Meteorology Today 11th Edition by C. Donald Ahrens – Test Bank

 

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Sample Test

Chapter_03_Seasonal_and_Daily_Temperatures

 

 

1. ​During an equinox, the days and nights are of equal length except at the poles.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

2. ​The winter solstice marks the shortest night of the year in the Northern Hemisphere.

 

a.

True

 

b.

False

 

ANSWER:  

False

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

3. ​The north-facing side of a hill in a mountainous region in the U.S. tends to be a better location for a ski run than the south-facing side.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

4. ​During a radiation inversion, wind machines can lift cool surface air to higher altitudes.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

5. ​Incoming solar radiation in middle latitudes is less in winter than in summer because the Sun’s rays slant more and spread their energy over a larger area.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

6. ​Water warms and cools much more slowly than land, because it takes more heat to raise the temperature of a given amount of soil 1°C than it does to raise the temperature of water 1°C.

 

a.

True

 

b.

False

 

ANSWER:  

False

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.7 – Summarize the relationship between latitude, land and water distribution, ocean currents, and elevation on the daily and regional temperature variations observed on Earth.

OTHER:  

Bloom’s: Understand

 

7. ​During summer near the North Pole, the Sun is above the horizon a shorter period of time than in the mid-latitudes.

 

a.

True

 

b.

False

 

ANSWER:  

False

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

8. ​In the Northern Hemisphere, summers are warmer than winters, even though Earth is actually closer to the Sun in January.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

9. ​If two cities have the same mean annual temperature, it means that their temperatures throughout the year are always similar.

 

a.

True

 

b.

False

 

ANSWER:  

False

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

10. ​Each day past the winter solstice the noon Sun is a little higher above the southern horizon.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

11. ​In the Northern Hemisphere, south-facing mountain slopes normally have a smaller diurnal range in temperature than north-facing slopes.

 

a.

True

 

b.

False

 

ANSWER:  

False

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

12. ​Even though the poles have 24 hours of sunlight during the summer, the average summer temperature there is nonetheless below 0°F.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

13. ​If clouds arrive at 2 a.m. in the middle of a calm, clear night, it is quite common to see temperatures rise after 2 a.m.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.7 – Summarize the relationship between latitude, land and water distribution, ocean currents, and elevation on the daily and regional temperature variations observed on Earth.

OTHER:  

Bloom’s: Understand

 

14. ​If you are a household gardener concerned about outside flowers and plants during cold weather, you can simply wrap them in plastic or cover each with a paper cup to protect them.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

15. ​The combination of heating and cooling degree days gives a practical indication of the energy requirements over the year.

 

a.

True

 

b.

False

 

ANSWER:  

True

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

16. ​Corn varieties are typically rated in terms of “days to maturity”. The reason this system works well is that corn always takes the same number of days to mature, independent of the growing location.

 

a.

True

 

b.

False

 

ANSWER:  

False

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

17. ​Cold, rainy days often feel warmer than dry days because air conducts heat away from the body better than water.

 

a.

True

 

b.

False

 

ANSWER:  

False

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.9 – Analyze why temperatures can “feel” differently on different occasions, i.e., in different geographical locations, on different days, and during different parts of the day, and describe the potential effects of extreme hot and cold temperatures on human health.

OTHER:  

Bloom’s: Analyze

 

18. ​In the Northern Hemisphere, which day has the fewest hours of daylight?

 

a.

​summer solstice

 

b.

​winter solstice

 

c.

​vernal equinox

 

d.

​autumnal equinox

 

e.

​spring solstice

 

ANSWER:  

b

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

19. ​Which latitude below would experience the fewest hours of daylight on December 22nd?

 

a.

​60°S

 

b.

​20°S

 

c.

​0°(Equator)

 

d.

​20°N

 

e.

​60°N

 

ANSWER:  

e

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

20. ​The Sun is directly overhead at Mexico City (latitude 19°N)

 

a.

​once a year.

 

b.

​twice a year.

 

c.

​four times a year.

 

d.

​never.

 

e.

​every month.

 

ANSWER:  

b

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

21. ​On what date is the Sun the most intense in the Northern Hemisphere?

