Chapter 12.1 Meteorology Study of atmospheric phenomena Weather- day to day variations Climate-...

45
THE CAUSES OF WEATHER Chapter 12.1
  • date post

    19-Dec-2015
  • Category

    Documents

  • view

    220
  • download

    3

Transcript of Chapter 12.1 Meteorology Study of atmospheric phenomena Weather- day to day variations Climate-...

Page 1: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

THE CAUSES OF WEATHER

Chapter 12.1

Page 2: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Meteorology

Study of atmospheric phenomena

Weather- day to day variations

Climate- average weather over a long period of time

Page 3: Chapter 12.1 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?• Because the Sun’s rays are more

spread out when they strike Earth at a low angle, the same amount of energy is spread over a larger area

Page 4: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

All weather is part of a constant redistribution of Earth’s heat energy—the continual motion of air and water reallocates

Heat energy among Earth’s surface, oceans, and atmosphere and balances it

Page 5: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Air Masses 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)

Page 6: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Air Mass Modification– 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.

Page 7: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Section Assessment1. Match the following terms with their definitions.

___ meteorology

___ weather

___ climate

___ air mass

___ air mass

modification

The Causes of Weather

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

Page 8: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Section Assessment2. Identify the winter characteristics of

each air mass.

___ A

___ cP

___ cT

___ mP

___ mT

The Causes of Weather

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

Page 9: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

WEATHER SYSTEMS

Chapter 12.2

Page 10: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Coriolis Effect

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

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)

Page 11: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Global Wind Systems

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

Page 12: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Other Wind Zones

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)

Page 13: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Jet Streams 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.

Page 14: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Fronts

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…

Page 15: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Cold Fronts– 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.

Page 16: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Warm Fronts– 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.

Page 17: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Stationary Fronts– 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.

Page 18: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Occluded Fronts– 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.

Page 19: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Pressure Systems 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.

Page 20: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Pressure SystemsHigh-Pressure Systems

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

Page 21: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Pressure SystemsLow-Pressure Systems

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

Page 22: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Pressure SystemsLow-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.

Page 23: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Section Assessment1. 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

Page 24: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Section Assessment2. 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

Page 25: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

GATHERING WEATHER DATA

Chapter 12.3

Page 26: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Gathering Weather Data 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.

Page 27: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Surface Data• Thermometer- measures temperature. • Barometer- measures air pressure.

• Hygrometer (phsychrometer)- measures humidity

• Anemometer- measures wind speed.

• Ceilometer- measures height & amount of cloud cover

Page 28: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Upper-Level Data To make accurate forecasts, meteorologists must

gather atmospheric data at heights of up to 30 000 m.

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

Page 29: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Weather Radar 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.

Page 30: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Doppler 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.

Page 31: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Doppler EffectAs 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.

Page 32: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Weather Satellites 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.

Page 33: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Infrared Imagery– 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.

Page 34: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Section Assessment1. Match the following terms with their

definitions.___ thermometer

___ barometer

___ anemometer

___ hygrometer

___ ceilometer

Gathering Weather Data

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

Page 35: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

WEATHER ANALYSIS

Chapter 12.4

Page 36: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Station Model a record of weather data for a particular site at a

particular time.

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

Page 37: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Surface Analysis 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.

Page 38: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Surface Analysis

• 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.

Page 39: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Surface Analysis 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

Page 40: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Short-Term Forecasts 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.

Page 41: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Short-Term Forecasts• An analog forecast involves comparing current

weather patterns to patterns that took place in the past. Can you name an example?

• Farmer’s Almanac

Page 42: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Long-Term Forecasts What do you notice about uncertainty as

forecasts are made further in advance?

Page 43: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Things to remember about forecasts… The most accurate and detailed forecasts are

short-term in nature.

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

Accuracy Declines with Time!

Less Accurate!More

Accurate!

Page 44: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Don’t blame the weatherman! (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.

Page 45: Chapter 12.1 Meteorology  Study of atmospheric phenomena  Weather- day to day variations  Climate- average weather over a long period of time.

Section Assessment1. Match the following terms with their

definitions.___ station model

___ isopleths

___ digital forecast

___ analog forecast

Weather Analysis

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