Notes
Slide Show
Outline
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Tropical Humid Climates (A)
  • Exists between 15-20° of the equator
  • The only truly winterless climates of the world
  • Unique due to the prevalence of moisture
    • Tropical Wet Climate (Af)
    • Tropical Monsoon (Am)
    • Tropical Savanna (Aw)
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Tropical Wet Climate (Af)
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Tropical Wet Climate (Af)
  • “f” stands for moist, from the German “feucht”
  • A monotonous, seasonless climate with endless repetition of rain and sun day after day (Avg. rain: 2.4” per month; avg. temperature is >64°F)
  • “Night is the winter of the tropics.”
  • High humidity makes for high sensible temperatures
  • Is a poorly ventilated climate with the exception of thermal convection due to extensive heating.
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Tropical Monsoon (Am)
  • Found primarily on windward (west-facing) coasts of southeastern Asia
  • During high-Sun (i.e. wet) season there is extensive instability of air masses, which brings torrents of rain
  • During low-Sun (i.e. dry) season Am climate is dominated by offshore winds (from a Asiatic high pressure center)
  • Avg. rain is between 100-200”
  • During the rainy season insolation is effectively blocked, which results in temperature being slightly lower
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Tropical Monsoon (Am)
  • Cherrapunji, India receives an annual average of 425” of rainfall.


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Tropical Savanna (Aw)
  • The most extensive of the A climates, savanna has clear-cut seasonal alternations of wet and dry periods
  • High-Sun season brings the ITCZ and pronounced rainfall
  • Low-Sun Season brings drought, including 3 or 4 rainless months
  • Three seasons: wet (w/ high sensible temperatures, muggy air, and frequent convective showers), dry (w/ clearing skies), and fire
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Savannas
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Tropical Savanna (Aw)
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ITCZ Seasonal Shift