NWS Air Quality FAQs
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COMMENT/QUESTION: I like the ozone map now available, but can't really use it. There is no "guidance" given on the explanatory page as to what is considered a high range and low range. Where can we get information on what are safe levels and what are not?

RESPONSE PROVIDED BY:
Chet Wayland, Manager
EPA’s AirNow Program

The ozone maps available as air quality forecasting guidance products represent concentrations of forecasted ground-level ozone. The guidance is used by state and local air quality forecasters to assist them in issuing Air Quality Index (AQI) forecasts. The AQI links air quality-- in this case, for ozone concentrations-- to health effects and cautionary language or interpretive guidance for individuals.

When ozone is the only pollutant affecting air quality, the risks to people’s health can be described from both short-term exposure to ozone (based on 1-hr averaged concentrations) and longer-term exposure to ozone (based on 8-hr average concentrations). EPA developed the following scale that relates shorter and longer-term exposure to the ambient ozone concentrations, in parts per billion (ppb), to health risk.

COMMENT/QUESTION: I found this service surfing around your website. Could someone please explain how the air quality in NYC could be so much better than the rest of the Northeast?

RESPONSE PROVIDED BY:
Ken Schere, Chief
Atmospheric Model Development Branch, Atmospheric Sciences Modeling Division
NOAA Research and EPA’s National Exposure Research Laboratory

By looking at ozone, it may seem as though the air quality is better in the middle of NYC than elsewhere around it. This is misleading though. Ozone is produced through a complex set of chemical reactions in the atmosphere. It needs the starting ingredients of nitrogen dioxide and hydrocarbons to make the reactions happen. These gases are emitted in copious amounts from urban areas, such as NYC. One usually finds higher ozone in a downwind direction from the urban area, since it takes a few hours for the chemical reactions to occur and form higher ozone concentrations. So the pollutant gases emitted within NYC may cause higher ozone to form a few hours downwind, such as in southern CT or Long Island . However, if the winds are calm, the ozone-forming reactions will occur closer to the urban source areas and cause ozone buildup in the urban cores.

A complicating factor is that one of the precursor gases emitted in urban areas, nitrogen oxide, also depletes ozone. The effect is most dramatic in the evening and overnight hours when there is little or no sunlight. The net effect of these chemical and transport processes often causes the ozone concentrations within the core of large urban areas to be lower than the surrounding areas. However the air is not "cleaner" here even if the ozone concentrations are lower. The urban core is bathed in the ozone precursor gases, which themselves can be irritating or in some cases, toxic. A host of other pollutants, including fine particles, are also released in the urban areas. And under conditions of light winds and stagnation, ozone too can build up within the urban cores.

National Weather Service
Office of Science and Technology
Page Author: Kenneth.Carey@noaa.gov
Technical problems: Shirley.Gunderson@noaa.gov
http://www.nws.noaa.gov/ost/air_quality/
Page last modified: November 21, 2005

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