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    This chapter has been cited by the following publications. This list is generated based on data provided by CrossRef.

    Li, Jingwan and Sharma, Ashish 2013. Evaluation of volcanic aerosol impacts on atmospheric water vapor using CMIP3 and CMIP5 simulations. Journal of Geophysical Research: Atmospheres, Vol. 118, Issue. 10, p. 4448.

    Feulner, Georg 2009. Climate modelling of mass-extinction events: a review. International Journal of Astrobiology, Vol. 8, Issue. 03, p. 207.

  • Print publication year: 2005
  • Online publication date: November 2009

Chapter 5 - Effects of volcanic eruptions on the atmosphere and climate


The bright sun was extinguish'd and the stars

Did wander darkling in the eternal space,

Rayless, and pathless, and the icy earth

Swung blind and blackening in the moonless air;

Morn came and went – and came, and brought no day …

A section from “Darkness” by Lord Byron, written in June 1816 on the shores of Lake Geneva in the midst of the “Year without a Summer,” 14 months after the great eruption of the volcano Tambora in Indonesia.


Interest in the effects of volcanic activity on atmospheric phenomena, including the importance of volcanism in moderating climate and weather, has a long but patchy history, with the earliest recognition of a connection stretching back to classical times (Forsyth, 1988). The modern era of description began with the flood lava eruption from the Lakagígar (Laki) fissure in Iceland. Benjamin Franklin is usually attributed with being the first to make the connection between reports of an eruption in Iceland and an appalling “dry fog” (a sulfuric acid aerosol cloud) that hung over Europe in the summer of 1783 (Franklin, 1784; see also Thordarson and Self, 2003). From this point on, the role of volcanism in influencing and moderating our climate and weather has been a topic of debate (Self and Rampino, 1988; Robock, 2000) culminating in the past few decades with the need for a detailed understanding of natural influences on, and variability in, our atmosphere.

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