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Ozone in the White Mountains You've probably heard of ozone — a colorless gas that has been in the news a great deal — but did you know that there is good ozone and bad ozone? Good ozone occurs naturally in the earth's upper atmosphere, where it helps shield against the sun's damaging ultraviolet rays. Sadly, this good ozone has been depleted in some parts of the world due to pollution, forming an "ozone hole." Bad ozone forms in the lower atmosphere when pollutants from cars and smokestacks undergo chemical reactions in the presence of sunlight and high temperatures. This bad ozone is hazardous to human health and the environment and becomes a particular problem in the summer months. Hikers are especially vulnerable because ozone often accumulates at high elevations such as mountain summits, where air pollution transported by wind can build up. Also, hikers breathe air in more deeply, thereby increasing their exposure. The AMC is involved in efforts to monitor ozone in the White Mountains and to inform the public about ozone and what can be done about it. The Research The AMC's monitoring shows that ozone levels are often higher at higher elevations. Analysis of the AMC's long-term data reveals that the average daily ozone levels on Mount Washington's summit (approximately 6,288 feet) are two to five times higher than the lower-elevation sites at Camp Dodge and in Pittsburg (at approximately 1,500 feet and 1,368 feet respectively). This finding is consistent with other high-elevation sites where ozone is monitored, such as New York's Adirondack Mountains and the Great Smoky Mountains of Tennessee and North Carolina. There are several reasons for the elevated ozone levels at mountain summits. One is that ozone is transported to summits by wind from other regions where air pollution is great. (See a graphic showing wind patterns on clean-air days vs. high-smog days in the Northeast.) Another is that ozone does not dissipate as much at summits as it does below treeline, because there are fewer surfaces (such as trees, etc.) that come into contact with the ozone and break it down. Finally, there is less "mixing" of the air at high summits. In addition to having higher levels of ozone, higher summits tend to see ozone levels remain high for longer periods, in contrast to lower elevations where ozone levels tend to vary predictably over the course of the day. At lower elevations, the lowest ozone levels tend to occur in the morning and the highest in the afternoon (when temperatures are highest and the sun's rays are strongest). AMC researchers have found that these cyclical daily or "diurnal" patterns of ozone concentration hold true at the low-elevation Camp Dodge and Pittsburg monitoring sites, while at the Mount Washington summit site, ozone remains consistently high throughout the day, resulting in a higher background level that continues to build in extended pollution events. The AMC monitors ozone at the base and summit of Mount Washington 24 hours a day from late May through the end of September. As of September 2002, ozone levels at the AMC's monitoring sites were in compliance with current federal standards overall, although short-term levels on Mount Washington occasionally exceeded the health standards. In addition, a hiker-health study conducted by the AMC found that hikers suffer lung impairment even when ozone is within federally acceptable levels. What Can You Do? If you are active on days when ozone levels are high, be sure to reduce your exertion if you notice symptoms such as coughing, wheezing, tightness in the chest, and/or restricted breathing. In addition to these protective measures, since ground-level ozone originates in pollution from human activity, there are many steps we can each take as individuals to help reduce the problem year-round:
See the EPA's Website for more specific ideas on things that you can do to help reduce air pollution. |
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