chapter 24 table of contents section 1 air masses section 2 fronts

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WeatherChapter 24

Table of Contents

Section 1 Air Masses

Section 2 Fronts

Section 3 Weather Instruments

Section 4 Forecasting the Weather



Section 1 Air MassesChapter 24

Objectives

• Explain how an air mass forms.

• List the four main types of air masses.

• Describe how air masses affect the weather of North America.




Air Masses

• Differences in air pressure are caused by unequal heating of Earth’s surface.

• The region along the equator receives more solar energy than the regions at the poles do.

• Conversely, cold air near the pole sinks and creates high-pressure centers.

• Differences in air pressure at different locations on Earth create wind patterns.




How Air Moves• Air moves from areas of high pressure to areas of low

pressure. Therefore, there is a general, worldwide movement of surface air from the poles toward the equator.

• Temperature and pressure differences on Earth’s surface create three wind belts in the Northern Hemisphere and three wind belts in the Southern Hemisphere.

• The Coriolis effect, which occurs when winds are deflected by Earth’s rotation, also influences wind patterns.




Formation of Air Massesair mass a large body of air throughout which temperature

and moisture content are similar

• When air pressure differences are small, air remains relatively stationary.

• If air remains stationary or moves slowly over a uniform region, the air takes on characteristic temperature and humidity of that region.

• Air masses that form over frozen polar regions are very cold and dry. Air masses that form over tropical oceans are warm and moist.




Types of Air Masses• Air masses are classified according to their source

regions.

• The source regions for cold air masses are polar areas. The source regions for warm air masses are tropical areas.

• Air masses that form over the ocean are called maritime. Air masses that form over land are called continental.

• The combination of tropical or polar air and continental or maritime air results in air masses that have distinct characteristics.




Types of Air Masses, continued

Continental Air Masses

• There are two types of continental air masses: continental polar (cP) and continental tropical (cT).

• Continental polar air masses are cold and dry. Continental tropical air masses are warm and dry.

• An air mass may remain over its source region for days or weeks. However, the air mass will eventually move into other regions because of global wind patterns.




Types of Air Masses, continued

Maritime Air Masses

• When these very moist masses of air travel to a new location, they commonly bring more precipitation and fog.

• The two different maritime air masses are maritime polar (mP) and maritime tropical (mT).

• Maritime polar air masses are moist and cold. Maritime tropical air masses are moist and warm.




Types of Air Masses, continuedThe diagram below shows the four types of air mass that influence North

America.




North American Air Mass• The four types of air masses that affect the weather

of North America come from six regions.

• An air mass usually brings the weather of its source region, but an air mass may change as it moves away from its source region.

• For example, cold, dry air may become warm and more moist as it moves from land to the warm ocean.




North American Air Mass, continued

Tropical Air Mass

• Continental tropical air masses form over the deserts of the Southwestern United States.

• These air masses bring dry, hot weather in the summer. They do not form in the winter.

• Maritime tropical air masses form over the warm water of the tropical Atlantic Oceans.

• Maritime tropical air masses also form over the warm areas of the Pacific Oceans.




Reading Check

Which air mass brings dry, hot weather in the summer?




Reading Check

Which air mass brings dry, hot weather in the summer?

a continental tropical air mass





Polar Air Masses

• Polar air masses from three regions—northern Canada and the northern Pacific and Atlantic Oceans—influence weather in North America.

• In summer, the air masses usually bring cool, dry weather.

• In winter, they bring very cold weather to the northern United States.





Polar Air Masses, continued

• Maritime polar air masses form over the North Pacific Ocean and are very moist, but they are not as cold as continental polar Canadian air masses.

• In winter, these maritime polar Pacific air masses bring rain and snow to the Pacific Coast.

• In summer, they bring cool, often foggy weather.





Polar Air Masses, continued

• Maritime polar Atlantic air masses move generally eastward toward Europe. But they sometimes move westward over New England and eastern Canada.

• In winter, they can bring cold, cloudy weather and snow.

• In summer, these air masses can produce cool weather, low clouds, and fog.



Chapter 24

Air Masses

Section 1 Air Masses



Section 2 FrontsChapter 24

Objectives

• Compare the characteristic weather patterns of cold fronts with those of warm fronts.

