Central California Ozone Study (CCOS) - Desert Research Institute
Central California Ozone Study (CCOS) - Desert Research Institute
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