Atmospheric convection

Atmospheric convection

Auto-curated
Playing 1/5
  • Convection

    YouTube 02:22
  • Radiation and heat transfer in the atmosphere

    YouTube 02:46
  • Atmospheric Convection Currents

    YouTube 03:59
  • What is global circulation? | Part Two | The three cells

    YouTube 03:35
  • 6. Convection in the Atmosphere

    YouTube 02:32

Atmospheric convection is the result of a parcel-environment instability, or temperature difference, layer in the atmosphere. Different lapse rates within dry and moist air masses lead to instability. Mixing of air during the day which expands the height of the planetary boundary layer leads to increased winds, cumulus cloud development, and decreased surface dew points. Moist convection leads to thunderstorm development, which is often responsible for severe weather throughout the world. Special threats from thunderstorms include hail, downbursts, and tornadoes.

Discover in context

This site is not available in the landscape mode.
Please rotate your phone or install our app.