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| Eruption at Eyjafjallajökull April 17, 2010. Credit: Árni Friðriksson |
What the authors found was that under two of three Representative Concentration Pathways (RCP4.5 and RCP8.5, but not so much under RCP2.6), global warming will likely have the effect of reducing the cooling effect of volcanoes.
The reason for this is, as the authors write: "the critical mass eruption rate required to reach the tropopause will increase as a consequence of:
- a decrease in the heights of tropospheric plumes driven by a decrease of the tropospheric temperature lapse rate; and
- an increase of the tropopause height."
