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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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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