Climate response to large, high‐latitude and low‐latitude volcanic eruptions in the Community Climate System Model

@article{Schneider2009ClimateRT,
  title={Climate response to large, high‐latitude and low‐latitude volcanic eruptions in the Community Climate System Model},
  author={David P. Schneider and Caspar Ammann and Bette L. Otto‐Bliesner and Darrell S. Kaufman},
  journal={Journal of Geophysical Research},
  year={2009},
  volume={114}
}
[1] Explosive volcanism is known to be a leading natural cause of climate change. The second half of the 13th century was likely the most volcanically perturbed half-century of the last 2000 years, although none of the major 13th century eruptions have been clearly attributed to specific volcanoes. This period was in general a time of transition from the relatively warm Medieval period to the colder Little Ice Age, but available proxy records are insufficient on their own to clearly assess… 

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References

SHOWING 1-10 OF 82 REFERENCES

Climatic response to high‐latitude volcanic eruptions

[1] Strong volcanic eruptions can inject large amounts of SO2 into the lower stratosphere, which over time, are converted into sulfate aerosols and have the potential to impact climate. Aerosols from

Dynamic winter climate response to large tropical volcanic eruptions since 1600

[1] We have analyzed the mean climate response pattern following large tropical volcanic eruptions back to the beginning of the 17th century using a combination of proxy-based reconstructions and

Mid- to Late Holocene climate change: an overview

Ice core and palaeoclimatic evidence for the timing and nature of the great mid‐13th century volcanic eruption

Ice cores from both the Arctic and Antarctic record a massive volcanic eruption in around AD 1258. The inter‐hemispheric transport of ash and sulphate aerosol suggests a low‐latitude explosive

Causes of climate change over the past 1000 years

  • Crowley
  • Environmental Science
    Science
  • 2000
A 21st-century global warming projection far exceeds the natural variability of the past 1000 years and is greater than the best estimate of global temperature change for the last interglacial.

Arctic Oscillation response to volcanic eruptions in the IPCC AR4 climate models

[1] Stratospheric sulfate aerosol particles from strong volcanic eruptions produce significant transient cooling of the troposphere and warming of the lower stratosphere. The radiative impact of

Volcanic and Solar Forcing of Climate Change during the Preindustrial Era

The climate response to variability in volcanic aerosols and solar irradiance, the primary forcings during the preindustrial era, is examined in a stratosphere-resolving general circulation model.

Pinatubo eruption winter climate effects: model versus observations

Large volcanic eruptions, in addition to the well-known effect of producing global cooling for a year or two, have been observed to produce shorterterm responses in the climate system involving

Volcanic forcing of climate over the past 1500 years: An improved ice core-based index for climate models

[1] Understanding natural causes of climate change is vital to evaluate the relative impacts of human pollution and land surface modification on climate. We have investigated one of the most

High‐latitude eruptions cast shadow over the African monsoon and the flow of the Nile

Nile River records indicate very low flow following the 1783–1784 Laki volcanic eruption, as well as after other high‐latitude volcanic eruptions. As shown by climate model simulations of the Laki
...