• Describe how a midlatitude cyclone forms.

• Describe the development of hurricanes, thunderstorms, and tornadoes.




Fronts• A cool air mass is dense and does not mix with the

less-dense air of a warm air mass.

• Thus, a boundary, called a front, forms between air masses.

• Changes in middle-latitude weather usually take place along the various types of fronts.

• Fronts do not exist in the Tropics because no air masses that have significant temperature differences exist there.




Fronts, continued

Cold Fronts

cold front the front edge of a moving mass of cold air that pushes beneath a warmer air mass like a wedge

• If the warm air is moist, clouds will form.




Fronts, continued

Cold Fronts, continued

• Large cumulus and cumulonimbus clouds typically form along fast-moving cold fronts.

• A long line of heavy thunderstorms, called a squall line, may occur in the warm, moist air just ahead of a fast-moving cold front.

• A slow-moving cloud front typically produces weaker storms and lighter precipitation than a fast-moving cold front does.




Fronts, continued

Warm Fronts

warm front the front edge of advancing warm air mass that replaces colder air with warmer air

• The slope of a warm front is gradual.

• Because of this gentle slope, clouds may extend far ahead of the surface location, or base, of the front.

• A warm front generally produces precipitation over a large area and may cause violent weather.




Fronts, continued

Stationary and Occluded Fronts

stationary front a front of air masses that moves either very slowly or not at all

occluded front a front that forms when a cold air mass overtakes a warm air mass and lifts the warm air mass of the ground and over another air mass

• Sometimes, when air masses meet, the cold moves parallel to the front, and neither air mass is displaced.




Polar Fronts and Midlatitudes Cyclones• Over each of Earth’s polar regions is a dome of cold

air that may extend as far as 60° latitude.

• The boundary where this cold polar air meets the tropical air mass of the middle latitudes, especially over the ocean, is called the polar front.

• Waves commonly develop along the polar front.

• A waves is a bend that forms in a cold front or stationary front.




Polar Fronts and Midlatitudes Cyclones, continued

midlatitude cyclone an area of low pressure that is characterized by rotating wind that moves toward the rising air of the central low-pressure region

• Waves are the beginnings of low-pressure storm centers called midlatitude cyclones or wave cyclones.

• These cyclones strongly influence weather patterns in the middle latitudes.




Polar Fronts and Midlatitudes Cyclones, continued

Stages of a Midlatitude Cyclones

• A midlatitude cyclone usually last several days.

• In North America, midlatitude cyclones generally travel about 45 km/h in an easterly direction as they spin counterclockwise.

• They follow several storm tracks, or routes, as they move from the Pacific coast to the Atlantic coast.



Section 2 FrontsChapter 24Polar Fronts and Midlatitudes Cyclones, continuedThe diagram below shows the different stages of a midlatitude cyclone.



Section 2 FrontsChapter 24Polar Fronts and Midlatitudes Cyclones, continuedAnticyclones

• Unlike the air in the midlatitude cyclone, the air of an anticyclone sinks and flows outward from a center of high pressure.

• Because of the Coriolis effect, the circulation of air around an anticyclone is clockwise in the Northern Hemisphere.

• Anticyclones bring dry weather, because their sinking air does not promote cloud formation.




Reading Check

How is the air of an anticyclone different from that of a midlatitude cyclone?




Reading Check

How is the air of an anticyclone different from that of a midlatitude cyclone?

The air of an anticyclone sinks and flows outward from a center of high pressure. The air of a midlatitude cyclone rotates toward the rising air of a central, low-pressure region.




Severe Weather

Thunderstorms

thunderstorm a usually brief, heavy storm that consists of rain, strong winds, lightning, and thunder

• Thunderstorms develop in three distinct stages.

• The thunderstorm dissipates as the supply of water vapor decrease.




Severe Weather, continued

Lightning

• During a thunderstorm, clouds discharge electricity in the form of lightning.

• The released electricity heats the air, and the air rapidly expands and produces a loud noise known as thunder.

• For lightning to occur, the clouds must have areas that carry distinct electrical charges.





Hurricanes

hurricane a severe storm that develops over tropical oceans and whose strong winds of more than 120 km/h spiral in toward the intensely low-pressure storm center

• A hurricane begins when warm, moist air over the ocean rises rapidly.