 

a.

​July 15

 

b.

​December 21

 

c.

​June 21

 

d.

​September 22

 

e.

​March 20

 

ANSWER:  

c

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

22. ​When it is January and winter in the Northern Hemisphere, it is ____ and ____ in the Southern Hemisphere.

 

a.

​January; summer

 

b.

​January; winter

 

c.

​July; winter

 

d.

​July; summer

 

e.

​March; spring

 

ANSWER:  

a

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

23. ​The most important reason why summers in the Southern Hemisphere are not warmer than summers in the Northern Hemisphere is that

 

a.

​Earth is closer to the Sun in January.

 

b.

​Earth is farther from the Sun in July.

 

c.

​over 80 percent of the Southern Hemisphere is covered with water.

 

d.

​the Sun’s energy is less intense in the Southern Hemisphere.

 

e.

​ice from Antarctica prevents it from getting very hot.

 

ANSWER:  

c

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

24. ​For maximum winter warmth, in the Northern Hemisphere, large windows in a house should face

 

a.

​north.

 

b.

​south.

 

c.

​east.

 

d.

​west.

 

e.

​any direction.

 

ANSWER:  

b

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

25. ​Our seasons are caused by

 

a.

​the amount of cloud cover during the different parts of the year.

 

b.

​the angle at which sunlight reaches Earth.

 

c.

​the proximity to the poles.

 

d.

​the constellation of Earth, Sun, and Moon.

 

e.

​differences in altitude.

 

ANSWER:  

b

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

26. ​Using sprinklers to prevent crop damage from cold air works best when

 

a.

​the air is fairly humid.

 

b.

​the air is fairly dry.

 

c.

​the air is dry and hot.

 

d.

​the air is dry and cold.

 

e.

​it’s over 30 degrees Celsius.

 

ANSWER:  

a

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

27. ​Earth is tilted at an angle of 23.5° with respect to the plane of its orbit around the Sun. If the amount of tilt were increased to 40°, we would expect in middle latitudes

 

a.

​hotter summers and colder winters than at present.

 

b.

​cooler summers and milder winters than at present.

 

c.

​hotter summers and milder winters than at present.

 

d.

​cooler summers and colder winters than at present.

 

e.

​no appreciable change from present conditions.

 

ANSWER:  

a

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

28. ​Although the polar regions radiate away more heat energy than they receive by insolation in the course of a year, they are prevented from becoming progressively colder each year by the

 

a.

​conduction of heat through the interior of Earth.

 

b.

​concentration of Earth’s magnetic field lines at the poles.

 

c.

​circulation of heat by the atmosphere and oceans.

 

d.

​the insulating properties of snow.

 

e.

​release of latent heat to the atmosphere when polar ice melts.

 

ANSWER:  

c

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

29. ​During the afternoon, the greatest temperature difference between surface air and the air several meters above occurs on a

 

a.

​clear, calm afternoon.

 

b.

​clear, windy afternoon.

 

c.

​cloudy, calm afternoon.

 

d.

​cloudy, windy afternoon.

 

e.

​cold, windy afternoon.

 

ANSWER:  

a

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.7 – Summarize the relationship between latitude, land and water distribution, ocean currents, and elevation on the daily and regional temperature variations observed on Earth.

OTHER:  

Bloom’s: Understand

 

30. ​The greatest variation in daily temperature usually occurs

 

a.

​at the ground.

 

b.

​about 5 feet above the ground.

 

c.

​at the top of a high-rise apartment complex.

 

d.

​at the level where thermals stop rising.

 

e.

​on top of a mountain.

 

ANSWER:  

a

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.6 – Define daily range of temperature, mean daily temperature, annual range of temperature, and mean annual temperature, and discuss the variables that influence these values.

OTHER:  

Bloom’s: Understand

 

31. ​The daily minimum temperature is usually observed

 

a.

​at the time of sunset.

 

b.

​near midnight.

 

c.

​several hours before sunrise.

 

d.

​around sunrise.

 

e.

​several hours after sunrise.

