ch16_atmosphere_students
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Student power point packet notesTRANSCRIPT
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CH. 16 – THE ATMOSPHERE
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Meteorology
Study of atmosphere & its dynamic processes (weather)
Weather – state of atmosphere at a given place for short period of time
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Meteorology
Climate - compilation of weather over time for a region
- changes gradually
Ex: Ice Age vs. present
Global warming
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Elements of Weather
1) 2) 3) 4) 5) 6)
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Heating the Atmosphere
Radiation – energy transmitted through space
Different types of energy travel at different wavelengths
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Heating the Atmosphere
All objects give off radiation:
Hotter object = shorter wavelength
Cooler object = longer wavelength
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Steps for heating the atmosphere:
1) Short wavelength solar radiation passes through atmosphere (uv & visible range)
2) Earth’s surface absorbs solar radiation & heats up
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Steps for heating the atmosphere:
3) Earth emits infrared radiation
4) CO2 & H2O vapor absorb infrared radiation
- “selective absorbers”
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Earth-Sun Relations
Causes annual variations in seasons at a given latitude
Rotation = Earth spins on axis
Revolution = Earth’s elliptical orbit around sun
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Earth’s axis:
Tilted 23 ½ o off vertical to plane of the ecliptic
- points to North Star
Most intense sunlight = solar rays striking Earth’s surface at 90o
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Earth-Sun Relations
Know for each season:
1) date
2) location of vertical rays of sun
3) nickname
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Controls of Temperature
1) Latitude controls:
a) Intensity = sun angle
Most intense = 90o
Lower sun angles = less intense
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Latitude
b) Amount = length of daylight hours
At night, Earth emits radiation w/o collecting anymore
- coolest temp. = _____________
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Latitude
Summer vs. WinterMore daylight hours = Earth builds
up surplus of energy (hot temp’s)Less daylight hours = Earth loses
more energy than it gains (cold temp’s)
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Latitude
Affects annual temperature rangei) Closer to equator = ____ annual
temp. rangeii) Closer to poles = _____ annual
temp. rangeWhy?
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Temperature Range
Difference between high & low temperatures
- daily, monthly, annual
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Controls of Temperature
2) Amount of water vapor
Water vapor acts as a “blanket”- critical to daily temperature
range
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Arid vs. Humid Regions
Arid regions:
Daily temp. range is__________
Humid regions:
Daily temp. range is __________
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Cloudy vs. Clear Nights
Cloudy night:
Daily temp. range is__________
Clear night:
Daily temp. range is __________
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Controls of Temperature
3) Land vs. water
____ heats more in summer
Land cools more in winter
Land has more variable annual temperature range than water
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Controls of Temperature
4) Elevation – land height above sea level
Cooler temp’s at higher elevations b/c:
a) Further from main heat source (“radiator”) = Earth’s surface
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Elevation
b) Less water vapor available in atmosphere
Why?
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Controls of Temperature
5) Geographic Position
- prevailing westerly wind directions between 30o & 60o latitude
- both hemispheres!
Ex: East Coast vs. West Coast
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Geographic Position
“Landlocked” cities have _______ annual temp. ranges
Coastal cities have ______ annual temp. ranges
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Global Temperature Distribution
Figures 16.32 & 16.33Isotherm = line connecting points
of equal temp’sNOTE:1) Isotherms run __________
Why?
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Global Temperature Distribution
2) Isotherm pattern is more ______ in Northern Hemisphere
Why?
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Global Temperature Distribution
3) Ocean surface currents alter general east-west trend of isotherms
“Gyre” = circular pattern of ocean currents
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Ocean Circulation
Poleward-moving currents are _______
Equatorward-moving currents are _______
Ex: Gulf Stream vs. California Current
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Ocean Circulation
Affects temperature mean at similar latitudes
Ex: England vs. Newfoundland