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  2. Climate variability and change - Wikipedia

    en.wikipedia.org/wiki/Climate_variability_and_change

    A change in the type, distribution and coverage of vegetation may occur given a change in the climate. Some changes in climate may result in increased precipitation and warmth, resulting in improved plant growth and the subsequent sequestration of airborne CO 2. Though an increase in CO 2 may benefit plants, some factors can diminish this increase.

  3. El Niño–Southern Oscillation - Wikipedia

    en.wikipedia.org/wiki/El_Niño–Southern...

    The Southern Oscillation is the accompanying atmospheric oscillation, which is coupled with the sea temperature change. El Niño is associated with higher than normal air sea level pressure over Indonesia, Australia and across the Indian Ocean to the Atlantic. La Niña has roughly the reverse pattern: high pressure over the central and eastern ...

  4. Climate change - Wikipedia

    en.wikipedia.org/wiki/Climate_change

    After 1970, the increasing accumulation of greenhouse gases and controls on sulfur pollution led to a marked increase in temperature. [51] [52] [53] NASA animation portraying global surface temperature changes from 1880 to 2023. The colour blue denotes cooler temperatures and red denotes warmer temperatures.

  5. Weather front - Wikipedia

    en.wikipedia.org/wiki/Weather_front

    A weather front is a boundary separating air masses for which several characteristics differ, such as air density, wind, temperature, and humidity. Disturbed and unstable weather due to these differences often arises along the boundary. For instance, cold fronts can bring bands of thunderstorms and cumulonimbus precipitation or be preceded by ...

  6. Thermal wind - Wikipedia

    en.wikipedia.org/wiki/Thermal_wind

    The thermal wind is the change in the amplitude or sign of the geostrophic wind due to a horizontal temperature gradient. The geostrophic wind is an idealized wind that results from a balance of forces along a horizontal dimension. Whenever the Earth's rotation plays a dominant role in fluid dynamics, as in the mid-latitudes, a balance between ...

  7. Mixed layer - Wikipedia

    en.wikipedia.org/wiki/Mixed_layer

    The surface mixed layer is a layer where this turbulence is generated by winds, surface heat fluxes, or processes such as evaporation or sea ice formation which result in an increase in salinity. The atmospheric mixed layer is a zone having nearly constant potential temperature and specific humidity with height.

  8. Wind - Wikipedia

    en.wikipedia.org/wiki/Wind

    This barrier jet can increase the low-level wind by 45%. [51] Wind direction also changes because of the contour of the land. [52] 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 ...

  9. Sudden stratospheric warming - Wikipedia

    en.wikipedia.org/wiki/Sudden_stratospheric_warming

    According to the World Meteorological Organization's Commission for Atmospheric Sciences: [12]: 19 "a stratospheric warming can be said to be major if at 10 mb or below the latitudinal mean temperature increases poleward from 60 degree latitude and an associated circulation reversal is observed (that is, the prevailing mean westerly winds ...