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Temperature
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a measure of the average speed at which molecules are moving or vibrating.
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Temperature scales Freeze Boil Celsius 100 Fahrenheit 32 212 Kelvin
100 Fahrenheit 32 212 Kelvin 273 373
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Conversions oF = (1.8 x oC) + 32 oC = 0.56 (oF – 32) K = oC + 273
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What Controls temperature?
1. Insolation differences (latitudinal , seasonal, daily) 2. Proximity to water bodies (land/water distribution) 3. Elevation 4. Ocean currents 5. Cloud Cover
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1. Insolation a. Latitudinal
High latitudes receive less insolation than low latitudes because… sun’s rays are more oblique Day length is variable Net energy surplus in tropics; net energy deficit in polar regions demonstrate
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b. Seasonal Changing angle of sun throughout the year changes temperature on a seasonal basis.
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c. Daily (diurnally) Changing angle of sun throughout the day changes temperature on a daily basis.
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Diurnal temperature pattern
Temperature increases as long as net all wave incoming exceeds net all wave outgoing. Min: end of deficit Max: end of surplus
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2. Proximity to water bodies
Water bodies have a moderating effect on temperature. Maritime locations (coastal, island) have smaller daily and annual ranges in temp than continental locations demonstration
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Small effect from Lake Superior on Duluth temperatures
Warmer winters, cooler summers near lake vs inland Top of the hill vs. harbor Harbor warmer in fall; cooler in spring Extreme example (May 2009)
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3. Elevation Temperature decreases as elevation increases.
less mass, less pressure, less absorption
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4. Ocean Currents Ocean exchanges heat with atmosphere and therefore
influences air temperature.
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Gulf Stream
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5. Cloud Cover Exert influence on shortwave and longwave exchanges:
Very efficient absorbers and emitters of longwave Reduce incoming shortwave High albedo
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Net Result: Dampen diurnal temp range
Cloudy: uniform temps, small diurnal range Clear: daytime high insolation and nighttime loss of longwave; large diurnal range About cloud measurement
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Factors affecting the air temperature of a place:
Review: Factors affecting the air temperature of a place: Insolation differences at various latitudes, during seasons, during the course of a day Proximity to big water bodies Elevation Ocean currents Cloud cover
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