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Chapter 8 The Ocean and the Atmosphere
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Weather & Climate
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Meteorology 1400’s Rain gauge Anemometer Humidity 1600’s Barometer Atmospheric circulation cells Edmund Halley George Hadley William Ferrell
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Weather Prediction & Chaos Theory
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Air-Sea Interface Vapor Pressure Evaporation Condensation
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Clouds
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Dimethyl Sulfides (DMS) Self-supporting thermal control system
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The Atmosphere
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Wind Stress & Turbulence
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Sea Ice Forms at polar latitudes Salt molecules excluded from ice latticework
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Sea Ice Floes Ridges & hummocks Fast ice
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Sea Ice Arctic Semi-enclosed 2-3 m 3% decrease per decade Antarctic Open 1-2 m
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Ice-Albedo Positive Feedback Loop How melting ice causes more ice to melt!
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Effects of Rotation Coriolis Effect
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Coriolis Effect Coriolis effect is the apparent deflection of moving objects to the right in the Northern Hemisphere and to the left in the Southern Hemisphere The deflection is caused by the differential speed of rotation between Earth’s equator and polar regions, relative to an object moving across the Earth’s surface. Centrifugal force
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