Tag Archives: volcanology

European medieval monks, Japanese scribes, and Middle Eastern chroniclers all contributed to volcanology

Volcanoes are not often a topic on this blog, which is focused on emerging science and technology. However, stories featuring scientific information from unexpected sources has long been a fascination of mine and this April 5, 2023 news item on ScienceDaily shines a light on an unusual cast of medieval scientific observers spanning the globe,

By observing the night sky, medieval monks unwittingly recorded some of history’s largest volcanic eruptions. An international team of researchers, led by the University of Geneva (UNIGE), drew on readings of 12th and 13th century European and Middle Eastern chronicles, along with ice core and tree ring data, to accurately date some of the biggest volcanic eruptions the world has ever seen. Their results, reported in the journal Nature, uncover new information about one of the most volcanically active periods in Earth’s history, which some think helped to trigger the Little Ice Age, a long interval of cooling that saw the advance of European glaciers.

llumination from the late 14th or early 15th century, which portrays two individuals observing a lunar eclipse. It features the words «La lune avant est eclipsee», «The moon is eclipsed» in english. © Source gallica.bnf.fr / BnF Courtesy: Université de Genève

An April 5, 2023 Université de Genève (UNIGE) press release (also on EurekAlert), which originated the news item, includes observations from Japanese scribes along with those from medieval European monks and Middle Eastern scholars,

It took the researchers almost five years to examine hundreds of annals and chronicles from across Europe and the Middle East, in search of references to total lunar eclipses and their colouration. Total lunar eclipses occur when the moon passes into the Earth’s shadow. Typically, the moon remains visible as a reddish orb because it is still bathed in sunlight bent round the Earth by its atmosphere. But after a very large volcanic eruption, there can be so much dust in the stratosphere – the middle part of the atmosphere starting roughly where commercial aircraft fly – that the eclipsed moon almost disappears.

Medieval chroniclers recorded and described all kinds of historical events, including the deeds of kings and popes, important battles, and natural disasters and famines. Just as noteworthy were the celestial phenomena that might foretell such calamities. Mindful of the Book of Revelation, a vision of the end times that speaks of a blood-red moon, the monks were especially careful to take note of the moon’s coloration. Of the 64 total lunar eclipses that occurred in Europe between 1100 and 1300, the chroniclers had faithfully documented 51. In five of these cases, they also reported that the moon was exceptionally dark.

The contribution of Japanese scribes 

Asked what made him connect the monks’ records of the brightness and colour of the eclipsed moon with volcanic gloom, the lead author of the work, Sébastien Guillet, senior research associate at the Institute for environmental sciences at the UNIGE,  said: “I was listening to Pink Floyd’s Dark Side of the Moon album when I realised that the darkest lunar eclipses all occurred within a year or so of major volcanic eruptions. Since we know the exact days of the eclipses, it opened the possibility of using the sightings to narrow down when the eruptions must have happened.”

The researchers found that scribes in Japan took equal note of lunar eclipses. One of the best known, Fujiwara no Teika, wrote of an unprecedented dark eclipse observed on 2 December 1229: ‘the old folk had never seen it like this time, with the location of the disk of the Moon not visible, just as if it had disappeared during the eclipse… It was truly something to fear.’ The stratospheric dust from large volcanic eruptions was not only responsible for the vanishing moon. It also cooled summer temperatures by limiting the sunlight reaching the Earth’s surface. This in turn could bring ruin to agricultural crops.

Cross-checking text and data 

“We know from previous work that strong tropical eruptions can induce global cooling on the order of roughly 1°C over a few years,” said Markus Stoffel, full professor at the Institute for environmental sciences at the UNIGE and last author of the study, a specialist in converting measurements of tree rings into climate data, who co-designed the study. “They can also lead to rainfall anomalies with droughts in one place and floods in another.”

Despite these effects, people at the time could not have imagined that the poor harvests or the unusual lunar eclipses had anything to do with volcanoes – the eruptions themselves were all but one undocumented. “We only knew about these eruptions because they left traces in the ice of Antarctica and Greenland,” said co-author Clive Oppenheimer, professor at the Department of Geography at the University of Cambridge. “By putting together the information from ice cores and the descriptions from medieval texts we can now make better estimates of when and where some of the biggest eruptions of this period occurred.”

Climate and society affected 

To make the most of this integration, Sébastien Guillet worked with climate modellers to compute the most likely timing of the eruptions. “Knowing the season when the volcanoes erupted is essential, as it influences the spread of the volcanic dust and the cooling and other climate anomalies associated with these eruptions,” he said.

As well as helping to narrow down the timing and intensity of these events, what makes the findings significant is that the interval from 1100 to 1300 is known from ice core evidence to be one of the most volcanically active periods in history. Of the 15 eruptions considered in the new study, one in the mid-13th century rivals the famous 1815 eruption of Tambora that brought on ‘the year without a summer’ of 1816. The collective effect of the medieval eruptions on Earth’s climate may have led to the Little Ice Age, when winter ice fairs were held on the frozen rivers of Europe. “Improving our knowledge of these otherwise mysterious eruptions, is crucial to understanding whether and how past volcanism affected not only climate but also society during the Middle Ages,” concludes the researcher.

