Supervolcano eruption can change the periodic wind system in the tropical stratosphere
Lake Atitlán in Guatemala is a beautiful lake lying in the caldera formed due to the Los Chocoyos supervolcano eruption. The event had huge impacts to the atmospheric circulation in the tropics according to a new study.
Credit: Steffen Kutterolf/GEOMAR
The question of what happens in the atmosphere when a supervolcano erupts, has concerned scientists in atmospheric chemistry and meteorology for a while. Now, a research team from UiO, GEOMAR, NCAR, and MPI-M have worked together and come closer to an answer. They present their new findings in the journal Geophysical Research Letters.
The object of their interest happened ∼75,000 years ago in the Guatemalan highlands—the supervolcano eruptionLos Chocoyos. Today, the eruption site is an enormous caldera, the Atitlán Caldera (14.6°N, 91.2°W). The caldera, now a lake, lies about 1,563 meters abovesea level, fringed by three cone-shaped volcanoes: Atitlán, Tolimán, and San Pedro.
When the volcano once erupted it had the magnitude of eight, the highest ranking on theVolcanic Explosivity Index (VEI).
The most beautiful lake in the world
The German explorer and naturalist Alexander vonHumbolt (1769—1859) called it “the most beautiful lake in the world” (Wikipedia). The beauty of Lake Atitlán is well known, and today it is one of the landscape highlights in Guatemala, and a national and international tourist attraction. It is surrounded by small Mayan villages.
Despite the volcano now being dead, the caldera gives evidence of the power the eruption had in the past, recently described in a study: A history of violence: Magma incubation, timing, and tephra distribution of the Los Chocoyos supereruption (Atitlán Caldera, Guatemala) by Cisneros et al (2021) inJournal of Quaternary Science.
The eruption is known as one of the largest volcanic events of the past 100,000 years, and must have been an inferno of magma, explosions and outburst of gasses.
Release of chemical components to the atmosphere
Analyzed samples of deposits in geological layers after the event show that when the eruption happened, it also emitted enormous amounts of sulfur, chlorine and bromine to the atmosphere. Volcanic ash after the Los Chocoyos outburst is found several places in the Guatemalan highlands and in marine deposits from deep-sea cores in the Pacific, the Mexico Gulf and even in the Atlantic Ocean.
The research team had the hypothesis that such large emissions from the outburst would cause multi‐decadal consequences to the atmosphere and the global climate. But for how long? And what strength and volume would the emissions have?
To get any further on these questions the research team had to use simulation models that represent today’s knowledge of the climate system. With this approach, it allowed them to simulate the impact of a Los Chocoyos‐like eruption, and the effect of huge amounts of emissions to the atmosphere (Brenna et al 2020 ACP).
Long lasting disruption of zonal wind system
Of special interest was the effect the emission would have on the quasi‐biennial oscillation (QBO), an alternating change of every other year of zonal wind directions in the stratosphere in the tropics. The stratosphere is the second layer in the Earth’s atmosphere from approximately 15 to 50 km altitude.
“An eruption at this dimension would supply amounts of aerosols and chemistry components to the atmosphere, and according to our model simulations, the eruption would cause a ∼10 year disruption of the QBO wind,” says Kirstin Krüger, author of the study. “The change in the QBO would have started 4 months post-eruption, with abnormal easterly winds lasting ∼5 years, followed by westerlies wind, before it returned to normal QBO conditions, but with a slightly prolonged periodicity.”
This disruption of the wind system is a result of heating of air caused by aerosols, and a cooling effect caused by ozone depletion after the eruption. This heating vs. cooling interact with the propagation of atmospheric waves and evolved to disrupt the QBO.