zenith insolation per area greater when sun is overhead
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zenith insolation per area: greater when Sun is overhead than near poles annually 2.4 times lower at poles than at equator Fig. 11.2a; source: Marshak The Earth SIO15-18: Lecture16: Winds and Weather Fig. 11.2a; source: Marshak The


  1. zenith insolation per area: greater when Sun is overhead than near poles annually 2.4 times lower at poles than at equator Fig. 11.2a; source: Marshak “The Earth” SIO15-18: Lecture16: Winds and Weather

  2. Fig. 11.2a; source: Marshak “The Earth” 2.4 less insolation/area near poles higher albedo (snow/ice) Fig. 11.3a; source: Ahrens “Meteorology Today” SIO15-18: Lecture16: Winds and Weather

  3. Fig. 11.2a; source: Marshak “The Earth” SIO15-18: Lecture16: Winds and Weather

  4. Fig. 12.10 see website! SIO15-18: Lecture16: Winds and Weather

  5. Fig. 12.10 wind blows from high to low pressure!! see website! SIO15-18: Lecture16: Winds and Weather

  6. Fig. 12.10 see website! SIO15-18: Lecture16: Winds and Weather

  7. Fig. 12.10 see website! SIO15-18: Lecture16: Winds and Weather

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