An international team led by 兔子先生传媒文化作品 researchers has cracked the chemical code driving the formation of iodine particles in the atmosphere, revealing how the element contributes to increased cloud cover and depletes molecules in the Earth鈥檚 protective ozone layer.
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The research, conducted at the world鈥檚 largest particle physics laboratory, the European Organization for Nuclear Research (CERN), was published today in the journal . It鈥檚 the first time that any experiment in the world has demonstrated the mechanism for how the gas-phase form of iodine鈥攌nown as iodic acid鈥攆orms, and suggests it has a听catalytic role in atmospheric particle formation.
It comes at a time when atmospheric iodine is increasing globally, with current levels triple what they were 70 years ago. Researchers hope that this new knowledge on iodine鈥檚 atmospheric interactions can be added to global atmospheric and climate models to help scientists better understand its environmental impacts鈥攕uch as increased cloud cover, which could exacerbate global warming-related thinning of Arctic sea ice.
Iodine is a common and highly reactive element, which can increase cloud cover and destroy ozone as a result of its听chemical interactions. Scientists now understand how iodic acid (HIO3) forms in the atmosphere.听(Credit: Henning Finkenzeller)听
鈥淭his paper establishes a link between the sources of iodine, how they are emitted into the atmosphere, and particle formation, which through subsequent growth, seeds clouds,鈥� said Rainer Volkamer, co-lead author on the paper, professor of chemistry at 兔子先生传媒文化作品 and (CIRES). 鈥淭hat link didn't exist before, and now we have established that link at the molecular level."
This link between iodine sources and atmospheric particle formation is a multi-step process. First iodine oxide radicals bond with themselves, then react with ozone and water to make iodic acid, with (singlet) oxygen and hypoiodous acid as co-products.
Iodine is a common and highly reactive element that forms radical species which undergo rapid chemical reactions lasting seconds to minutes in the atmosphere. Most iodine found in the atmosphere comes from the ocean鈥攚here it exists as iodide, also present in table salt. Its three-fold increase in the atmosphere over the past 70 years is linked to an increase in anthropogenic air pollution: as harmful, ground-level ozone reacts with the ocean-based iodide, it releases volatile iodine gasses to the atmosphere.
While iodine has been studied for 150 years, it is only in the past two decades that researchers such as Volkamer have revealed its important role within the atmosphere. In 2020, Volkamer and 兔子先生传媒文化作品 and CIRES researchers published research showing how iodine reaches the stratosphere and eats away at the ozone that protects the planet from harmful UV radiation.
鈥淚odine is the new kid on the block, among other halogens, that play into the recovery of the ozone layer,鈥� said Volkamer.
The Cosmics Leaving Outdoor Droplets (CLOUD) experiment at CERN, Geneva uses an ultraclean chamber facility to study how gases form new particles (nucleation), and grow to affect cloud formation. The primary goal of CLOUD is to understand the influence of galactic cosmic rays (GCRs) on aerosols and clouds, and their implications for climate. (Credit: CERN)听
DisCERNing chemical processes
To study this missing link, the research team turned to CERN, home to the pristine conditions required to observe and collect data on these particles. Here, 听(Cosmics Leaving Outdoor Droplets) has become the world鈥檚 leading laboratory experiment to study the remaining poorly understood aspects of aerosol and cloud formation.
Volkamer鈥檚 research group, the Atmospheric Trace Molecule Spectroscopy (ATMOSpec) Lab, is one of only three universities in the U.S. (along with Caltech and Carnegie Mellon University) who are part of this collaboration, along with 16 European partners.听
鈥淭his is the only such experiment that exists in the world,鈥� said Volkamer. 鈥淚t's an honor to be part of the collaboration and to be leading it in the context of a study like this one.鈥�
In the CLOUD chamber at CERN, the researchers had access to a laboratory environment with perfect control over conditions like temperature, pressure, humidity, ozone concentration, and iodine concentration, as well as access to different light sources resembling different aspects of the solar spectrum.
By setting up this artificial, indoor atmosphere where certain reactions may or may not happen, the scientists could accurately gather data on iodine chemical reactions that form and grow particles.
鈥淭his is a great example of experiments and computations coming together to answer a question that neither of them could have answered on their own,鈥� said , co-lead author on the study and professor of chemistry at the University of Helsinki.
To determine whether what they observed in the laboratory translated to the real world, they also tested their findings in the air surrounding the Ma茂do observatory on R茅union Island in the southern Indian Ocean鈥攁 remote location free of much of the influence of human activity鈥攁nd were able to corroborate their laboratory results.
A catalytic role on climate
Unlike other elements such as sulfur (or sulfuric acid), iodine doesn鈥檛 need the help of other molecules (known as 鈥渂ases鈥�) to form atmospheric particles. It鈥檚 also quite efficient at this process, compared to other elements, the researchers found.
Therefore, the formation of particles from iodic acid is not limited to coastal iodine hot spots, or locations where these chemical bases are available, but rather can occur throughout the atmosphere.
鈥淚t鈥檚 a global phenomenon, and the global significance of iodine in particle formation may be bigger than currently thought,鈥� said Henning Finkenzeller, first author on the study, a part of his dissertation at 兔子先生传媒文化作品.
Iodine is also fundamentally different from other particle-forming vapors, said Finkenzeller, because of its ability to kick-start the formation of atmospheric particles, and the fact that one iodine atom can kick-start this process multiple times. This catalytic role in particle formation enhances its effects in the atmosphere wherever it goes, whether that role is eliminating protective ozone molecules or increasing cloud cover.
As human activity increases the availability of iodine in the atmosphere, due to our negative impacts on air quality around the world, this short-lived element鈥檚 impacts may be long-lasting. As sea ice melts in the Arctic, more iodine can enter the atmosphere, increase cloud cover and enhance warming effects on the region. And in the tropics, storms can send this iodine high into the atmosphere, where it impacts our protective ozone layer.
鈥淲e still need to better understand iodine recycling chemistry. But now that we understand the source mechanism, we are one step closer to understanding how excess iodine impacts particle formation, clouds and ozone recovery in our planet's atmosphere,鈥� said Volkamer.听
As a global leader in climate, environmental and energy research, the University of Colorado Boulder is partnering with United Nations Human Rights to co-host the Right Here,听Right Now Global Climate Summit in fall 2022.听
