The Soufrière Hills eruption in Montserrat in 1995
Scientific outlines of global warming have remained relatively unchanged for decades. Climate scientists, however, armed with better satellites and long-term data, continue to refine their understanding of the jogs up and down that typify the planet’s surface temperature, which can remain flat for years at a time before rising again. There are many pieces to this puzzle, and for more than a decade, one mystery has been centered high in the sky, in the freezing stratosphere.
Given its height, many miles above sea level, the stratosphere is typically a barren place. Suspended above the weather, this dry atmospheric layer rarely houses anything more tangible than gases. Occasionally a vast volcanic eruption—like Mount Pinatubo, in 1991—might inject a load of…
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