 

ANSWER:  

d

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.6 – Define daily range of temperature, mean daily temperature, annual range of temperature, and mean annual temperature, and discuss the variables that influence these values.

OTHER:  

Bloom’s: Understand

 

32. ​In clear weather, the air next to the ground is usually ____ than the air above during the night and ____ than the air above during the day.

 

a.

​hotter; more humid

 

b.

​colder; less humid

 

c.

​warmer; colder

 

d.

​warmer; warmer

 

e.

​colder; warmer

 

ANSWER:  

e

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.7 – Summarize the relationship between latitude, land and water distribution, ocean currents, and elevation on the daily and regional temperature variations observed on Earth.

OTHER:  

Bloom’s: Understand

 

33. ​Suppose yesterday morning you noticed ice crystals (frost) on the grass, yet the minimum temperature reported in the newspaper was only 35°F. The most likely reason for this apparent discrepancy is that

 

a.

​temperature readings are taken in instrument shelters more than 5 feet above the ground.

 

b.

​the thermometer was in error.

 

c.

​the newspaper reported the wrong temperature.

 

d.

​the thermometer was read before the minimum temperature was reached for that day.

 

e.

​the thermometer was read incorrectly.

 

ANSWER:  

a

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

34. ​At what time during a 24-hour day would a radiation temperature inversion best be developed?

 

a.

​at sunset

 

b.

​near sunrise

 

c.

​toward the end of the morning

 

d.

​between 3 and 5 p.m. when the air temperature reaches a maximum

 

e.

​at noon

 

ANSWER:  

b

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

35. ​The lag in daily temperature refers to the time lag between the

 

a.

​time of maximum solar radiation and the time of maximum temperature.

 

b.

​time of minimum temperature and the time of maximum solar radiation.

 

c.

​minimum and maximum temperature for a day.

 

d.

​minimum and maximum solar energy received at the surface for a given day.

 

e.

​sunrise and sunset.

 

ANSWER:  

a

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

36. ​Ideal conditions for a strong radiation inversion are a

 

a.

​clear, calm, dry, winter night.

 

b.

​clear, calm, moist, summer night.

 

c.

​cloudy, calm, moist, winter night.

 

d.

​cloudy, windy, moist, summer night.

 

e.

​clear, windy, dry, summer night.

 

ANSWER:  

a

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

37. ​On a clear, calm night, the ground and air above cool mainly by which process?

 

a.

​evaporation

 

b.

​reflection

 

c.

​convection

 

d.

​conduction

 

e.

​radiation

 

ANSWER:  

e

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

38. ​In a hilly region, the best place to plant crops that are sensitive to low temperatures is

 

a.

​on the valley floor.

 

b.

​along the hillsides.

 

c.

​on the top of the highest hill.

 

d.

​in any dry location.

 

e.

​near streams and rivers.

 

ANSWER:  

b

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

39. ​One would expect the lowest temperatures to be found next to the ground on a

 

a.

​clear, damp, windy night.

 

b.

​cloudy night.

 

c.

​clear, dry, calm night.

 

d.

​clear, dry, windy night.

 

e.

​rainy night.

 

ANSWER:  

c

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.7 – Summarize the relationship between latitude, land and water distribution, ocean currents, and elevation on the daily and regional temperature variations observed on Earth.

OTHER:  

Bloom’s: Understand

 

40. ​If tonight’s temperature is going to drop into the middle 20s (°F) and a fairly stiff wind is predicted, probably the best way to protect an orchard against a hard freeze is to (assume that cost is not a factor)

 

a.

​use helicopters.

 

b.

​use wind machines.

 

c.

​sprinkle the crops with water.

 

d.

​put orchard heaters to work.

 

e.

​pray for clouds.

 

ANSWER:  

c

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

41. ​An important reason for the large daily temperature range over deserts is

 

a.

​there is little water vapor in the air to absorb and re-radiate infrared radiation.

 

b.

​the light-colored sand radiates heat very rapidly at night.

 

c.

​dry air is a very poor heat conductor.

 

d.

​free convection cells are unable to form above the hot desert ground.

 

e.

​the ozone content of desert air is very low.