• When moisture in the rising warm air condenses, a large amount of energy in the from of latent heat is released. This heat increase the force of the rising air.





Hurricanes, continued

• A fully developed hurricane consists of a series of thick cumulonimbus cloud bands that spiral upward around the center of the storm.

• The most dangerous aspect of a hurricane is a rising sea level and large waves, called a storm surge.

• Every hurricane is categorized on the Safir-Simpson scale by using several factors. These factors include central pressure, wind speed, and storm surge.




Reading Check

Where do hurricanes develop?




Reading Check

Where do hurricanes develop?

over warm tropical seas





Tornadoes

tornado a destructive, rotating column of air that has very high wind speeds and that maybe visible as a funnel-shaped cloud

• The smallest, most violent, and shortest-lived severe storm is a tornado.

• A tornado forms when a thunderstorm meets high-altitude horizontal winds. These winds cause the rising air in the thunderstorm to rotate.





Tornadoes, continued

• A storm cloud may develop a narrow, funnel-shaped rapidly spinning extension that reaches downward and may or may not touch the ground.

• If the funnel does touch the ground, it generally moves in a wandering, haphazard path.

• The destructive power of a tornado is due to mainly the speed of the winds. These winds may reach speeds of more than 400 km/h.



Chapter 24

Types of Fronts

Section 2 Fronts



Section 3 Weather InstrumentsChapter 24

Objectives

• Identify four instruments that measure lower-atmospheric weather conditions.

• Describe how scientists measure conditions in the upper atmosphere.

• Explain how computers help scientists understand weather.




Measuring Lower-Atmospheric ConditionsAir Temperature

thermometer an instrument that measures and indicates temperature

• A common type of thermometer uses a liquid—usually mercury or alcohol—sealed in a glass tube to indicate temperature.

• A rise in temperature causes the liquid to expand and fill more of the tube. A drop in temperature causes the liquid to contract and fill less of the tube.




Measuring Lower-Atmospheric Conditions, continuedAir Temperature, continued

• Another type of thermometer is an electrical thermometer.

• As the temperature rises, the electric current that flows through the material of the electrical thermometer increases and is translated into temperature readings.

• A thermistor, or thermal resistor, is a type of electrical thermometer that responds very quickly to temperature changes.




Measuring Lower-Atmospheric Conditions, continuedAir Pressure

barometer an instrument that measures atmospheric pressure

• Changes in air pressure affect air masses.

• The approach of a front is usually indicated by a drop in air pressure.




Measuring Lower-Atmospheric Conditions, continuedWind Speed

anemometer an instrument used to measure wind speed

• A typical anemometer consists of small cups that are attached by spokes to a shaft that rotates freely.

• The wind pushes against the cup and causes them to rotate. This rotation triggers an electrical signal that registers the wind speed in meters per second or in miles per hour.




Measuring Lower-Atmospheric Conditions, continuedWind Direction

wind vane an instrument used to determine direction of the wind

• The wind vane is commonly an arrow-shaped device that turns freely on a pole as the tail catches the wind.

• Wind direction may be described by using one of 16 compass directions, such as north-northeast. Wind direction also may be recorded in degrees by moving clockwise and beginning with 0° at the north.




Reading Check

Which instrument is used to measure air pressure?




Reading Check

Which instrument is used to measure air pressure?

A barometer is used to measure atmospheric pressure.




Measuring Upper-Atmospheric ConditionsRadiosonde

radiosonde a package of instruments that is carried aloft by balloons to measure upper atmospheric conditions, including temperature, dew point, and wind velocity

• The radiosonde sends measurements as radio waves to a receiver that records the information.

• When the balloon reaches a very high altitude, the balloon expands and bursts, and the radiosonde parachutes back to Earth.



Section 3 Weather InstrumentsChapter 24Measuring Upper-Atmospheric Conditions, continuedRadar

radar radio detection and ranging, a system that uses reflected radio waves to determine the velocity and location of objects

• For example, large particles of water in the atmosphere reflect radar pulses.

• The newest Doppler radar can indicate the precise location, movement,and extent of a storm. It can also indicate the intensity of precipitation and wind patterns within a storm.



