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Circulation in the Atmosphere. Circulation in the atmosphere. Newton’s Law. What regulates the motion of fluid particles in the ocean and atmosphere?. What drives the circulation of the atmosphere?. Differential Heating From Equators to Poles. troposphere. surface. Higher Latitudes.
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Circulation in the Atmosphere Circulation in the atmosphere
Newton’s Law What regulates the motion of fluid particles in the ocean and atmosphere?
What drives the circulation of the atmosphere? Differential Heating From Equators to Poles
troposphere surface Higher Latitudes Equator/Tropics What drives the circulation of the atmosphere?
Vertical view of air pressure (global convection) High Pressure Low Pressure Low 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
v Newton’s Law 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
v Newton’s Law 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
v Newton’s Law 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
v Newton’s Law 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 L H Fpressure FCoriolis FCoriolis Fpressure Low Pressure System High Pressure System
Atmosheric Circulation 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
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
Atmosheric Circulation Part II 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
Atmosheric Circulation Part III 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
Atmosheric Circulation Part III 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
A look at the atmospheric circulation from space http://www.atmos.washington.edu/~ovens/loops/wxloop.cgi?wv_moll+/14d/ Advection of water vapour associated with Eastrerlies and Westerlies Strong convection over tropical region Generation of Tropical Cyclones