NOy


 

Instrument:NOy
Principal Investigators:David W. Fahey Ru-Shan Gao
Organization:Aeronomy Laboratory
National Oceanic and Atmospheric Administration
R/E/AL6
325 Broadway
Boulder, CO 80303
University of Colorado, Boulder and NOAA/Aeronomy Laboratory
R/E/AL6
325 Broadway
Boulder, CO 80303
Co-Investigators:Steve Ciciora, John Holecek, Rich McLaughlin, Megan Northway, Peter Popp, Tom Thompson, Richard Winkler

Measurement Description: The NOy instrument has three independent chemiluminescence detectors for simultaneous measurements of NOy, NO2, and NO (see Figure 1). Each detector utilizes the reaction between NO in the sample with reagent O3. The NO/O3 reaction produces excited state NO2 which emits light of near 1µ m wavelength. Emitted photons are detected with a cooled photomultiplier tube. NOy is the sum of the individual reactive nitrogen oxide species present in the lower stratosphere:

NOy = NO + NO2 + HNO3 + 2N2O5 + ClONO2 + HO2 + HO2 + ...

 

Figure 1. Three channel NOy instrument layout. The internal components reside inside the ER-2 fuselage in the Q-bay. The external inlet is located approximately 48 cm below the Q-bay fuselage opening. The cooled detectors are Hamamatsu R1333 photomultiplier tubes.

Because NOy species other than NO do not respond in the chemiluminescence detector, NOy component species are reduced to NO by catalytic reduction on a gold surface with carbon monoxide (CO) acting as a reducing agent. Conversion efficiencies are > 90% at surface temperatures of 300°C. An NO signal representing NOy is then detected by chemiluminescence in the detector module. The catalyst is located outside the aircraft fuselage in order to avoid inlet line losses (see Figure 2). NO2 is photolytically converted to NO in a glass cell in the presence of intense UV light between 300 and 400 nm (see Figure 3). The conversion fraction is > 50% for a residence time of 1 s. The chemiluminescence detector detects NO as well as the additional NO from NO2. The third channel measures NO directly by passing the ambient sample through the detector module.

The response of each detector is checked several times in flight by standard addition of NO or NO2 calibration gas. The baseline of each measurement is determined in part by the addition of synthetic air that contains no reactive nitrogen. A continuous flow of water vapor is added directly to the sample flow in order to reduce the background signal in the detectors.

The sampling inlet for NOy is located outside the fuselage of the aircraft in a separate football-shaped housing (see Figure 2). The shape of the housing allows for the inertial separation of large aerosols (> 5 µm diameter) from the NOy inlet at the downstream end of the housing.

Figure 2. Cross-sectional view of the external inlet housing (see Figure 1) on the ER-2 aircraft, showing the sampling points for the total water, ozone, and NOy measurements and some components of the NOyand total water sampling lines.

 

Figure 3. The NO2 photolysis system using a Heraeus UV lamp and glass photolysis cell. Borosilicate glass and color glass filters remove unwanted UV and IR radiation from the lamp flux. Air from the fuselage is used to cool the cell in flight.

For smaller particles, the difference between the sample flow velocity in the inlet opening and the aircraft velocity cause ambient aerosol particles to be oversampled in the NOy inlet. This feature assists in the identification of aerosol particles that contain NOy.

 

Accuracy: < 20% plus precision
Detection Limit: < 0.1 ppbv NOy, < 0.02 ppbv NO, 0.1 ppbv NO2
Sample Time: 1 sec
Location on ER-2: Lower Q-bay rack

 

References:

Fahey, D. W., C. S. Eubank, G. Hübler, and F. C. Fehsenfeld,Evaluation of a catalytic reduction technique for the measurement of total reactive odd-nitrogen NOy in the atmosphere, J. Atmos. Chem.,3, 435-468, 1985.
Fahey, D. W., K. K. Kelly, G. V. Ferry, L. R. Poole, J. C. Wilson, D. M. Murphy, M. Loewenstein, and K. R. Chan,in situ aerosol measurements of total reactive nitrogen, total water, and aerosol in a polar stratospheric cloud in the Antarctic,J. Geophys. Res.,94, 11299-11315, 1989.
Fahey, D. W., E. R. Keim, E. L. Woodbridge, R.-S. Gao, K. A. Boering, B. C. Daube, S. C. Wofsy, R. P. Lohmann, E. J. Hintsa, A. E. Dessler, C. R. Webster, R. D. May, C. A. Brock, J. C. Wilson, R. C. Miake-Lye, R. C. Brown, J. M. Rodriguez, M. Loewenstein, M. H. Proffitt, R. M. Stimpfle, S. W. Bowen, and K. R. Chan,in situ observations in aircraft exhaust plumes in the lower stratosphere at midlatitudes, J. Geophys. Res., 100, 3065-3074, 1995.
Gao, R.-S., E. R. Keim, E. L. Woodbridge, S. J. Ciciora, M. H. Proffitt, and D. W. Fahey, New photolysis system for NO2 measurements in the lower stratosphere, J. Geophys. Res., 99, 20673-20681, 1994.
Kawa, S. R., D. W. Fahey, L. E. Heidt, W. H. Pollock, S. Solomon, D. E. Anderson, M. Loewenstein, M. H. Proffitt, J. J. Margitan, and K. R. Chan, Photochemical partitioning of the reactive nitrogen and chlorine reservoirs in the high latitude stratosphere, J. Geophys. Res., 97, 7905-7923, 1992. Kawa, S. R., D. W. Fahey, K. K. Kelly, J. E. Dye, D. Baumgardner, B. W. Gandrud, M. Loewenstein, G. V. Ferry, and K. R. Chan,The Arctic polar stratospheric cloud aerosol: Aircraft measurements of reactive nitrogen, total water, and particles, J. Geophys. Res., 97, 7925-7938, 1992.