Photographer David Villacrés’ Twitter feed is teeming with various types of landscape photographs— from city streets to starry night skies and enormous volcanoes. For the Ecuador-based Villacrés, his home country is his muse. “All you need is Ecuador” is a frequent hashtag on his posts. Primarily a nature photographer, he often photographs the Ecuadorian Andes, which is home to the country’s glaciers.
Two glacier-covered volcanoes in Chile are at yellow alert, the second phase on a four-color scale. At yellow alert, Nevados de Chillán and Villarrica volcanoes are under advisory, meaning they are exhibiting signs of instability. While they are currently on the lower end of the warning spectrum, the two are still among the highest-risk volcanoes in the country, with long histories of activity and eruptions. Shown in the images below, smoke can be seen drifting from the mouth of the snow-capped Villarrica volcano, a clear indicator of volcanic activity.
According to Chile’s National Geology and Mining Service, the two volcanoes became active approximately 650,000 years ago. However, their surfaces are marked by formations from postglacial (the period after the most recent glaciation) eruptions that have occurred over the last 10,000 years. Interactions between lava and ice have drastically altered the topographic features of the Nevados de Chillán and Villarrica volcanoes. Evidence shows glaciers and ice sheets slowed or halted the flow of lava from these volcanoes. The lava melted holes into glacial ice and rapidly cooled after encountering ice sheets. In the 20th century, more recent activity has resulted in 100 fatalities related to mudflows, or lahars, on the slopes of the Villarrica Volcano.
The Nevados de Chillán and Villarrica volcanoes pose imminent threats to the populations living in their shadows. At the base of both volcanoes are cities where tourism from summer vacation facilities and winter sports complexes has been successful. The communities living under the threat of active volcanoes constantly risk destruction from lahars, falling ash, and lava flows. Images of Nevados de Chillán from April 1, 2020 show the volcano puffing out smoke, a stark contrast to the serene images of the volcano on April 2. The difference in appearance of Nevados de Chillán in just this two-day period shows the variability of the volcanic activity.
GlacierHub has previously reported on Nevados de Chillán, posting about a change in alert level in October 2019. That article highlighted that the volcano had been upgraded to orange alert, which indicates a significant risk of eruption. This month’s yellow alert is an obvious de-escalation since GlacierHub’s last report on Nevados de Chillán. Continue to check GlacierHub for updates on this and other glacier-covered volcanoes.
In the second half of the 1800s, glaciers in the Alps rapidly shrunk in length, some by hundreds of meters. Their alarming retreat, documented in photographs, has often been a symbol of the human influence on global climate, as the accelerated melting aligned with increased production of industrial soot. But were there other factors that drove the rapid glacier recession in the Alps at the end of the Little Ice Age?
A new study in The Cryosphere led by Michael Sigl, a chemist and climatologist at the Paul Scherrer Institute (PSI) in Switzerland, challenges the notion that human-made industrial soot, or more formally black carbon, from European industrialization was primarily responsible for the observed deglaciation during the 15-year period between 1860 and 1875.
Based on their comparison of high-resolution black carbon deposition records from ice cores from the Colle Gnifetti glacier in the Swiss Alps and historical data of the changing lengths of major Alpine glaciers, the researchers discovered that “when black carbon concentrations started to significantly rise (around 1875), Alpine glaciers had already experienced 80 percent of their 19thcentury retreat, meaning that black carbon was not the first responsible for this retreat, contrary to what was suggested in a previous study,” team member Dimitri Osmont, a doctoral student at the PSI, told GlacierHub, referring to earlier research published in the Proceedings of the National Academy of Sciences of the United States of America.
“Of course, this doesn’t mean that black carbon didn’t contribute at all (especially during the 20th century when concentrations are significantly higher, and also today in the case of Himalayan glaciers), but it was not the first driver,” Osmont told GlacierHub.
Sigl further elaborated on the discrepancies between his team’s findings and that of previous research in discussion with GlacierHub. “If the glaciers had actually been forced to retreat by more abundant soot impurities in the snow, one would expect the glaciers’ retreat to have been synchronous with or slightly lagging increases in black carbon deposition. But we observe the exact opposite and conclude that other factors, predominantly volcanism, account for most of past glacier variability,” he said.
Volcanoes? Indeed, a series of massive volcanic eruptions in the early 1800s, like the catastrophic Mount Tambora in 1815 behind Europe’s Year Without a Summer, resulted in a few decades of cooler and wetter conditions conducive for the Alpine glaciers to surge and grow. Not to belittle the sheer devastation experienced locally and the socioeconomic effects of altered agricultural patterns across the globe, other positive takeaways of the eruptions included artistic inspiration for vibrant sunsets in J. M. W. Turner paintings, the backdrop of Mary Shelley’s Frankenstein, and the peak of larger glaciers in the Alps to phenomenal lengths in the middle of the 1850s.
