How does the sun affect our climate?
Our sun is the source of most of the energy that drives the biological and physical processes in the world around us—in oceans and on land it fuels plant growth that forms the base of the food chain, and in the atmosphere, it warms air which drives our weather.
The rate of energy coming from the sun changes slightly day to day. Over many millennia the earth-sun orbital relationship can change the geographical distribution of the sun’s energy over the earth’s surface. It has been suggested that changes in solar output might affect our climate—both directly, by changing the rate of solar heating of the earth and atmosphere, and indirectly, by changing cloud forming processes.
Over the time-scale of millions of years, the change in solar intensity is a critical factor influencing climate (e.g., ice ages). However, changes in the rate of solar heating over the last century cannot account for the magnitude of the rise in global mean temperature since the late 1970s.
Scientists have considered the sun-climate hypothesis to explain the earth’s rapid warming. The evidence collected shows that the sun noticeably affects our climate over millions of years, but it is not the cause of recent warming.
The rate at which energy from the sun reaches the top of earth’s atmosphere is called “total solar irradiance” (or TSI). TSI fluctuates slightly from day to day and week to week. In addition to these rapid, short-term fluctuations, there is an 11-year cycle in TSI measurements related to “sunspots” (a part of the sun’s surface that is temporarily cooler and darker than its neighboring regions).
Two different hypotheses have been proposed to test whether solar radiation can explain climate change.
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