{"id":251432,"date":"2017-06-15T16:51:38","date_gmt":"2017-06-15T20:51:38","guid":{"rendered":"http:\/\/www.rochester.edu\/newscenter\/?p=251432"},"modified":"2020-04-13T17:22:48","modified_gmt":"2020-04-13T21:22:48","slug":"ancient-ozone-levels-give-researchers-glimpse-future-effects-climate-change","status":"publish","type":"post","link":"https:\/\/www.rochester.edu\/newscenter\/ancient-ozone-levels-give-researchers-glimpse-future-effects-climate-change\/","title":{"rendered":"Ancient ozone levels provide a glimpse into future effects of climate change"},"content":{"rendered":"

As plants, animals, volcanoes, human beings, cars, and factories emit gases and particles into the atmosphere, invisible molecules in the air around us act as miniscule cleanup crews to remove this pollution.<\/p>\n

These tiny cleansers are known as oxidants and are crucial for maintaining climate and human health. In atmospheric science, they pack a powerful punch against pollutants: when oxidants chemically react with pollutants and greenhouse gases, they cleanse these pollutants from the atmosphere by altering them into biologically useful or easily dissolved agents, such as carbon dioxide or nitrates.<\/p>\n

In order to better understand the power of atmospheric oxidants\u2014and the factors that effect their ability to do their work\u2014Lee Murray, an assistant professor of earth and environmental sciences at the University of Rochester, developed a computer model that shows how the concentration of oxidants changes under different climate conditions and temperatures. Then Murray, along with colleagues at the University of Washington, Princeton, and Harvard, compared model data to analysis conducted at the University of Washington\u2019s lab on 100,000-year-old Greenland ice cores.<\/p>\n

Their surprising discoveries, recently published in the journal Nature<\/em><\/a>, led them to rethink what it is that controls oxidant levels.<\/p>\n

 <\/p>\n

https:\/\/www.rochester.edu\/newscenter\/wp-content\/uploads\/2017\/06\/Murray-oxidants-animation.mp4<\/a><\/video><\/div>\n

One year of simulated daily ozone levels from the last Ice Age, about 21,000 years before the present. Warmer colors such as red indicate greater amounts of ozone in the troposphere, the lowest part of the atmosphere. The background image is from the <\/em>National Oceanic and Atmospheric Administration<\/em> and shows surface topography for this period. (University animation \/ Lee T. Murray)<\/em><\/p>\n

 <\/p>\n

Atmospheric scientists had believed that levels of ozone\u2014one major oxidant\u2014in surface air rise as temperature increases. Water vapor, plants, and soil bacteria emissions contribute to the production of ozone, and because these increase as temperature warms, existing models of atmospheric chemistry typically find more ozone in warmer climates.<\/p>\n

What the ice core measurements implied, however, is that when the atmosphere underwent large temperature shifts, ozone levels were actually greater in colder periods than in warmer ones.<\/p>\n

How did 100,000 ice cores yield this information? And what might explain the unexpected finding?<\/p>\n

\u201cWe\u2019re interested in how the reactive composition of the atmosphere has changed over the past because it helps in determining how human activity might perturb the atmosphere into the future,\u201d Murray says. Murray draws on that atmospheric data to develop computer models that might help make these projections. And the better and more refined the data, the more confident he and other scientists can be in the predictive capacity of their models.<\/p>\n

Ice cores provide a 100,000-year-old climate record, starting with a warm period, continuing through a full Ice Age and ending at the present day, with several shorter periods of abrupt warming and cooling in between.<\/p>\n

In order to explain how ozone levels could be higher in colder than in warmer temperatures, the researchers had to figure out what factors were more influential than temperature effects on emissions in determining ozone levels.<\/p>\n

After comparing model and ice core data, the researchers proposed two new mechanisms that they hypothesize may affect the concentration of ozone.<\/p>\n

The first involves increased circulation of ozone between the troposphere\u2014the air around and above us where weather occurs\u2014and the stratosphere, directly above it.<\/p>\n

Ozone is \u201cgood up high, bad nearby.\u201d Stratospheric ozone\u2014where the so-called ozone layer is found\u2014is important for shielding harmful solar radiation and preventing cancer. Tropospheric ozone is a major oxidant that helps cleanse pollution from the atmosphere. However, when ozone is produced close to the Earth\u2019s surface (as with smog created from vehicle exhaust and power plants), it acts as a biological irritant that can lead to human health problems, ecosystem damage, and crop losses.<\/p>\n

\"graphic
Stratospheric ozone\u2014where the ozone layer is found\u2014is important for shielding against harmful solar radiation. Tropospheric ozone is a major oxidant that helps cleanse pollution from the atmosphere. However, ground-level or \u201cbad\u201d ozone (smog) is a biological irritant that can lead to human health problems, ecosystem damage, and crop loss. Emissions from cars, trucks, factories, and power plants are large contributors to bad ozone. (University illustration \/ Julia Joshpe)<\/em><\/figcaption><\/figure>\n

\u201cNatural abundances of oxidants are essential for life,\u201d Murray says. \u201cOne of the things that makes Earth\u2019s atmosphere unique is that it\u2019s a highly oxidizing environment that converts biological waste gases to useful nutrients. That said, when oxidant levels in the atmosphere get too high due to human activity, they try to cleanse us<\/em> from the atmosphere.\u201d<\/p>\n

Air circulates between the stratosphere and the troposphere, rising in the tropics and dropping back down at the poles, in a pattern known as the Brewer-Dobson circulation<\/a>. Several factors can speed up this circulation, including sea surface temperatures and natural- and human-induced greenhouse gas levels. Since most ozone is produced naturally in the higher-level stratosphere, if circulation speeds up, more ozone would be transported from the tropical stratosphere where it is primarily produced to the troposphere.<\/p>\n

\u201cThere is strong evidence showing that the Brewer-Dobson circulation became stronger during the last glacial maximum,\u201d says Qiang Fu, a professor of atmospheric sciences at the University of Washington. \u201cThat means there was less stratospheric ozone in the tropics but more in the high latitudes, and then more ozone going down from the stratosphere to the troposphere.\u201d<\/p>\n

A second possible explanation for the finding, researchers say, is a less-understood group of oxidants: halogens. These chemical compounds that include chlorine, iodine, and fluorine, have not been fully studied, but researchers suspect they could compete with, and therefore influence, the levels of other oxidants, including ozone.<\/p>\n

\u201cThe largest source of halogens is from sea salt, and we know from ice cores that sea salt is much higher in colder climates,\u201d says Becky Alexander, an associate professor of atmospheric sciences at the University of Washington.<\/p>\n

The researchers suspect that both factors act in tandem to affect oxidant levels during the big swings in Earth’s temperature. Recognizing the mechanisms that affect oxidant levels can help researchers see how human activities might then alter the natural levels of ozone oxidants present in the atmosphere.<\/p>\n

The research was funded by the National Science Foundation.<\/p>\n","protected":false},"excerpt":{"rendered":"

A computer model developed at Rochester, and used to compare model data to analysis on 100,000-year-old Greenland ice cores, has shown a surprising result.<\/p>\n","protected":false},"author":912,"featured_media":251502,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[116],"tags":[21782,18852,29502,32532,27132,23252,18572,16072],"class_list":["post-251432","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-sci-tech","tag-climate-change","tag-department-of-earth-and-environmental-sciences","tag-featured-post-side","tag-lee-murray","tag-natural-sciences","tag-planets","tag-research-finding","tag-school-of-arts-and-sciences"],"acf":[],"yoast_head":"\nAncient ozone levels provide a glimpse into future effects of climate change<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, 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