 

ANSWER:  

a

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

42. ​Over Earth as a whole, one would expect to observe the smallest variation in temperature from day to day and from month to month

 

a.

​at the North Pole.

 

b.

​in the center of a large land mass.

 

c.

​along the Pacific coast of North America.

 

d.

​high in the mountains in the middle of a continent.

 

e.

​on a small island near the equator.

 

ANSWER:  

e

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.6 – Define daily range of temperature, mean daily temperature, annual range of temperature, and mean annual temperature, and discuss the variables that influence these values.

OTHER:  

Bloom’s: Understand

 

43. ​Hypothermia is most common in

 

a.

​hot, humid weather.

 

b.

​cold, wet weather.

 

c.

​hot, dry weather.

 

d.

​cold, dry weather.

 

e.

​cold, dry weather.

 

ANSWER:  

b

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.9 – Analyze why temperatures can “feel” differently on different occasions, i.e., in different geographical locations, on different days, and during different parts of the day, and describe the potential effects of extreme hot and cold temperatures on human health.

OTHER:  

Bloom’s: Analyze

 

44. ​The wind-chill factor

 

a.

​relates body heat loss with wind to an equivalent temperature with no wind.

 

b.

​indicates the temperature at which water freezes on exposed skin.

 

c.

​takes into account humidity and air temperature in expressing the current air temperature.

 

d.

​tells farmers when to protect crops from a freeze.

 

e.

​determines how low the air temperature will be on any given day.

 

ANSWER:  

a

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.9 – Analyze why temperatures can “feel” differently on different occasions, i.e., in different geographical locations, on different days, and during different parts of the day, and describe the potential effects of extreme hot and cold temperatures on human health.

OTHER:  

Bloom’s: Analyze

 

45. ​When a liquid thermometer is held in direct sunlight,

 

a.

​it will accurately measure the air temperature.

 

b.

​it will measure a much higher temperature than that of the air.

 

c.

​it will measure a much lower temperature than that of the air.

 

d.

​it will measure the temperature of the Sun rather than the air.

 

e.

​it can overheat and explode.

 

ANSWER:  

b

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

46. ​An ideal shelter for housing a temperature-measurement instrument should be

 

a.

​white.

 

b.

​black.

 

c.

​in the shade.

 

d.

​both white and in the shade.

 

e.

​both black and in the shade.

 

ANSWER:  

d

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

47. ​On the summer solstice, the highest position of the noonday Sun is located

 

a.

​near the North Pole.

 

b.

​in the mid-latitudes of the Northern Hemisphere.

 

c.

​in the mid-latitudes of the Southern Hemisphere.

 

d.

​near the South Pole.

 

e.

​near the equator.

 

ANSWER:  

b

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

48. ​Longer days are generally associated with

 

a.

​less insolation.

 

b.

​more heating degree days.

 

c.

​more insolation.

 

d.

​colder daily temperatures.

 

e.

​large daily temperature variations.

 

ANSWER:  

c

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

49. ​Which of the following latitudes is closer to Earth’s axis?

 

a.

​0°N

 

b.

​15°N

 

c.

​40°N

 

d.

​60°N

 

e.

​90°N

 

ANSWER:  

e

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

50. ​At any given time, ____ of Earth is illuminated by the Sun.

 

a.

​one-fourth

 

b.

​one-third

 

c.

​one-half

 

d.

​two-thirds

 

e.

​three quarters

 

ANSWER:  

c

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

51. ​In the northern hemisphere, a solar panel should be placed on the side of the roof facing

 

a.

​east.

 

b.

​west.

 

c.

​north.

 

d.

​south.

 

e.

​any of these directions.

 

ANSWER:  

d

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

52. ​Because air temperatures normally decrease with increasing height, trees found on the cooler north-facing side of mountains are often those that usually grow

 

a.

​at lower elevations.

 

b.

​near the Arctic circle.

 

c.

​in arid climates.

 

d.

​near the equator.

 

e.

​at higher elevations.

 

ANSWER:  

e

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

53. ​Because the west side of a house warms rapidly in the afternoon, rooms facing that direction should have ____ windows in order for them to act as a thermal buffer.

