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Published byShania Fair Modified over 10 years ago
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Air Temperature
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► Temperature : a measure of the average speed at which molecules are moving or vibrating.
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► Air temperature the rate of motion of gas molecules in the atmosphere as a result of the absorption of energy measured by a thermometer
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Temperature scales ► Celsius water freezes at 0 o water boils at 100 o ► Fahrenheit water freezes at 32 o water boils at 212 o ► Kelvin no molecular motion at 0 K water freezes at 273 K water boils at 373 K
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Conversions ► o F = (1.8 x o C) + 32 ► o C = 0.56 ( o F - 32) ► K = o C + 273
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What determines the temperature of a place? 1. Insolation (daily and annual cycles) 2. Latitude 3. Urban/Rural Surface 4. Coastal vs. Interior location 5. Elevation
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1. Insolation A. Changing angle of noon sun throughout the year changes temperature on a seasonal basis.
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► Why temperature difference between equinoxes?
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► Spring : at end of cold, short day period more energy loss ► Autumn : at end of warm, long day period more energy gain
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1. Insolation B. Changing angle of sun throughout the day changes temperature on a daily basis.
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► lag between max insolation and max temperature because highest temp at time of max ABSORBED insolation
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2. Latitude ► Higher latitudes receive less insolation than lower latitudes sun’s rays are more oblique daylength is variable Net energy surplus in tropics; net energy deficit in polar regions
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3. Urban/rural Surface ► Evapotranspiration differences ► Urban impervious surfaces ► Urban highly absorbent (low albedo) surfaces ► Urban fuel consumption and excess heat ► “Urban heat island”
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4. Coastal vs. interior locations ► Water bodies have a moderating effect on temperature.
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► “Land heats up and cools down more rapidly than water.” Therefore: ► Coastal: smaller temperature ranges than continental locations. ► Coastal locations have their maximum temperatures well after maximum insolation.
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► Lake effect in Duluth is an example of changes in temperature due to being close to a large body of water.
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5. Altitude / Elevation ► Temperature decreases as elevation increases. less mass, less pressure, less absorption
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Exception: temperature inversion
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► Conditions favorable for a temperature inversion: cool, clear, calm night
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