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8.5: Atmospheric Convection and Air Pressure Gradients/Systems

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    Atmospheric Convection

    Convection is the circulation of fluid due to density differences. Atmospheric convection works like a pot of boiling soup, warm fluid rising (in middle) and cool fluid falling (on sides). A rising storm thunderhead is an example of atmospheric convection. Warm moist air rises, expands, releases energy as clouds form. After releasing its heat and moisture, the cooled air sinks, displacing warm air below (Figure 8.13).

    Air convection
    Figure 8.13. Atmospheric convection.

    Air Pressure Gradients and Air Pressure Systems

    • Surface winds blow from high to low pressure - this is called a pressure gradient—displayed as lines of equal barometric pressure on a weather map (Figure 8.14). An air mass is a body of air with a relative horizontally uniform temperature, humidity, and pressure:

    High pressure systems have dry conditions with sinking air masses.
    Low pressure systems have wetter conditions with rising air masses.

    Air pressure gradient and air pressure systems
    Figure 8.14. Air pressure gradients and air pressure systems.

    8.5: Atmospheric Convection and Air Pressure Gradients/Systems is shared under a not declared license and was authored, remixed, and/or curated by Miracosta Oceanography 101 (Miracosta)) via source content that was edited to conform to the style and standards of the LibreTexts platform; a detailed edit history is available upon request.