Presentation is loading. Please wait.

Presentation is loading. Please wait.

Atmosheric Circulation Part II

Similar presentations


Presentation on theme: "Atmosheric Circulation Part II"— Presentation transcript:

1 Atmosheric Circulation Part II
Important Concepts to remember: Redistribution of Heat Effects of Rotation The role of friction Conservation of angular momentum

2 Seasonal Heating

3 Differential Heating From Equators to Poles

4 Non rotating view of Atmospheric Circulation
High Pressure Low Pressure

5 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

6 Rotation effects, the Coriolis Force

7 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)

8 Easterlies (Trades) Westerlies
Schematic depiction of the development of the atmospheric circulation, starting from a state of rest Easterlies (Trades) Westerlies

9 Circulation in the atmosphere
Problem? Circulation in the atmosphere

10 Role of Friction

11 Easterlies (Trades) Westerlies
Schematic depiction of the development of the atmospheric circulation, starting from a state of rest Easterlies (Trades) Westerlies

12 Circulation in the atmosphere
Diagram of Atmospheric Circulation Circulation in the atmosphere

13 Vertical view of the atmosphere and Poleward Transport of Heat
Hadley Cell Ferrel Cell Polar Cell Pole Equator

14 Midlatitude Cyclones

15 Poleward Heat Transport

16

17 Role of Friction on synoptic scales

18 L H Vortices Low Pressure System High Pressure System Fpressure
FCoriolis FCoriolis Fpressure Low Pressure System High Pressure System

19

20 Hurricane IVAN H H L Fpressure H H FCoriolis

21

22 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

23 Rotation effects are not always important

24 Land-Sea Breeze

25 Moonsoons, a continental scale land-sea breeze


Download ppt "Atmosheric Circulation Part II"

Similar presentations


Ads by Google