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Atmosheric Circulation Part II. Important Concepts to remember: Redistribution of Heat Effects of Rotation The role of friction Conservation of angular momentum. Seasonal Heating. Differential Heating From Equators to Poles. Non rotating view of Atmospheric Circulation. High Pressure.
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Atmosheric Circulation Part II Important Concepts to remember: Redistribution of Heat Effects of Rotation The role of friction Conservation of angular momentum
Differential Heating From Equators to Poles
Non rotating view of Atmospheric Circulation High Pressure Low Pressure
Schematic depiction of the development of the atmospheric circulation,starting from a state of rest Easterlies (Trades) Westerlies Redistribution of Heat – Large scale convective Cells
Some practical rules to remember: Fpressure Low Pressure High Pressure FCoriolis • Particle will have the Coriolis force 90 degrees to the right • Particles will tend to move along line of constant pressure • Particles will have the high pressure on their right (same as Coriolis)
Schematic depiction of the development of the atmospheric circulation,starting from a state of rest Easterlies (Trades) Westerlies
Problem? Circulation in the atmosphere
Schematic depiction of the development of the atmospheric circulation,starting from a state of rest Easterlies (Trades) Westerlies
Diagram of Atmospheric Circulation Circulation in the atmosphere
Vertical view of the atmosphere and Poleward Transport of Heat Hadley Cell Ferrel Cell Polar Cell Pole Equator
Vortices L H Fpressure FCoriolis FCoriolis Fpressure Low Pressure System High Pressure System
Hurricane IVAN H H L Fpressure H H FCoriolis
Polar High L L Subpolar Low H H H Subtropical High L Eq. Low L L H H H L L