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  2. Solar activity and climate - Wikipedia

    en.wikipedia.org/wiki/Solar_activity_and_climate

    [28] [42] Lockwood and Fröhlich, 2007, found "considerable evidence for solar influence on the Earth's pre-industrial climate and the Sun may well have been a factor in post-industrial climate change in the first half of the last century", but that "over the past 20 years, all the trends in the Sun that could have had an influence on the Earth ...

  3. Effect of Sun angle on climate - Wikipedia

    en.wikipedia.org/wiki/Effect_of_Sun_angle_on_climate

    The amount of heat energy received at any location on the globe is a direct effect of Sun angle on climate, as the angle at which sunlight strikes Earth varies by location, time of day, and season due to Earth's orbit around the Sun and Earth's rotation around its tilted axis.

  4. Should we dim the sun to help curb climate change? - AOL

    www.aol.com/news/dim-sun-help-curb-climate...

    At best, it’s viewed as a means of temporarily staving off the direst weather effects of climate change while the world carries out the lengthy and expensive effort of decarbonizing the global ...

  5. Solar phenomena - Wikipedia

    en.wikipedia.org/wiki/Solar_phenomena

    The energy of this sunlight supports almost all life [b] on Earth by photosynthesis, [13] and drives Earth's climate and weather. [14] As recent as the 19th century, scientists had little knowledge of the Sun's physical composition and source of energy.

  6. Orbital forcing - Wikipedia

    en.wikipedia.org/wiki/Orbital_forcing

    Orbital forcing is the effect on climate of slow changes in the tilt of the Earth's axis and shape of the Earth's orbit around the Sun (see Milankovitch cycles).These orbital changes modify the total amount of sunlight reaching the Earth by up to 25% at mid-latitudes (from 400 to 500 W/(m 2) at latitudes of 60 degrees).

  7. Illustrative model of greenhouse effect on climate change

    en.wikipedia.org/wiki/Illustrative_model_of...

    The total average energy per unit time radiated by Earth is equal to the average energy flux j times the surface area 4πR 2, where R is Earth's radius. On the other hand, the average energy flux absorbed from sunlight is the solar constant S 0 times Earth's cross section of πR 2, times the fraction absorbed by Earth, which is one minus Earth ...

  8. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    The Earth's weather is a consequence of its illumination by the Sun and the laws of thermodynamics. The atmospheric circulation can be viewed as a heat engine driven by the Sun's energy and whose energy sink, ultimately, is the blackness of space. The work produced by that engine causes the motion of the masses of air, and in that process it ...

  9. A look at what scientists say about the polar vortex and climate change. Fox Weather 19 hours ago Winter storm live tracker: Snowfall maps, current alerts, weather warnings, ice forecasts and more