What is global circulation? | Part One | Differential heating

Met Office - Learn About Weather1 minute read

The Earth's curvature leads to differential heating, creating a thermal gradient between the equator and poles due to concentrated solar radiation at the equator. This gradient is moderated by global circulation, which redistributes heat through three large atmospheric cells in both hemispheres, maintaining habitable conditions in equatorial and polar regions.

Insights

  • The Earth's curvature results in uneven heating, with the equator receiving more direct sunlight compared to higher latitudes, creating a significant temperature difference between the equator and the poles.
  • Global atmospheric circulation plays a crucial role in balancing these temperature differences by redistributing heat through three major circulation cells in each hemisphere, which helps maintain livable conditions across diverse regions of the planet.

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Summary

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Heat Distribution and Earth's Atmospheric Circulation

  • The Earth's curvature causes differential heating, with more concentrated solar radiation at the equator and less at higher latitudes, leading to a thermal gradient between the equator and poles.
  • Global circulation redistributes heat through three large atmospheric cells in both hemispheres, preventing extreme temperature variations that could make equatorial and polar regions uninhabitable.
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