Section 3 Weather InstrumentsChapter 24Measuring Upper-Atmospheric Conditions, continuedWeather Satellites

• Satellite images provide weather information for regions where observations cannot be made from ground.

• The direction and speed of the wind at the level of the clouds can also be measured by examining a continuous sequence of cloud images.

• Satellite instruments can also measure marine conditions.



Section 3 Weather InstrumentsChapter 24Measuring Upper-Atmospheric Conditions, continuedComputers

• Before computers were available, solving the mathematical equations that describe the behavior of the atmosphere was very difficult, and sometimes impossible.

• In addition to solving many of these equations, computers can store weather data from around the world. These data can provide information that is useful in forecasting weather changes.



Section 4 Forecasting the WeatherChapter 24

Objectives

• Explain how weather stations communicate weather data.

• Explain how a weather map is created.

• Explain how computer models help meteorologists forecast weather.

• List three types of weather that meteorologists have attempted to control.



Chapter 24

Global Weather Monitoring

• Weather stations around the world exchange the weather information they have collected.

• The World Meteorological Organization (WMO) sponsors a program called World Weather Watch to promote the rapid exchange of weather information.

• It also offers advice on the effect of weather on natural resource and on human activities, such as farming and transportation.




Interactive weather map

• http://www.wunderground.com/wundermap/

http://www.edheads.org/activities/weather/



Chapter 24

Weather MapsWeather Symbols

station model a pattern of meteorological symbols that represent the weather at a particular observing station and that is recorded on a weather map

• Common weather symbols describe cloud cover, wind speed, wind direction, and weather conditions, such as type of precipitation and storm activity.




Chapter 24

Weather Maps, continued

Weather Symbols, continued

• Other information included in the station model are the air temperature and the dew point.

• The dew point indicates how high the humidity of the air is, or how much water is in the air.

• The station model also indicates the atmospheric pressure by using a three-digit number in the upper right hand corner.




Chapter 24

Weather Maps, continuedThe diagram below shows the different weather symbols used on weather

maps.




Chapter 24


Plotting Temperature and Pressure

• Lines that connect points of equal temperatures are called isotherms.

• Lines that connect points of equal atmospheric pressure are called isobars.

• The spacing and shape of the isobars help meteorologists interpret their observations about the speed and direction of the wind.




Chapter 24


Plotting Fronts and Precipitation

• Most weather maps mark the locations of fronts and areas of precipitation.

• Fronts are identified by sharp changes in wind speed and direction, temperature or humidity.

• Areas of precipitation are commonly marked by using colors or symbols.




Chapter 24

Weather Maps, continuedThe diagram below shows an example of a typical weather map.




Chapter 24

Reading Check

How do meteorologists mark precipitation on a weather map?




Chapter 24

Reading Check

How do meteorologists mark precipitation on a weather map?

Areas of precipitation are marked by using colors or symbols.




Chapter 24

Weather Forecasts

• To forecast the weather, meteorologists regularly plot to the intensity and path of weather systems on maps.

• Meteorologists then study the must recent weather map and compare it with maps from previous hours.

• By following the progress of weather systems, meteorologist can forecast the weather.




Chapter 24

Weather Forecasts, continued

Weather Data

• Computers models can show the possible weather conditions for several days.

• Comparing models helps meteorologists better predict weather.

• By using computers, scientists can manipulate data on temperature and pressure to simulate errors in measuring these data.




Chapter 24

Reading Check

Why do meteorologists compare models.




Chapter 24

Reading Check

Why do meteorologists compare models.

Meteorologists compare computer models because different models are better at predicting different weather variables. If information from two or more models matches, scientists can be more confident of their predictions.




Chapter 24


Types of Forecasts

• Meteorologists make four types of forecasts.

• Daily forecasts predict weather conditions for a 48-hour period. Extended forecasts look ahead 3 to 7 days. Medium range forecasts look ahead 8 to 14 days. Long-range forecasts cover monthly and seasonal periods.

• Accurate weather forecasts can be made for 0 to 7 days. However, accuracy decreases with each day.




Chapter 24


Severe Weather Watches and Warnings

• One main goal of meteorology is to reduce the amount of destruction caused by severe weather by forecasting severe weather early.

• A watch is issued when the conditions are ideal for severe weather.

