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Atmospheric ChemistryFrom its earliest days, NCAR has analyzed the makeup of the atmosphere and the human activities that change it. Only ultraprecise sensors can fully capture the ebb and flow of the atmosphere's constituents. NCAR has developed some of the world's most sensitive instruments for monitoring air chemistry and its changes over time. The center also works closely with other institutions on global projects to assess the validity of measurement techniques. Most of the chemicals that play large roles in our atmosphere, such as the greenhouse gas carbon dioxide, are called trace gases. They exist in tiny proportions--measured in parts per million, per billion, or even per trillion. Some of these gases form and dissolve in seconds, while others circle the globe for millennia.
NCAR uses a variety of tools to measure trace gases and aerosols. Whole air samplers SatellitesFrom space, sensors can intercept upward-flowing radiation and use it to obtain a global-scale picture of air chemistry. NCAR has collaborated with other labs and universities on two major instruments aboard NASA satellites:
Launched in 1999, MOPITT ( Measurements of Pollution in the Troposphere), senses infrared radiation, from which the distribution of carbon monoxide in thetroposphere, the lowest layer of the atmosphere, can be determined. Carbon monoxide persists in the atmosphere for several weeks, making it a good marker for pollution. Since its launch in 2004, HIRDLS (High Resolution Dynamics Limb Sounder) has been gearing up to gather fine-scale data on aerosols and 10 trace gases, including ozone and water vapor, from altitudes of 5 to 50 miles (8-80 km). Looking at Earth's limb (the edge of Earth from the satellite perspective), HIRDLS gathers information by measuring the infrared radiation emitted by atmospheric gases. Spectrometers Chromatographs Along with community collaborators, NCAR researchers often design special configurations of instruments for capturing the chemistry at work in such locations as an evergreen forest or a snow-covered polar site. Whether in the field or the laboratory, the goal is not only to measure the air as it is, but also to deduce the changes--some rapid, some slow--that keep the atmosphere's chemical makeup in constant flux. < previous | index | next >
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