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Chapter 17 The Atmosphere: Structure and Temperature

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Chapter 17. The Atmosphere: Structure and Temperature. Section 17.3. Temperature Controls. Temperature Controls. Why Temperatures Vary Temperature is one of the basic elements of weather and climate. - PowerPoint PPT Presentation

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Page 1: Chapter 17

Chapter 17

The Atmosphere:Structure and Temperature

Page 2: Chapter 17

Section 17.3

Temperature Controls

Page 3: Chapter 17

Temperature Controls

Why Temperatures Vary• Temperature is one of the basic elements of

weather and climate.• A temperature control is any factor that

causes temperature to vary from place to place and from time to time.

• Factors that exert a strong influence on temperature are:– Latitude, heating of land and water, altitude,

geographic position, cloud cover, and ocean currents.

Page 4: Chapter 17

Temperature Controls

Why Temperatures Vary• Because variations in the angle of the sun’s

rays and length of daylight depend on latitude, they are responsible for warmer temperatures in the tropics and colder temperatures towards the poles.

• Seasonal temperature changes happen as the sun’s vertical rays move toward and away from a particular latitude during the year.

Page 5: Chapter 17

Question:Which of the following is NOT a factor that controls temperature?

A. LongitudeB. Cloud coverC. Ocean currentsD. Altitude

Page 6: Chapter 17

Temperature Controls

Land and Water• Land heats more rapidly and to higher temperatures

than water.• Land also cools more rapidly and to lower temperatures

than water.• Temperature variations are considerably greater over

land than over water.– Example: Vancouver has moderate temps compared to

Winnipeg due to the proximity to the Pacific Ocean. – Ex: Water accounts for 61% of the Northern Hemisphere

and land accounts for the remaining 39%. In the Southern Hemisphere, 81% of the surface is water and only 19% is land. The Southern Hemisphere shows smaller annual temperature variations.

Page 7: Chapter 17

Land & Water

Mean Monthly Temperatures for Vancouver and Winnipeg

Page 8: Chapter 17

Temperature Controls

Geographic Position• Geographic settings also play a large role in

temperature variations.– A coastal location where prevailing winds blow from the

ocean onto shore (windward coast) experience full moderating influence of the ocean – cool summers and mild winters.

– A coastal location where the prevailing winds blow from the land to the ocean (leeward coast) will have a more continental temperature pattern.

– Example: Eureka, CA is more moderate due to a windward coast compared to NY,NY that has more extreme temps due to the leeward coast.

Page 9: Chapter 17

Temperature Controls

Mean Monthly Temperatures for Eureka and New York City

Page 10: Chapter 17

Temperature Controls

Geographic Position• Mountain ranges also effect temperature

variations, as they act as barriers.– Mountain ranges cut off the moderating influence

of the oceans, thus making those on the windward side of the mountains have more of a marine influence and those on the leeward side a more continental influence.

– Example: Spokane has more extreme temp. than Seattle due to the Cascade Mts cutting off the influences of the Pacific Ocean.

Page 11: Chapter 17

Temperature Controls

Mean Monthly Temperatures for Seattle and Spokane

Page 12: Chapter 17

Temperature Controls

Altitude• Altitude is another temperature control. • The higher the altitude, the cooler the

temperatures.• The lower the altitude, the higher the

temperatures.• This is caused by having more or less

atmosphere.• Example: Quito, Ecuador is cooler than

Guayaquil due to its altitude.

Page 13: Chapter 17

Temperature Controls

Mean Monthly Temperatures for Guayaquil and Quito

Page 14: Chapter 17

Temperature Controls

Cloud Cover and Albedo• Cloud cover also greatly effects temperature.• Many clouds have a high albedo, and therefore reflect a

significant portion of the sunlight that strikes them back to space.– Albedo: The fraction of total radiation that is reflected by

any surface.• By reducing the amount of incoming solar radiation, the

maximum temperatures on a cloudy day will be lower than on a cloudless day.

• The opposite is true during the night where clouds act as a blanket by absorbing outgoing radiation emitted by the Earth and reradiating it back to the surface.

Page 15: Chapter 17

Temperature Controls

Clouds Reflect and Absorb Radiation

Page 16: Chapter 17

Question:Vancouver, British Columbia, enjoys a moderate year-round climate, which is due to

A. The many mountain ranges surrounding the city.

B. Its latitude.C. Its relatively high elevation.D. Its close proximity to the Pacific Ocean.

Page 17: Chapter 17

Question:The temperature differences seen between Seattle, Washington, and Spokane, Washington, illustrate the effect ofA. Cloud cover.B. Geographic position.C. Altitude.D. Ocean currents.

Page 18: Chapter 17

Question:The temperature differences between Quito, Ecuador, and Guayaquil, Ecuador, illustrate the effect of A. Cloud coverB. Geographic position.C. Altitude.D. Ocean currents.

Page 19: Chapter 17

Question:What causes clouds to reflect a portion of sunlight back to space?

A. The amount of oxygen in the atmosphereB. Evaporation from the landC. Temperature differences between the land

and the atmosphereD. A characteristic known as albedo

Page 20: Chapter 17

Question:Clouds absorb outgoing radiation emitted by Earth and reradiate a portion of it back to the surface during

A. Nighttime.B. Daytime.C. Summer.D. Times of heavy rainfall.

Page 21: Chapter 17

Temperature Controls

World Distribution of Temperature• Isotherms are lines that connect points that

have the same temperature.– From hot colors near the equator to cool colors

towards the poles.– Isotherms show a general trend of temperatures

of land and water, changes in latitude, and ocean currents.

– Isotherms generally trend east to west and show a decrease in temperatures from the tropics towards the poles.

Page 22: Chapter 17
Page 23: Chapter 17

Question:Which of the following is a general trend on a world isothermal map?

A. Temperatures decrease from east to west.B. Isotherms become wider closer to the poles.C. There are more isotherms closer to the

equator.D. Temperatures decrease from the tropics

toward the poles.