Volcanic eruptions and climate change!

By Kayode Adeoye   |   11 November 2015   |   5:14 am  

PHOTO: cdkn.org

PHOTO: cdkn.org

A volcanic eruption occurs when hot materials like lava, rocks, dust ash and gas escape from the earth’s crust through vents to the lithosphere. Some derisively refer to volcanic eruptions as Mother Nature’s way of farting! Due to the seriousness of the matter, the effects of climate change on the environment have been analyzed over the last two DrillBytes’ columns. In a report conducted by a team of geophysicists of the University of Geneva and released 31 August, 2015 (Estimates of volcanic-induced cooling in the Northern Hemisphere over the last 1,500 years), the analysis of the impact of volcanic eruptions over the climate was eruditely explained. This impact, which is the focus of the column this week, concludes DrillBytes’ trilogy on climate change.

Large volcanic eruptions inject considerable amounts of sulphure in the stratosphere which, once converted into aerosols, block sun rays and tend to cool the surface of the earth down for several years. An international team of researchers has just developed a method, published in Nature Geoscience, to accurately measure and simulate the induced drop in temperature. Considered the most important volcanic event of the 20th century, the eruption of Mount Pinatubo (June 1991) injected 29 million tons of sulphure dioxide in the stratosphere and provoked a global cooling of 0.40C on average.

To quantify the temporary cooling induced by the largest eruptions over the last 1,500 years, whose magnitude exceeded Mount Pinatubo’s, scientists usually adopt two approaches: Dendroclimatology which relies on the analysis of tree-ring based proxies and climate model simulations in response to the volcanic particles effect. But until now, these two approaches delivered results that were quite contradictory, and this prevented scientist from accurately assessing the impact of major volcanic eruptions on climate. Simulations showed greater (between two and four times higher) and longer cooling than dendroclimatic reconstructions. This gap even led some geophysicists to doubt the capacity of tree-ring based proxies to measure the impact of past major volcanic events in climate and to question the models’ ability in simulating precisely the climate response to strong volcanic impacts.

Reconstruction of observational proxy and model evidence Today, researchers from the University of Geneva (UNIGE), Switzerland, the Institut Pierre Simon Laplace, IRD, the French Alternative Energy Commission (CEA) and the national center for scientific research (CNRS), France have managed to reconcile the two approaches and developed a method to evaluate accurately the consequence of future high-magnitude eruptions on climate to better anticipate their impact on our societies.

In this multi-disciplinary team, dendrochronologists came up with a new reconstruction of the Northern Hemisphere summer temperature in the last 1,500 years. This reconstruction is mainly based on maximum latewood density, a parameter which is very sensitive to temperature variations. Data has been collected throughout the Northern Hemisphere from Scandinavia and Siberia all the way to Quebec, including Alaska, the Alps and the Pyrenees. The inclusion of density allowed clear detection of all major eruptions. Results show that the year following a large eruption is characterized by a greater cooling than asserted in previous reconstructions and that this cooling does not last for more than three years at an hemispheric scale.

In parallel, using a sophisticated climate model, climate physicists calculated the drop in temperature caused by the two largest volcanic events of the last millennium, the Samalas and Tambora eruptions which occurred in Indonesia in the years 1257 and 1815. This model combines data about location of volcanoes, the period of eruption, the amount of sulphure dioxide injected, and integration of results from a microphysical model which simulates the volcanic aerosol life cycle from their formation, following the oxidation of sulphure dioxide, to their sedimentation and elimination from the atmosphere. “This unusual approach enables us to realistically simulate the size of the volcanic aerosols particles and hence, their life expectancy in the atmosphere which directly influences both the extent and persistence of the cooling induced by an eruption”, explains Markus Stoffel, a researcher at UNIGE. These new simulations show that disruptions in ray exchange, caused by volcanic activity, were largely overestimated in previous climate simulations, used in the latest Inter-governmental Panel on Climate Change, IPCC report.

For the first time, results provided by reconstructions and climate models about the intensity of cooling converge and demonstrate that the Tampora and Samaras eruptions generated an average drop in temperature in the Northern Hemisphere fluctuating between 0.80C and 1.30C during the summer of year 1258 and year 1816. Both approaches also agree on the average persistence of the significant cooling which is estimated at two years to three years. These results pave the way to a better assessment of the role played by volcanism on climate change.

It is clear from the erudite submission that volcanic eruptions have a direct bearing on the temperature of the immediate environment which translates to changes in climatic conditions over time. Understanding our habitat to manage its challenges is the focus of the research.

•Kayode Adeoye is an oil and gas expert.

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