

  • Weather systems generally follow the path of the jet streams.


Fronts
Fronts Earth’s heat energy—the continual motion of air and water reallocates

  • Narrow region separating two air masses of different densities that are caused by differences in temperature, pressure, and humidity.

  • Cause dramatic changes in weather.

  • 4 main types…


Cold fronts
Cold Fronts Earth’s heat energy—the continual motion of air and water reallocates

  • cold, dense air displaces warm air & forces the warm air to rise steeply

  • Cause clouds, showers, and sometimes thunderstorms

  • Ex: solid blue line with blue triangles that point in the direction of the front’s motion.


Warm fronts
Warm Fronts Earth’s heat energy—the continual motion of air and water reallocates

  • advancing warm air displaces cold air with a gradual frontal slope

  • characterized by lots of cloudiness & precipitation.

  • Ex: solid red line with red semicircles pointing in the direction of the front’s motion.


Stationary fronts
Stationary Fronts Earth’s heat energy—the continual motion of air and water reallocates

  • Two air masses meet and stall.

  • Seldom have extensive cloud & heavy precipitation patterns.

  • represented by a combination of short segments of cold- and warm-front symbols.


Occluded fronts
Occluded Fronts Earth’s heat energy—the continual motion of air and water reallocates

  • A cold air mass overtakes a warm front, wedging the warm air upward.

  • Precipitation is common on both sides of an occluded front.

  • Alternating purple triangles and semicircles that point toward the direction of motion.


Pressure systems
Pressure Systems Earth’s heat energy—the continual motion of air and water reallocates

  • At Earth’s surface, rising air is associated with low pressure and sinking air is associated with high pressure.

  • Rising or sinking air, combined with the Coriolis effect, results in the formation of rotating low- and high-pressure systems in the atmosphere.

  • Air in these systems moves in a general circular motion around either a high- or low-pressure center.


Pressure systems1
Pressure Systems Earth’s heat energy—the continual motion of air and water reallocates

High-Pressure Systems

  • In a high-pressure system, air sinks, so that when it reaches Earth’s surface it spreads away from the center.


Pressure systems2
Pressure Systems Earth’s heat energy—the continual motion of air and water reallocates

Low-Pressure Systems

  • In a low-pressure systems, air rises, causing an inward net flow toward the center and then upward.


Pressure systems3
Pressure Systems Earth’s heat energy—the continual motion of air and water reallocates

Low-Pressure Systems

  • A wave cyclone tends to produce inclement weather usually begins along a stationary front.

  • Parts of it move south as a cold front and north as a warm front in a counterclockwise or cyclonic circulation.


Section assessment2
Section Assessment Earth’s heat energy—the continual motion of air and water reallocates

1. Match the following terms with their definitions.

___ Coriolis effect

___ trade winds

___ jet streams

___ front

A. narrow bands of high-altitude, westerly winds that flow at high speeds

B. the narrow region separating two air masses of different densities

C. the major wind zones that occur at 30° north and south latitude

D. a result of Earth’s rotation that causes moving particles such as air to be deflected to the right in the northern hemisphere and to the left in the southern hemisphere

D

C

A

B


Section assessment3
Section Assessment Earth’s heat energy—the continual motion of air and water reallocates

2. Identify whether the following statements are true or false.

______ Low pressure systems are usually associated with fair weather.

______ A stationary front occurs when two air masses meet and stall.

______ In general, weather patterns follow the jet streams.

______ The overall circulation in a low-pressure system always rotates in a clockwise direction.

false

true

true

false


Chapter 12 3

Chapter 12.3 Earth’s heat energy—the continual motion of air and water reallocates

Gathering weather data


Gathering weather data
Gathering Weather Data Earth’s heat energy—the continual motion of air and water reallocates

  • Meteorologists measure temperature, air pressure, wind, & relative humidity to make weather forecasts.

  • Two of the most important factors in weather forecasting are the accuracy and frequency of the data.


Surface data
Surface Data Earth’s heat energy—the continual motion of air and water reallocates

  • Thermometer- measures temperature.

  • Barometer- measures air pressure.

  • Hygrometer (phsychrometer)- measures humidity

  • Anemometer- measures wind speed.

  • Ceilometer- measures height & amount of cloud cover


Upper level data
Upper-Level Data Earth’s heat energy—the continual motion of air and water reallocates

  • To make accurate forecasts, meteorologists must gather atmospheric data at heights of up to 30 000 m.

  • Radiosonde- sensorsattached to a weather balloon to measure upper level data and wind speeds.


Weather radar
Weather Radar Earth’s heat energy—the continual motion of air and water reallocates

  • A weather radar system is used to pinpoint where rain is falling.

  • The system transmits and displays electromagnetic waves that bounce, or scatter, off of large raindrops.


