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Temperature Controls
By: Hannah Barber
Vocabulary:
• Albedo- The fraction of total radiation that is
reflected by any surface.
• Isotherm- Lines that connect points that have
the same temperature.
Key terms:
• Factors other than latitude that exert a strong
influence on temperature include heating of land and
water, altitude geographic position, cloud cover, and
ocean currents.
• Land heats more rapidly and to higher temperatures
than water. Land also cools more rapidly and to
lower temperatures than water.
• Many clouds have a high albedo, and therefore
reflect a significant portion of the sunlight that
strikes them back to space.
Temperature:
• Temperature is one of the basic elements of
weather and climate. There are many
instruments that help you determine the
temperature and many ways to describe the
temperature.
Why temperatures vary:
• A temperature control is any factor that
causes temperature to vary from place to
place and from time to time.
• Seasonal temperature changes happen as the
sun’s vertical rays move toward and away
from a particular latitude during the year.
Land and water:
• The largest contrast of temperature is
between land and water. The temperature
variations are considerably greater over land
than over water.
• In the Northern Hemisphere, the water
accounts are 61% water and 39% land.
• In the Southern Hemisphere, the water
accounts are 81% and 19% land.
Geographic Position:
• The geographic setting can greatly influence
temperatures experienced at a specific
location.
Altitude:
• As you go up in altitude, the temperature
decreases but as you go down in altitude the
temperature will increase.
Cloud Cover and Albedo:
• The extent of cloud cover is a factor that influences
temperatures in the lower atmosphere. By reducing the
amount of incoming solar radiation, the maximum
temperatures on a cloud-covered day will be lower than on a
day when clouds are absent and the sky is clear.
• At night, clouds have the opposite effect. Clouds act as a
blanket by absorbing outgoing radiation emitted by Earth and
reradiating a portion of it back to the surface.
World Distribution of Temperature
• Near the equator is where temperatures are
hotter and near the poles is where the
temperatures are cooler.
• Latitude controls on incoming solar radiation,
which in turn heats Earth’s surface and the
atmosphere above it.

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Temperature controls

  • 2. Vocabulary: • Albedo- The fraction of total radiation that is reflected by any surface. • Isotherm- Lines that connect points that have the same temperature.
  • 3. Key terms: • Factors other than latitude that exert a strong influence on temperature include heating of land and water, altitude geographic position, cloud cover, and ocean currents. • Land heats more rapidly and to higher temperatures than water. Land also cools more rapidly and to lower temperatures than water. • Many clouds have a high albedo, and therefore reflect a significant portion of the sunlight that strikes them back to space.
  • 4. Temperature: • Temperature is one of the basic elements of weather and climate. There are many instruments that help you determine the temperature and many ways to describe the temperature.
  • 5. Why temperatures vary: • A temperature control is any factor that causes temperature to vary from place to place and from time to time. • Seasonal temperature changes happen as the sun’s vertical rays move toward and away from a particular latitude during the year.
  • 6. Land and water: • The largest contrast of temperature is between land and water. The temperature variations are considerably greater over land than over water. • In the Northern Hemisphere, the water accounts are 61% water and 39% land. • In the Southern Hemisphere, the water accounts are 81% and 19% land.
  • 7. Geographic Position: • The geographic setting can greatly influence temperatures experienced at a specific location.
  • 8. Altitude: • As you go up in altitude, the temperature decreases but as you go down in altitude the temperature will increase.
  • 9. Cloud Cover and Albedo: • The extent of cloud cover is a factor that influences temperatures in the lower atmosphere. By reducing the amount of incoming solar radiation, the maximum temperatures on a cloud-covered day will be lower than on a day when clouds are absent and the sky is clear. • At night, clouds have the opposite effect. Clouds act as a blanket by absorbing outgoing radiation emitted by Earth and reradiating a portion of it back to the surface.
  • 10. World Distribution of Temperature • Near the equator is where temperatures are hotter and near the poles is where the temperatures are cooler. • Latitude controls on incoming solar radiation, which in turn heats Earth’s surface and the atmosphere above it.