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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
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Seasonal Heating
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Differential Heating From Equators to Poles
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Non rotating view of Atmospheric Circulation
High Pressure Low Pressure
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Redistribution of Heat – Large scale convective Cells
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
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Rotation effects, the Coriolis Force
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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)
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Easterlies (Trades) Westerlies
Schematic depiction of the development of the atmospheric circulation, starting from a state of rest Easterlies (Trades) Westerlies
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Circulation in the atmosphere
Problem? Circulation in the atmosphere
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Role of Friction
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Easterlies (Trades) Westerlies
Schematic depiction of the development of the atmospheric circulation, starting from a state of rest Easterlies (Trades) Westerlies
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Circulation in the atmosphere
Diagram of Atmospheric Circulation Circulation in the atmosphere
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Vertical view of the atmosphere and Poleward Transport of Heat
Hadley Cell Ferrel Cell Polar Cell Pole Equator
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Midlatitude Cyclones
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Poleward Heat Transport
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Role of Friction on synoptic scales
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L H Vortices Low Pressure System High Pressure System Fpressure
FCoriolis FCoriolis Fpressure Low Pressure System High Pressure System
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Hurricane IVAN H H L Fpressure H H FCoriolis
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L L H H H L L L H H H L L Polar High Subpolar Low Subtropical High
Eq. Low L L H H H L L
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Rotation effects are not always important
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Land-Sea Breeze
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Moonsoons, a continental scale land-sea breeze
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