 

a.

​small

 

b.

​larger

 

c.

​medium-size

 

d.

​no

 

e.

​many

 

ANSWER:  

a

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

54. ​If the cold occurs over a widespread area for a long enough time to damage certain crops, the extreme cold is called (a) ____.

 

a.

​frost

 

b.

​dew frost

 

c.

​freeze

 

d.

​dew

 

e.

​nip

 

ANSWER:  

c

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

55. ​Fruit trees are particularly vulnerable to cold weather ____.

 

a.

​when they are fruit-bearing

 

b.

​when they are bare

 

c.

​right after fruit have been picked

 

d.

​when they are blossoming

 

e.

when the first leaves show up

 

ANSWER:  

d

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

56. ​Heating degree days are determined by subtracting the ____ temperature for the ____ from 65 degrees Fahrenheit.

 

a.

​coldest; year

 

b.

​mean; year

 

c.

​warmest; week

 

d.

​coldest; day

 

e.

​mean; day

 

ANSWER:  

e

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

57. ​The term cooling degree day is used during ____ weather.

 

a.

warm

 

b.

​cold

 

c.

​freezing

 

d.

​humid

 

e.

​any

 

ANSWER:  

a

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

58. ​Farmers use an index called ____ as a guide to planting and for determining the approximate dates when a crop will be ready for harvesting.

 

a.

​heating degree days

 

b.

​harvesting degree days

 

c.

​growing degree days

 

d.

​cooling degree days

 

e.

​ripening degree days

 

ANSWER:  

c

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

59. ​A growing degree day for a particular crop is defined as a day on which the mean daily temperature is ____ degree above the base temperature (also known as the zero temperature)—the minimum temperature required for growth of that crop.

 

a.

​one

 

b.

​two

 

c.

​three

 

d.

​four

 

e.

​five

 

ANSWER:  

a

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

60. ​In humid Iowa, where summer nighttime temperatures are high, corn takes ____ time to mature than in the drier west.

 

a.

​the same amount of

 

b.

​twice as much

 

c.

​a quarter of the

 

d.

​more

 

e.

​less

 

ANSWER:  

e

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

61. ​In cold weather, when the air is calm, the temperature we perceive—called the sensible temperature—is often ____ a thermometer might indicate.

 

a.

​lower than

 

b.

​higher than

 

c.

​the same as

 

d.

​a fraction of what

 

e.

​at least twice as high as

 

ANSWER:  

b

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.9 – Analyze why temperatures can “feel” differently on different occasions, i.e., in different geographical locations, on different days, and during different parts of the day, and describe the potential effects of extreme hot and cold temperatures on human health.

OTHER:  

Bloom’s: Analyze

 

62. ​The wind-chill index takes into account the wind speed at about ____ above the ground instead of the where official readings are usually taken.

 

a.

​10 m (33 ft)

 

b.

​5 m (16.5 ft)

 

c.

​100 m (330 ft)

 

d.

​1.5 m (5 ft)

 

e.

​15 m (50 ft)

 

ANSWER:  

d

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.9 – Analyze why temperatures can “feel” differently on different occasions, i.e., in different geographical locations, on different days, and during different parts of the day, and describe the potential effects of extreme hot and cold temperatures on human health.

OTHER:  

Bloom’s: Analyze

 

63. ​The first sign of hypothermia is ____.

 

a.

​stupor

 

b.

​dehydration

 

c.

​exhaustion

 

d.

​collapse

 

e.

​frostbite

 

ANSWER:  

c

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.9 – Analyze why temperatures can “feel” differently on different occasions, i.e., in different geographical locations, on different days, and during different parts of the day, and describe the potential effects of extreme hot and cold temperatures on human health.

OTHER:  

Bloom’s: Analyze

 

64. ​This type of thermometer has a glass bulb attached to a sealed, graduated tube about 25 cm (10 in.) long. A very small opening, or bore, extends from the bulb to the end of the tube. A liquid in the bulb (usually mercury or red-colored alcohol) is free to move from the bulb up through the bore and into the tube. When the air temperature increases, the liquid in the bulb expands, and rises up the tube. When the air temperature decreases, the liquid contracts, and moves down the tube. Hence, the length of the liquid in the tube represents the air temperature.

