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Chapter 10 General Circulation of the Atmosphere General refers to the average air flow, actual winds will vary considerably. Average conditions help identify driving forces. The basic cause of the general circulation is unequal heating of the Earth’s surface Warm air is transferred from the Tropics to the Poles Cool air is transferred from the Poles to the Tropics General Circulation of the Atmosphere Single Cell Model Assume uniform water surface Sun always directly overhead the Equator Earth does not rotate Result: huge thermally direct convection cell (Hadley) 1. 2. 3. Three Cell Model Allow earth to spin = three cells (Hadley, Ferrell, Polar) Alternating belts of pressure starting with L at Equator Alternating belts of wind with NE just North of Equator General Circulation of the Atmosphere Average Surface Wind and Pressure: The Real World Semi-permanent high and lows Northern vs. Southern Hemisphere Major features shift seasonally with the high sun ○ North in July ○ South in December General Circulation of the Atmosphere General Circulation and Precipitation Patterns Rain where air rises (low pressure) Less rain where air sinks (high pressure) Average Wind Flow and Pressure Patterns Aloft North-South temperature and pressure gradient at high altitudes creates West-East winds, particularly at mid to high latitudes. Jet Streams 100-200 kt winds at 10-15km, thousands of km long, several 100 km wide and a few km thick (polar and subtropical) Observations: Dishpan Experiment Illustrates waves, with trough and ridge, develops in a rotating pan with heat on the exterior and cold at the center. Jet Streams Polar and Subtropical Jet Established by steep temperature and pressure gradients between circulation cells. Between tropical-mid-latitude cell (subtropical) and mid-latitude-polar cell (polar) Gradients greatest at polar jet Topic: Momentum Low-latitudes: atmosphere gains momentum High-latitudes: atmosphere losses momentum Conservation of Momentum Jet Streams Other Jet Streams Tropical easterly jet stream Low-level jet (nocturnal) Polar night jet streams Atmosphere Ocean Interactions Global Winds and Surface Ocean Currents Ocean surface dragged by wind, basins react to high pressure circulation forming gyres Cold current, flowing north to south, on west side of continent Warm current, flowing south to north, on east side of continent Oceanic front Stepped Art Fig. 10-14, p. 273 Atmosphere Ocean Interactions Upwelling Ekman spiral, Ekman transport Water moving away from the coast causes upwelling El Nino and the Southern Oscillation El Nino: irregular warm episode off west coast of South America Southern Oscillation: rise in pressure over W Pacific, fall in the E Pacific, equatorial countercurrent ENSO La Nina teleconnection Atmosphere Ocean Interactions Pacific Decadal Oscillation Reversal in Pacific Ocean temperatures Warm = more Pacific storms Cool = cool, wet NW North America, wetter over the Great Lakes, salmon fisheries decline Atmosphere Ocean Interactions North Atlantic Oscillation Reversal of pressure in North Atlantic Ocean affecting weather in Europe and eastern coast of North America Positive = strong Westerlies, storms in N Europe, wet and mild in eastern US Negative = wet southern Europe and Mediterranean, cold and dry in eastern US Atmosphere Ocean Interaction Arctic Oscillation Closely related to NAO Pressure changes between Arctic and adjacent southern areas causes changes upper-level winds Positive = mild winter in US and W Europe Negative = cold US, cold dry Europe, wet Mediterranean