The slight increase in solar energy during the peak production of sunspots is absorbed by stratospheric ozone, warming the air in the stratosphere over the tropics, where sunlight is most intense. The additional energy also stimulates the production of additional ozone there that absorbs even more solar energy.
Since the stratosphere warms unevenly, with the most pronounced warming occurring nearer the equator, stratospheric winds are altered and, through a chain of interconnected processes, end up strengthening tropical precipitation.
At the same time, the increased sunlight at solar maximum — a peak of sunspot and solar storm activity we're currently headed toward — causes a slight warming of ocean surface waters across the subtropical Pacific, where sun-blocking clouds are normally scarce. That small amount of extra heat leads to more evaporation, putting additional water vapor into the atmosphere. The moisture is carried by trade winds to the normally rainy areas of the western tropical Pacific, fueling heavier rains and reinforcing the effects of the stratospheric mechanism.
These two processes reinforce each other and intensify the effect.
These stratospheric and ocean responses during solar maximum keep the equatorial eastern Pacific even cooler and drier than usual, producing conditions similar to a La Nina event. However, the cooling of about 1-2 degrees Fahrenheit is focused farther east than in a typical La Nina (the opposite sister effect of the warm-water El Nino), is only about half as strong, and is associated with different wind patterns in the stratosphere
Al Gore could not be reached for comment.
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