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Atmosphere and Hydrosphere SJCHS
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Atmosphere Atmosphere: Layer of gases that surround the Earth Composition 78 % Nitrogen 21% Oxygen 1% Other (Water Vapor, CO 2 ) Particles: dust, pollen, smoke, exhaust, pyroclastic material
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Atmosphere Troposphere: 0- ~12 km; temperature decreases as altitude increases Heated by solar radiation; where most weather events occur
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Atmosphere Ozone Layer: Made of O 3 Formation absorbs UV light from the sun
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Atmosphere A major function of atmosphere is to regulate heating of Earth
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Radiation Solar radiation: Energy that heats Earth in form of following rays: UV, visible light, infrared
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Radiation Light can be transmitted, absorbed, reflected
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Radiation 50 % of solar energy is absorbed by Earth ’ s surface/ocean 20% of solar energy is absorbed by atmosphere 30% is reflected to space from atmosphere, clouds, surface
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Convection Convection: Transfer of heat by the movement of a fluid (such as air or water)
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Convection A pocket of air (or a thermal) is heated at surface of Earth by conduction, becoming less dense Air rises, expands, and cools Cool air is more dense and will fall to Earth Convection circulation cycle repeats
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Coriolis Effect Due to rotation counterclockwise of the Earth, objects change direction (NOT SPEED) Northern Hemisphere: Deflect right Southern Hemisphere: Deflect left
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Cyclones Tropical Cyclone (aka hurricane or typhoon): Storms that form at low pressure areas over warm water
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Videos: Hurricane Formation
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Fronts Front: Boundary between air masses; where most major weather events occur
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Fronts Warm Front: Warm air moves above cold air causing precipitation
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Fronts Cold Front: Cold air sinks under warm air causing heavy precipitation
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Seasons Solar energy that strikes the Earth ’ s surface directly is more intense than solar energy that strikes at an angle
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Seasons Due to Earth ’ s spherical shape, areas at equator get more sun than areas near the poles
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Seasons Albedo: Measurement of light reflected from a surface high albedo, more reflection, lower temperatures
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Seasons Earth ’ s orbit is elliptical and Earth is at a tilt
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Seasons SeasonTilt of EarthDay lengthTemperature SummerTowardsLongerWarmer WinterAwayShorterColder Northern Hemisphere (opposite for Southern Hemisphere)
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Seasons In Northern hemisphere, objects facing south get more sunlight in mid- latitudes
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Seasons Applications Ski runs tend to be on north side of mountains Solar panels face south
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Convection Unequal heating, convection and the CE causes global wind patterns that affect climate on Earth
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Why is the sky blue? When sunlight enters the atmosphere, light can scatter (reflected in many directions)
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Why is the sky blue? Light that is reflected is what we see (other colors absorbed)
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Why is the sky blue? When light hits an oxygen or nitrogen (or any small molecule) shorter wavelengths of light are scattered Light will be scattered in all directions
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Why is the sky blue? Larger particles (water vapor) scatter different wavelengths Traveling through more atmosphere scatters different wavelengths
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Why isn’t the sky violet? Human eyes contain red, green, and blue cones that allow us to see color The brain interprets the color of sky as blue
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Hydrosphere Hydrosphere: Ocean (salt) and freshwater on or underneath Earth(ground water/aquifers) Freshwater is a limited resource
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Videos: Freshwater as a limited resource and solutions Water in Africa Play Pump Water in California
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Ocean Currents Upper ocean circulation is driven by winds Gyres: Circular motion of water Clockwise in Northern Hemisphere, Counterclockwise in Southern Hemisphere
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Ocean Currents Thermohaline/ Deep Water Circulation: Colder/ high salinity water sinks, warmer/ less salinity water rises forming a deep water current
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Hydrosphere http://video.pbs.org/video/2203388630 http://video.pbs.org/video/2222028532 http://video.pbs.org/video/1533347949 http://video.pbs.org/video/2212706337 http://video.pbs.org/video/2263346756 http://www.history.com/videos/the-aswan-high-dam#the- aswan-high-dam
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