 

a.

​liquid-in-glass thermometer

 

b.

​mercury thermometer

 

c.

​maximum thermometer

 

d.

​minimum thermometer

 

e.

​thermistor

 

ANSWER:  

a

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

65. ​Another name for an infrared sensor is ____.

 

a.

​thermistor

 

b.

​radiosonde

 

c.

​light thermometer

 

d.

​radiometer

 

e.

​thermocouple

 

ANSWER:  

d

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

66. ​A(n) ____ thermometer consists of two different pieces of metal (usually brass and iron) welded together to form a single strip.

 

a.

​thermograph

 

b.

​bilateral

 

c.

​electrical

 

d.

​thermoresistant

 

e.

​bimetallic

 

ANSWER:  

e

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

67. ​Data loggers are gradually replacing ____.

 

a.

​radiosondes

 

b.

​mechanical thermographs

 

c.

​electrical thermometers

 

d.

​mercury thermometers

 

e.

​wind-chill measurement devices

 

ANSWER:  

b

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

68. ​The daily (diurnal) range of temperature is greatest next to the ____________________.

ANSWER:  

ground

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

69. ​Considering each hemisphere as a whole, seasonal temperature variation in the Southern Hemisphere is ____________________ that in the Northern Hemisphere.

ANSWER:  

​less

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

70. ​The maximum in daytime surface temperature typically occurs ____________________ Earth receives its most intense solar radiation.

ANSWER:  

after​

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

71. ​In July, at middle latitudes in the Northern Hemisphere, the day is more than ____________________ hours long and is getting ____________________ with each passing day.

ANSWER:  

12; shorter

twelve; shorter​

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

72. ​In the northern hemisphere, north-facing hillsides have a(n) ____________________ growing season than south-facing hillsides.

ANSWER:  

​shorter

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

73. ​Maximum daily temperatures under hazy skies are typically ____________________ than those under clear skies.

ANSWER:  

greater

higher​

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.6 – Define daily range of temperature, mean daily temperature, annual range of temperature, and mean annual temperature, and discuss the variables that influence these values.

OTHER:  

Bloom’s: Understand

 

74. ​In many areas of the far western United States, only sparse vegetation grows on ____________________-facing slopes.

ANSWER:  

south​

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s: Understand

 

75. ​During the Northern Hemisphere’s summer, the daylight hours in northern latitudes are ____________________ than in middle latitudes.

ANSWER:  

longer​

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

76. ​If it is winter and January in New York City, the season in Sydney, Australia is ____________________.

ANSWER:  

summer​

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

77. ​In Pennsylvania and New York, wine grapes are planted on the side of ____________________ rather than in valleys.

ANSWER:  

hills

REFERENCES:  

Local Seasonal Variations

LEARNING OBJECTIVES:  

METT.AHRE.16.3.3 – Explain the reasons for local seasonal variations, and demonstrate how these variations can be most effectively utilized.

OTHER:  

Bloom’s:Understand

 

78. ​Minimum thermometers are usually read during the ____________________, yet they are reset in the ____________________.

ANSWER:  

morning; afternoon​

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.10 – Outline various techniques and devices that can be used to measure temperature on Earth.

OTHER:  

Bloom’s: Understand

 

79. ​On a warm summer day, one city experienced a daily range of 22°C (40°F), while another had a daily range of 10°C (18°F). One of these cities is located in New Jersey and the other in New Mexico. The highest daily range probably occurred in ____________________ where relatively dry summer air allows for large daily temperature ranges. The lowest daily range more than likely occurred in ____________________ where the humid summer air keeps the daily temperature range small.

ANSWER:  

New Mexico; New Jersey​

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.4 – Describe the variability observed in daytime warming as a function of location, and compare this with the geographical factors and processes that control nighttime cooling.

OTHER:  

Bloom’s: Remember

 

80. ​Because water heats and cools more slowly than land, the lag in daily temperature over water is usually much ____________________ than that experienced over land.