• A warning is given when severe weather has been spotted or is expected within 24 hours.




Chapter 24

Controlling the Weather

• Some meteorologists are investigating methods of controlling rain, hail, and lightning.

• Currently, the most researched method for producing rain has been cloud seeding.

• Cloud seeding can also be used to prevent more severe precipitation.




Chapter 24

Controlling the Weather, continued

Hurricane Control

• Hurricanes have also been seeded with freezing nuclei in an effort to reduce the intensity of the storm.

• During Project Stormfury, which took place from 1962 to 1983, four hurricanes were seeded, and the project had mixed results.

• Scientists have, for the most part, abandoned storm and hurricane control because it is not an attainable goal with existing technology.




Chapter 24

Controlling the Weather, continued

Lightning Control

• Seeding of potential lightning storms with silver-iodide nuclei has seemed to modify the occurrence of lighting.

• However, no conclusive results have been obtained.




Maps in ActionChapter 24

Maps in ActionWeather-Related Disasters, 1980–2003



Multiple Choice

1. What tool do meteorologists use to analyze particle movements within storms?

A. an anemometerB. a radiosonde balloonC. doppler radarD. satellite imaging

Standardized Test PrepChapter 24



Multiple Choice, continued

1. What tool do meteorologists use to analyze particle movements within storms?

A. an anemometerB. a radiosonde balloonC. doppler radarD. satellite imaging





2. What kind of front forms when two air masses move parallel to the boundary located between them?

F. an occluded frontG. a polar frontH. a warm frontI. a stationary front





3. Which of the following weather systems commonly forms over warm tropical oceans?

A. thunderstormsB. hurricanesC. tornadoesD. anticyclones





4. What often happens to maritime air masses as they move inland over mountainous country?

F. They bring warm, dry weather conditions.G. They produce clouds and hurricanes.H. They bring cold, dry weather conditions.I. They lose moisture passing over mountains.





5. What type of air mass originates over the south- weathern desert of the United States in summer?

A. continental polar air massB. continental tropical air massC. maritime polar air massD. maritime tropical air mass




Short Response

6. What type of front is formed when a warm air mass is overtaken by a cold air mass, which causes the warm air to lift above the cold air?




Short Response, continued

6. What type of front is formed when a warm air mass is overtaken by a cold air mass, which causes the warm air to lift above the cold air?

Cold front





7. What do closely spaced isobars indicate about the wind on a weather map?





7. What do closely spaced isobars indicate about the wind on a weather map?

high-speed winds




Interpreting Graphics

Use the diagram below to answer questions 11 and 12. The diagram shows a station model.




Interpreting Graphics, continued

11. What letter represents the current barometric reading shown in the model?

A. letter AB. letter BC. letter CD. letter D






11. What letter represents the current barometric reading shown in the model?

A. letter AB. letter BC. letter CD. letter D




12.What weather information do the symbols indicated by the letters E and F provide? Interpret this part of the station model.





12.What weather information do the symbols indicated by the letters E and F provide? Interpret this part of the station model.

E is wind direction, and F is wind speed. Currently, the station model is showing a 30-knot wind that is blowing in from south.





Use the diagram below to answer questions 13 and 14. The diagram shows a home weather station.





13.Which of the following weather instruments shown uses the cooling effect of evaporation to take measurements.

A. a rain gaugeB. a psychrometerC. a wind sockD. a thermometer





14.Describe how an anemometer is used to calculate wind speed.





14.Describe how an anemometer is used to calculate wind speed.

Answers should include: as the cups on the anemometer catch the wind, the device begins to rotate; the speed of this rotation, usually given in revolutions per minute, and the circumference of the circle made by the cups are used to calculate wind speed; rudimentary devices rely on the user to count the revolutions per minute of the device and to perform the necessary math to determine the wind speed; in modern computerized devices, a number of factors may be considered to obtain the most accurate measurement possible, including the circumference of the device, friction of the air, and drag.




Air Masses

Chapter 24



Stages of a Midlatitude Cyclone

Chapter 24



Weather Symbols

Chapter 24



Weather Map of the United States

Chapter 24



Weather-Related Disasters, 1980-2003

Chapter 24

chapter 24 table of contents section 1 air masses section 2 fronts

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