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Central California Ozone Study (CCOS) - Desert Research Institute

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(e.g., HNO 3 , PAN, N 2 O 5 , HONO, and NO 3 ). Therefore the thermal catalytic method is used to<br />

measure NO, and then NO plus other nitrogen oxides as a group. If the group is not well defined, it<br />

is referred commonly as NO x , since the species included in the group depend on factors such as<br />

inlet and line losses and environmental factors. HNO 3 is most prone to line losses. Placing the<br />

converter as close to the sample inlet as possible minimizes these losses. Chemiluminescence<br />

analyzers that are configured in this manner are commonly known as NOy analyzers. NOy, or<br />

reactive nitrogen oxides, consists of a variety of species, the most abundant of which are NO,<br />

NO2, PAN and HNO 3 . TEI Model 42CY is configured with dual converters, which allows<br />

estimates of HNO3 by difference between the signals with and without an in-line nylon filter or<br />

NaCl impregnated fiber denuder.<br />

C.4 Supplemental Measurements of <strong>Ozone</strong><br />

Supplemental air quality measurements are needed during intensive operational periods<br />

(IOPs) in order to examine the three-dimensional distribution of ozone in the study area and to<br />

quantify some of the important species, other than those routinely monitored, which participate in<br />

ozone photochemistry.<br />

C.4.1 <strong>Ozone</strong>sondes<br />

In addition to atmospheric pressure, temperature, and moisture (relative humidity or wet<br />

bulb temperature), balloon-borne radiosondes can be equipped with instrumentation to measure the<br />

vertical distributions of ozone mixing ratios. <strong>Ozone</strong>sondes have lower quantifiable limit of less<br />

than 15 ppb with precision of ± 5 ppb or ± 10%.<br />

<strong>Ozone</strong>sondes provide ozone data that are averaged over short vertical distances and are<br />

thus nearly instantaneous measurements at a particular location. The data are only "snapshots" at<br />

each level of the atmosphere. As the radiosonde rises, it can be transported downwind, so<br />

measurements are not made above a fixed location. The typical response time of the instrument (><br />

80% of step change in 1 minute) may affect accuracy during ascent through sharp gradients in<br />

ozone mixing ratios. Balloon soundings usually can be made two to eight times per day on<br />

selected sampling days within reasonable budget contraints, but they are not cost-effective for<br />

long-term monitoring. Use of ozonesondes are most cost-effective when coupled to existing<br />

radiosonde releases.<br />

C.4.2 <strong>Ozone</strong> Aloft<br />

Lidar Measurements<br />

The Elight <strong>Ozone</strong> Profiler measure vertical ozone profiles starting at approx. 50 m up to<br />

2000 m with a detection limit of 1mg/m³ * m. This corresponds to a detection limit of 5µg/m³ with<br />

200 m range resolution. The system can be delivered as outdoor version with air-water cooling<br />

and with water-water cooling as indoor version. The optics and the electronics are integrated in an<br />

outdoors housing which allows system operation under different weather conditions. In the system<br />

a data analysis software package is implemented for the on-line determination of the ozone<br />

concentration as function of the height. This information can be delivered in form of ASII files or<br />

as graphical tables. Technical specification for the Elight <strong>Ozone</strong> Profiler is available at their web<br />

site at http://www.elight.de/profiler2.htm.<br />

C-8

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