01.01.70

Note that the numbers provided in this review post are best estimates from each paper.  For the sake of comprehensibility we have not included error bars, but we have provided links to the original fact-finding for those who would like to see the uncertainty ranges in each estimate.

Most of the studies discussed below looked at the same few influences on far-reaching temperature, because they are the dominant effects.

As we know,  human greenhouse gas (GHG) emissions  heated the planet by increasing the abundance of greenhouse gases in the atmosphere, thus  increasing the greenhouse clout .

Solar activity  also warms or cools the planet by increasing or decreasing the amount of emanation reaching the Earth’s atmosphere and surface.

Volcanic vigour  generally cools the planet over short timeframes by releasing sulfate aerosols into the feel, which block sunlight and reduce the amout of solar radiation reaching the exterior.  However, unlike many greenhouse gases, aerosols are washed out of the feeling quickly, mostly after just 1-2 years.  Thus the main volcanic crashing on long-term temperature changes occur when there is an extended full stop of particularly high or low volcanic activity.

Source: PlanetSave.com

by Mike Fast

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by Robert Wenzel

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