ANSWER:  

larger​

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.7 – Summarize the relationship between latitude, land and water distribution, ocean currents, and elevation on the daily and regional temperature variations observed on Earth.

OTHER:  

Bloom’s: Understand

 

81. ​If the tilt of Earth’s axis suddenly increased to 45o, average winter temperatures in the middle latitudes of the Northern Hemisphere would ____________________.

ANSWER:  

decrease​

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

82. ​Thermometers are designed to measure ___________________ and are not placed in direct sunlight, whereas our bodies, on the other hand, are influenced by both air temperature and direct sunlight. Therefore, we usually feel ____________________ on a cold, calm, sunny day than a thermometer indicates.

ANSWER:  

air temperature; warmer​

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.9 – Analyze why temperatures can “feel” differently on different occasions, i.e., in different geographical locations, on different days, and during different parts of the day, and describe the potential effects of extreme hot and cold temperatures on human health.

OTHER:  

Bloom’s: Analyze

 

83. ​The ____________________ degree-day is based on the assumption that people will begin to use their furnaces when the mean daily temperature drops below 65 degrees Fahrenheit.

ANSWER:  

heating degree​

REFERENCES:  

Applications of Air Temperature Data

LEARNING OBJECTIVES:  

METT.AHRE.16.3.8 – Interpret the meaning of cooling degree days, heating degree days, and growing degree days, and explain the relevance of each of these terms to human life.

OTHER:  

Bloom’s: Understand

 

84. ​In some years around the middle of autumn, there is an unseasonably warm spell, especially in the eastern two-thirds of the United States. This warm period is commonly referred to as ____________________.

ANSWER:  

​Indian Summer

Indian summer

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Remember

 

85. ​Orchard heaters that generate smoke are known as ____________________.

ANSWER:  

smudge pots​

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

86. ​Describe the seasons that you would experience in Australia in comparison to those in Germany.

ANSWER:  

Student answers may vary somewhat, but overall need to demonstrate knowledge that Australia is located in the Southern Hemisphere, whereas Germany is located in the Northern Hemisphere.

After June 21st, the Southern Hemisphere is tilted away from the Sun. Nights are long, days are short, and solar rays come in at an angle, which means that air temperatures are fairly low. The June solstice marks the astronomical beginning of winter in the Southern Hemisphere, however, summer does not “officially” begin until the Sun is over the Tropic of Capricorn (231/2S) on December 21st. So, when it is winter and June in the Southern Hemisphere, it is summer and June in the Northern Hemisphere. Conversely, when it is summer and December in the Southern Hemisphere, it is winter and December in the Northern Hemisphere.

We know Earth comes nearer to the Sun in January than in July. Even though this difference in distance amounts to only about 3 percent, the energy that strikes the top of Earth’s atmosphere is almost 7 percent greater on January 3 than on July 4. These statistics might lead us to believe that summer should be warmer in the Southern Hemisphere than in the Northern Hemisphere. However, this is not the case. A close examination of the Southern Hemisphere reveals that nearly 81 percent of the surface is water, compared to 61 percent in the Northern Hemisphere. The added solar energy due to the closeness of the Sun is absorbed by large bodies of water, becoming well mixed and circulated within them. This process keeps the average summer (January) temperatures in the Southern Hemisphere cooler than average summer (July) temperatures in the Northern Hemisphere. Because of water’s large heat capacity, it also tends to keep winters in the Southern Hemisphere warmer than we might expect. Another difference between the seasons of the two hemispheres concerns their length. Because Earth follows an elliptical path as it journeys around the Sun and because the ellipse is slightly off-center from the Sun, the total number of days from the vernal (March 20) to the autumnal (September 22) equinox is about 7 days longer than from the autumnal to vernal equinox. This means that spring and summer in the Northern Hemisphere not only last about a week longer than northern fall and winter, but also about a week longer than spring and summer in the Southern Hemisphere. Hence, the shorter spring and summer of the Southern Hemisphere somewhat offsets the extra insolation received due to a closer proximity to the Sun.

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.2 – Compare and contrast the cycle of seasons observed in the Northern Hemisphere with those in the Southern Hemisphere.