The team argues that this more favorable atmosphere for the glaciers allowed them to grow to their peak size in the 1850s and that the rapid retreat from 1860 to 1875 was the glaciers simply returning to their “normal” size. They conclude that whatever role anthropogenic black carbon had in Alpine glacier retreat before 1875 was negligible in comparison to the natural decadal factors.
But other scientists disagree with their findings, including Thomas Painter, the author of the study whose hypothesis was tested and a principal scientist at NASA’s Jet Propulsion Laboratory in California. “Sigl et al. performed admirable work with their ice core analysis, and it is alone an important contribution to understanding deposition dynamics of atmospheric constituents,” Painter told GlacierHub. However, he found that the study “attacked a strawman argument that the glacier retreat in the 19th century predated the emergence of black carbon deposition and its additional absorption of sunlight in the snowpack.” He challenges this new study’s claims that they disprove his hypothesis. “The glaciers did start retreating from a cold period, but they then kept on strongly retreating to lengths not seen in the previous centuries, while air temperature and precipitation didn’t change sufficiently to cause this,” he said.
Regardless of the differing conclusions, none of the scientists from the recent study contacted by GlacierHub discounted the role of human activity on glacier retreat. “Just to be very clear, the study in no way neglects the generally significant contribution of anthropogenic emissions to the ongoing observed worldwide glacier retreat, but black carbon, at least for the alpine region, was not a major factor for the 19th century retreat,” stated Theo Jenk, another co-author of the study from PSI. Painter and Jenk’s colleagues are sure to butt heads further, but all in the name of sound scientific endeavor.
This week’s Photo Friday explores the Aleutian Islands in Alaska. The Aleutian Islands, which separate the Bering Sea from the Pacific Ocean, consist of a series of islands and islets that contain 40 active and 17 inactive volcanoes. These volcanic islands formed from the subduction of the Pacific tectonic plate beneath the North American tectonic plate, and some of the volcanoes are glaciated. Scientists have determined that many of the islands had glaciers at one period.
The Aleutian Islands are also part of the Alaska Maritime National Wildlife Refuge (AMNWR), which protects various seabird colonies. As the largest wildlife refuge in the United States, more seabirds nest on the islands than anywhere else in North America. Puffins, gulls, cormorants, cackling geese, and terns, among others, call the area home. See pictures of some of these birds and the Aleutian Islands from the air, land, and sea below.
From Xanterra: “Just 150 years ago, 150 glaciers graced these spectacular alpine summits. Only 25 remain large enough today to be considered ‘functional,’ say scientists who expect the park’s glaciers to vanish by 2030, with many disappearing before that. People heeding the advice to visit soon will find a variety of national park lodging and dining spots that are making environmental stewardship part of the park experience.”
From Journal of Applied Volcanology: “As populations around the world encroach upon the flanks of nearby volcanoes, an increasing number of people find themselves living at risk from volcanic hazards. How these individuals respond to the threats posed by volcanic hazards influences the effectiveness of official hazard mitigation, response, and recovery efforts. Ideally, those who are aware of the hazards and concerned should feel motivated to become better prepared; however, research repeatedly shows that an accurate risk perception often fails to generate adequate preparedness… This study explores the barriers that people in the Skagit Valley of Washington face when deciding whether or not to prepare for lahars as well as the impact of participation in hazard management on household preparedness behaviors.”
Read more about Washington’s lahar preparedness here.
How Changing Climate Affects Ecosystems
From Environmental Research Letters: “Climate change is undeniably occurring across the globe, with warmer temperatures and climate and weather disruptions in diverse ecosystems (IPCC 2013, 2014). In the Arctic and Subarctic, climate change has proceeded at a particularly breakneck pace (ACIA 2005)… However, climate warming is forecast to be even more extreme in the future. In order to predict the impacts of further global change, experiments have simulated these future conditions by warming the air and/or soil, increasing CO2 levels, altering nutrient fertilization, modifying precipitation, or manipulating snow cover and snowmelt timing (Elmendorf et al 2015, Wu et al 2011, Bobbink et al 2010, Cooper 2014). Changes in biodiversity at high latitudes are expected to have profound impacts on ecosystem functioning, processes, and services (Post et al 2009).”
Read more about how changing climate affects ecosystems here.