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  2. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    The rising air creates a low pressure zone near the equator. As the air moves poleward, it cools, becomes denser, and descends at about the 30th parallel, creating a high-pressure area. The descended air then travels toward the equator along the surface, replacing the air that rose from the equatorial zone, closing the loop of the Hadley cell. [3]

  3. Westerlies - Wikipedia

    en.wikipedia.org/wiki/Westerlies

    If the Earth were tidally locked to the Sun, solar heating would cause winds across the mid-latitudes to blow in a poleward direction, away from the subtropical ridge. . However, the Coriolis effect caused by the rotation of Earth tends to deflect poleward winds eastward from north (to the right) in the Northern Hemisphere and eastward from south (to the left) in the Southern Hemisph

  4. Polar easterlies - Wikipedia

    en.wikipedia.org/wiki/Polar_easterlies

    In the study of Earth's atmosphere, polar easterlies are the dry, cold prevailing winds that blow around the high-pressure areas of the polar highs at the North and South Poles. [1] Cold air subsides at the poles creating high pressure zones, forcing an equatorward outflow of air; that outflow is then deflected westward by the Coriolis effect.

  5. Hadley cell - Wikipedia

    en.wikipedia.org/wiki/Hadley_cell

    Hadley's model of the global atmospheric circulation being characterized by hemisphere-wide circulation cells was also challenged by weather observations showing a zone of high pressure in the subtropics and a belt of low pressure at around 60° latitude. This pressure distribution would imply a poleward flow near the surface in the mid ...

  6. High-pressure area - Wikipedia

    en.wikipedia.org/wiki/High-pressure_area

    A high-pressure area, high, or anticyclone, is an area near the surface of a planet where the atmospheric pressure is greater than the pressure in the surrounding regions. Highs are middle-scale meteorological features that result from interplays between the relatively larger-scale dynamics of an entire planet's atmospheric circulation .

  7. Trade winds - Wikipedia

    en.wikipedia.org/wiki/Trade_winds

    An increase of temperature with height is known as a temperature inversion. When it occurs within a trade wind regime, it is known as a trade wind inversion. [12] The surface air that flows from these subtropical high-pressure belts toward the Equator is deflected toward the west in both hemispheres by the Coriolis effect. [13]

  8. Wind and solar generated a record amount of global power in 2022

    www.aol.com/news/wind-solar-generated-record...

    Record growth in wind and solar last year pushed worldwide electricity generation to its cleanest-ever level, a report found, reflecting a renewable energy boom that researchers say could herald ...

  9. Wind - Wikipedia

    en.wikipedia.org/wiki/Wind

    This barrier jet can increase the low-level wind by 45%. [52] Wind direction also changes because of the contour of the land. [53] If there is a pass in the mountain range, winds will rush through the pass with considerable speed because of the Bernoulli principle that describes an inverse relationship between speed and pressure. The airflow ...