Total volcanic stratospheric aerosol optical depths and implications for global climate change

By D. Ridley, S. Solomon, J. Barnes, V. Burlakov, T. Deshler, S. I. Dolgii, A. Herber, T. Nagai, Ryan Reynolds Neely, A. V. Nevzorov and 7 more. 2014

192 citations recorded by the source corpus.

Understanding the cooling effect of recent volcanoes is of particular interest in the context of the post‐2000 slowing of the rate of global warming. Satellite observations of aerosol optical depth above 15 km have demonstrated that small‐magnitude volcanic eruptions substantially perturb incoming solar radiation. Here we use lidar, Aerosol Robotic Network, and balloon‐borne observations to provide evidence that currently available satellite databases neglect substantial amounts of volcanic aerosol between the tropopause and 15 km at middle to high latitudes and therefore underestimate total radiative forcing resulting from the recent eruptions. Incorporating these estimates into a simple climate model, we determine the global volcanic aerosol forcing since 2000 to be −0.19 ± 0.09 Wm−2. This translates into an estimated global cooling of 0.05 to 0.12°C. We conclude that recent volcanic events are responsible for more post‐2000 cooling than is implied by satellite databases that neglect volcanic aerosol effects below 15 km.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/c2308f7f2d9d44cc52df8401ee3ad40516750b4a

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

  1. Andrew Gettelman
  2. Steven Ghan
  3. R. Easter
  4. D. Marsh
  5. Douglas E. Kinnison
  6. S. Solomon
  7. M. Mills
  8. A. Schmidt

In Global and Planetary Change

  1. Andrew Gettelman
  2. Steven Ghan
  3. R. Easter
  4. S. Solomon
  5. D. Marsh
  6. M. Mills
  7. A. Schmidt
  8. Ed Hawkins

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