Here’s a link to and a citation for the paper,

Lunar eclipses illuminate timing and climate impact of medieval volcanism by Sébastien Guillet, Christophe Corona, Clive Oppenheimer, Franck Lavigne, Myriam Khodri, Francis Ludlow, Michael Sigl, Matthew Toohey, Paul S. Atkins, Zhen Yang, Tomoko Muranaka, Nobuko Horikawa & Markus Stoffel. Nature volume 616, pages 90–95 (2023) Issue Date: 06 April 2023 DOI: https://doi.org/10.1038/s41586-023-05751-z Published online: 05 April 2023

This paper is open access.

Café Scientifique (Vancouver, Canada) on climate change and rise of complex life on Nov. 24, 2015 and Member of Parliament Joyce Murray’s Paris Climate Conference breakfast meeting

On Tuesday, November 24, 2015 at 7:30 pm in the back room of The Railway Club (2nd floor of 579 Dunsmuir St. [at Seymour St.]), Café Scientifique will be hosting a talk about climate change and the rise of complex life (from the Nov. 12, 2015 announcement),

Our speaker for the evening will be Dr. Mark Jellinek.  The title of his talk is:

The Formation and Breakup of Earth’s Supercontinents and the Remarkable Link to Earth’s Climate and the Rise of Complex Life

Earth history is marked by the intermittent formation and breakup of “supercontinents”, where all the land mass is organized much like a completed jigsaw puzzle centered at the equator or pole of the planet. Such events disrupt the mantle convective motions that cool our planet, affecting the volcanic and weathering processes that maintain Earth’s remarkably hospitable climate, in turn. In this talk I will explore how the last two supercontinental cycles impelled Earth into profoundly different climate extreme’s: a ~150 million year long cold period involving protracted global glaciations beginning about 800 million years ago and a ~100 million year long period of extreme warming beginning about 170 million years ago. One of the most provocative features of the last period of global glaciation is the rapid emergence of complex, multicellular animals about 650 million years ago. Why global glaciation might stimulate such an evolutionary bifurcation is, however, unclear. Predictable environmental stresses related to effects of the formation and breakup of the supercontinent Rodinia on ocean chemistry and Earth’s surface climate may play a crucial and unexpected role that I will discuss.

A professor in the Dept. of Earth, Ocean and Atmospheric Sciences at the University of British Columbia, Dr. Jellinek’s research interests include Volcanology, Geodynamics, Planetary Science, Geological Fluid Mechanics. You can find out more about Dr. Jellinek and his work here.

Joyce Murray and the Paris Climate Conference (sold out)

Joyce Murray is a Canadian Member of Parliament, (Liberal) for the riding of Vancouver Quadra who hosts a regular breakfast meeting where topics of interest (child care, seniors, transportation, the arts, big data, etc.) are discussed. From a Nov. 13, 2015 email announcement,

You are invited to our first post-election Vancouver Quadra MP Breakfast Connections on November 27th at Enigma Restaurant, for a discussion with Dr. Mark Jaccard on why the heat will be on world leaders in Paris, in the days leading to December 12th,  at the Paris Climate Conference (COP 21).

After 20 years of UN negotiations, the world expects a legally binding universal agreement on climate to keep temperature increases below 2°C! The climate heat will especially be on laggards like Canada and Australia’s new Prime Ministers. What might be expected of the Right Honorable Justin Trudeau and his provincial premiers? What are the possible outcomes of COP21?

Dr. Jaccard has worked with leadership in countries like China and the United States, and helped develop British Columbia’s innovative Climate Action Plan and Carbon Tax.

Join us for this unique opportunity to engage with a climate policy expert who has participated in this critical global journey. From the occasion of the 1992 Rio Earth Summit resulting in the UN Framework Convention on Climate Change (UNFCCC), through the third Conference of Parties’ (COP3) Kyoto Protocol, to COP21 today, the building blocks for a binding international solution have been assembled. What’s still missing?

Mark has been a professor in the School of Resource and Environmental Management at Simon Fraser University since 1986 and is a global leader and consultant on structuring climate mitigation solutions. Former Chair and CEO of the British Columbia Utilities Commission, he has published over 100 academic papers, most of these related to his principal research focus: the design and application of energy-economy models that assess the effectiveness of sustainable energy and climate policies.

When: Friday November 27th 7:30 to 9:00AM

Where: Enigma Restaurant 4397 west 10th Avenue (at Trimble)

Cost: $20 includes a hot buffet breakfast; $10 for students (cash only please)

RSVP by emailing joyce.murray.c1@parl.gc.ca or call 604-664-9220

SOLD OUT!

They’re not even taking names for a waiting list. You can find out more about Dr. Jaccard’s work here.