OTHER:  

Bloom’s: Understand

 

87. ​What are the hottest (coldest) place in the United States? What factors cause these extreme conditions at these locations?

ANSWER:  

Student answers should state that on July 10, 1913, Greenland Ranch in Death Valley, California, the highest temperature ever reliably observed in the world was 57 degrees Celsius (134 degrees Fahrenheit). Here, air temperatures are persistently hot throughout the summer, with the average maximum for July being 47 degrees Celsiu1221s (116 degrees Fahrenheit). During the summer of 1917, there was an incredible period of 43 consecutive days when the maximum temperature reached 120 degrees Fahrenheit or higher. One of the hottest urban areas in the United States is Palm Springs, California, where the average high temperature during July is 108 degrees Fahrenheit. Another hot city is Yuma, Arizona. Located along the California-Arizona border, Yuma’s high temperature during July also averages 108 degrees Fahrenheit. In 1937, the high in Yuma reached 100 degrees Fahrenheit or more for 101 consecutive days. In a more humid climate, the maximum temperature rarely climbs above 41degrees Celsius (106 degrees Fahrenheit). However, during the record heat wave of 1936, the air temperature reached 121 degrees Fahrenheit near Alton, Kansas. And during the heat wave of 1983, which destroyed about $7 billion in crops and increased the nation’s air-conditioning bill by an estimated $1 billion, Fayetteville reported North Carolina’s all-time record high temperature when the mercury hit 110 degrees Fahrenheit.

One city in the United States that experiences very low temperatures is International Falls, Minnesota, where the average temperature for January is –16 degrees Celsius (3 degrees Fahrenheit). Located several hundred miles to the south of International Falls, Minneapolis–St. Paul is the coldest major urban area in the nation, with an average temperature of –9 degrees Celsius (16 degrees Fahrenheit) for January. For duration of extreme cold, Minneapolis reported 186 consecutive hours of temperatures below 0 degrees Fahrenheit during the winter of 1911–1912. Within the forty-eight adjacent states, however, the record for the longest duration of severe cold belongs to Langdon, North Dakota, where the thermometer remained below 0 degrees Fahrenheit for 41 consecutive days during the winter of 1936.

The most extensive cold wave in the United States occurred in February 1899. Temperatures during this cold spell fell below 0 degrees Fahrenheit in every existing state, including Florida. This extreme cold event was the first and only of its kind in recorded history. Record temperatures set during this extremely cold outbreak still stand today in many cities of the United States. The official record for the lowest temperature in the forty-eight adjacent states belongs to Rogers Pass, Montana, where on the morning of January 20, 1954 the mercury dropped to –57 degrees Celsius (–70 degrees Fahrenheit). The lowest official temperature for Alaska, –62 degrees Celsius (–80 degrees Fahrenheit), occurred at Prospect Creek on January 23, 1971.​

REFERENCES:  

Why Earth Has Seasons

LEARNING OBJECTIVES:  

METT.AHRE.16.3.1 – Illustrate how Earth’s seasons are affected by Earth’s proximity to the Sun, the Sun’s angle to Earth, and the number of daylight hours on Earth.

OTHER:  

Bloom’s: Apply

 

88. ​Many gardeners know that, when a frost is expected, plants can be protected by covering them with large plastic tubs. Explain why this is an effective way of protecting plants from frost.

ANSWER:  

An appropriate student answer would be that small plants or shrubs may be protected from cold temperatures by covering them with straw, cloth, or plastic sheeting because this prevents ground heat from being radiated away to the colder surroundings. If you are a household gardener concerned about outside flowers and plants during cold weather, simply wrap them in plastic or cover each with a paper cup. On cold nights, certain crops can also be damaged by low temperatures. If the cold occurs over a widespread area for a long enough time to damage certain crops, the extreme cold is called a freeze.​

REFERENCES:  

Daily Warming and Cooling Air Near the Surface

LEARNING OBJECTIVES:  

METT.AHRE.16.3.5 – Discuss the impact that severe cooling can have on agriculture.

OTHER:  

Bloom’s: Understand

 

 

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