Doppler radar
Doppler Earth’s heat energy—the continual motion of air and water reallocates Radar

  • Doppler effect- the change in wave frequency that occurs in energy, such as sound or light, as that energy moves toward or away from an observer.

  • Meteorologists use Doppler radar estimate speed and direction of winds during storms including those that are experiencing severe weather such as thunderstorms and tornados.


Doppler effect
Doppler Effect Earth’s heat energy—the continual motion of air and water reallocates

As the train approaches, the sound waves ahead of it are compressed. These shorter waves have a high frequency, so the horn sounds high. Behind the train, the sound waves are stretched out. These longer waves have a lower frequency, so the horn sounds lower.


Weather satellites
Weather Satellites Earth’s heat energy—the continual motion of air and water reallocates

  • One of the main uses of satellites in orbit around Earth is to observe weather.

  • Cameras mounted aboard a weather satellite take photos of Earth at regular intervals.


Infrared imagery
Infrared Imagery Earth’s heat energy—the continual motion of air and water reallocates

  • Weather satellites use both visible light and invisible radiation to observe the atmosphere.

  • Infrared imagery detects differences in thermal energy

  • Because the strength of a storm is related to its height, infrared imagery can be used to establish a storm’s potential to produce severe weather.


Section assessment4

Gathering Weather Data Earth’s heat energy—the continual motion of air and water reallocates

Section Assessment

1. Match the following terms with their definitions.

___ thermometer

___ barometer

___ anemometer

___ hygrometer

___ ceilometer

A. an instrument that measures air pressure

B.an instrument that measures the height of cloud layers and estimates the amount of sky covered by clouds

C.an instrument that measures wind speed

D. an instrument that measures temperature

E. an instrument that measures relative humidity

D

A

C

E

B


Chapter 12 4

Chapter Earth’s heat energy—the continual motion of air and water reallocates 12.4

Weather analysis


Station model
Station Model Earth’s heat energy—the continual motion of air and water reallocates

  • a record of weather data for a particular site at a particular time.

  • Symbols are used to represent weather data in a station model.


Surface analysis
Surface Analysis Earth’s heat energy—the continual motion of air and water reallocates

  • To plot data nationwide or globally, meteorologists use isopleths.

  • Isopleths- lines that connect points of equal value, such as pressure or temperature.

  • Lines of equal pressure are called isobars.

  • Lines of equal temperature are called isotherms.


Surface analysis1
Surface Analysis Earth’s heat energy—the continual motion of air and water reallocates

  • You can tell how fast wind is blowing in an area by noting how closely isobars are spaced.

  • Isobars - close together indicate a large pressure difference over a small area = strong winds.

  • Isobars spread far apart indicate a small difference in pressure which equates to light winds.


Surface analysis2
Surface Analysis Earth’s heat energy—the continual motion of air and water reallocates

  • Isobars also indicate the locations of high- and low-pressure systems.

Of the states listed below, which is the windiest?

___ California

___ Texas

___ Missouri

___ South Carolina


Short term forecasts
Short-Term Forecasts Earth’s heat energy—the continual motion of air and water reallocates

  • Weather systems change directions, speed, and intensity with time in response to changes in the upper atmosphere.

  • A reliable forecast must analyze data from different levels in the atmosphere.

  • A digital forecast, most used today, is a forecast that relies on numerical data.


Short term forecasts1
Short-Term Forecasts Earth’s heat energy—the continual motion of air and water reallocates

  • An analog forecast involves comparing current weather patterns to patterns that took place in the past. Can you name an example?

    • Farmer’s Almanac


Long term forecasts
Long-Term Forecasts Earth’s heat energy—the continual motion of air and water reallocates

  • What do you notice about uncertainty as forecasts are made further in advance?


Things to remember about forecasts
Things to remember about forecasts… Earth’s heat energy—the continual motion of air and water reallocates

  • The most accurate and detailed forecasts are short-term in nature.

Less Accurate!

Forecasts in the one- to three-day range are the most accurate.

Accuracy Declines with Time!

More Accurate!


Don t blame the weatherman or woman
Don’t blame the weatherman! Earth’s heat energy—the continual motion of air and water reallocates (or woman)

  • Meteorologists rely on computer generated models to predict the weather. Sometimes they will have many different models with different predictions, which is where experience, training and their education come into play. It is an imperfect science, to say the least.


Section assessment5

Weather Analysis Earth’s heat energy—the continual motion of air and water reallocates

Section Assessment

1. Match the following terms with their definitions.

___ station model

___ isopleths

___ digital forecast

___ analog forecast

A. lines that connect points of equal or constant values

B. a forecast that relies on numerical data

C. a record of weather data for a particular site at a particular time

D. a forecast that involves comparing current weather patterns to patterns that took place in the past

C

A

B

D


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