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Non rotating planet. Rotating planet. Wind belts: symmetric case, and then land effects. Monsoons. Angular momentum. Change in length of day. time. Wind as a function of latitude and height. (Wells). Temperature as a function of latitude and height. (Wells).

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## Non rotating planet

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**Angular momentum**Change in length of day time**Wind**as a function of latitude and height (Wells)**Temperature as a**function of latitude and height (Wells)**Annual sea level pressure and winds**Wallace and Hobbs**Surface winds**& precipitation Wallace and Hobbs**Northern hemisphere - temperature difference from zonal**average in lower troposphere. (0 to 5 km)**Variability in pressure at ~ 8km**(i.e., weather!) This is actually the difference between the daily averaged height of the 200mb pressure level and its 5-day running average**Southern hemisphere - temperature difference from zonal**average in lower troposphere (0 to 5 km).**Southern hemisphere: heat flux from surface to atmosphere**(Winter) Wm-2**Southern hemisphere winter**Variability in pressure at ~ 8km (i.e., weather!) This is actually the difference between the daily averaged height of the 200mb pressure level and its 5-day running average

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