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This lecture explores the general model of atmospheric circulation, including the basic nature of atmospheric motion on our rotating Earth. It discusses what regulates the motion of fluid particles in the ocean and atmosphere, the driving forces behind atmospheric circulation, and the role of heating by the sun. The lecture also covers air pressure, the Coriolis force, and the circulation patterns in different latitudes.
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Lecture 06 Circulation in the Atmosphere Circulation in the atmosphere
Learning objects • Review the general model of atmospheric circulation • Explore the basic nature of atmospheric motion on our rotating Earth
Newton’s Law What regulates the motion of fluid particles in the ocean and atmosphere?
troposphere surface Higher Latitudes Equator/Tropics What drives the circulation of the atmosphere? Heating by the sun AIR PRESSURE
Vertical view of air pressure (global convection) High Pressure Low Pressure High Pressure
Horizontal view of air pressure at ocean surface High Pressure + Higher Latitudes Surfaces of constant pressure y (latitude) x (longitude) _ Equator/Tropics Low Pressure
Newton’s Law v y (latitude) x (longitude) u Motion across Latitudes Motion along Latitude
Hurricane IVAN H H L H H
t3 t4 t2 t5 t1 Fpressure FCoriolis Rate of Rotation North Hemisphere Low Pressure B A High Pressure
Newton’s Law v y (latitude) x (longitude) u Motion across Latitudes Motion along Latitude
t3 t4 t2 t5 t1 Fpressure FCoriolis Rate of Rotation North Hemisphere A B High Pressure Low Pressure
Newton’s Law v y (latitude) x (longitude) u Motion across Latitudes Motion along Latitude
Fpressure FCoriolis FCoriolis Fpressure Fpressure Fpressure FCoriolis FCoriolis When this balance is reached the movement of the particles (and therefore of the flow) is called geostrophic motion
Newton’s Law v y (latitude) x (longitude) u Motion across Latitudes Motion along Latitude
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)
Hurricane IVAN H H L Fpressure H H FCoriolis
Vortices in N.H. L H Fpressure FCoriolis FCoriolis Fpressure Low Pressure System High Pressure System
Vertical view of the atmosphere Pole Equator
Polar High L L Subpolar Low H H H Subtropical High L Eq. Low L L H H H L L
Vertical view of the atmosphere and Poleward Transport of Heat Pole Equator
Differential Heating From Equators to Poles
How the ocean responds to the atmospheric wind and how it contributes to the heat transport
Important Concepts to remember: Redistribution of Heat Effects of Rotation The role of friction Conservation of angular momentum
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
Review of Conservation of angular momentum (a second look) The Atmopsheric Circulation (a view from space and from NWS models) A closer look at Huricanes, their formation and the oceanic response Zonal average circulation Radiative Budget
Schematic depiction of the development of the atmospheric circulation,starting from a state of rest Easterlies (Trades) Westerlies