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  1. P. J. Crutzen, “The Influence of Nitrogen Oxides on the Atmospheric Ozone Content,” Q. J. R. Meteorol. Soc. 96, 320 (1970).
    [CrossRef]
  2. “Atmospheric Ozone1985, WMO Global Ozone Research and Monitoring Report, No. 16, (Geneva, World Meteorological Organization), see especially Appendix B: Spectroscopic Database, Infrared to Microwave.”
  3. H. K. Roscoe et al., “Intercomparison of Remote Measurements of Stratospheric NO and NO2,” in preparation, (1986).
  4. L. S. Rothman et al., “AFGL Trace Gas Compilation: 1982 Version,” Appl. Opt. 22, 1616 (1983).
    [CrossRef] [PubMed]
  5. C. Camy-Peyret, J.-M. Flaud, A. Perrin, K. Narahari Rao, “Improved Line Parameters for the ν3 and ν2 + ν3 − ν2 Bands of 14N16O2,” J. Mol. Spectrosc. 95, 72 (1982).
    [CrossRef]
  6. C. Camy-Peyret, J.-M. Flaud, J. Laurent, G. M. Stokes, “First Infrared Measurements of Atmospheric NO2 from the Ground,” Geophys. Res. Lett. 10, 35 (1983).
    [CrossRef]
  7. W. G. Mankin, “Airborne Fourier Transform Spectroscopy of the Upper Atmosphere,” Opt. Eng. 17, 39 (1978).
    [CrossRef]
  8. M. T. Coffey, W. G. Mankin, A. Goldman, “Simultaneous Spectroscopic Determination of the Latitudinal, Seasonal and Diurnal Variability of Stratospheric N2O, NO, NO2, and HNO3,” J. Geophys. Res. 86, 7331 (1981).
    [CrossRef]
  9. A. Perrin, J.-M. Flaud, C. Camy-Peyret, “Calculated Line Positions and Intensities for the ν1 + ν3 and ν1 + ν2 + ν3 − ν2 Bands of 14N16O2,” Infrared Phys. 22, 343, (1982).
    [CrossRef]
  10. V. Malathy Devi et al., “Tunable Diode Laser Spectroscopy of NO2 at 6.2 μm,” J. Mol. Spectrosc. 93, 179 (1982).
    [CrossRef]
  11. V. Malathy Devi, B. Fridovich, G. D. Jones, D. G. S. Snyder, A. Neuendorffer, “Temperatures Dependence of the Widths of N2-Broadened Lines of the ν3 Band of 14N16O2,” Appl. Opt. 21, 1537 (1982).
    [CrossRef]
  12. A. Goldman, F. G. Fernald, W. J. Williams, D. G. Murcray, “Vertical Distribution of NO2 in the Stratosphere as Determined from Balloon Measurements of Solar Spectra in the 4500 Å Region,” Geophys. Res. Lett. 5, 257 (1978).
    [CrossRef]

1983

C. Camy-Peyret, J.-M. Flaud, J. Laurent, G. M. Stokes, “First Infrared Measurements of Atmospheric NO2 from the Ground,” Geophys. Res. Lett. 10, 35 (1983).
[CrossRef]

L. S. Rothman et al., “AFGL Trace Gas Compilation: 1982 Version,” Appl. Opt. 22, 1616 (1983).
[CrossRef] [PubMed]

1982

C. Camy-Peyret, J.-M. Flaud, A. Perrin, K. Narahari Rao, “Improved Line Parameters for the ν3 and ν2 + ν3 − ν2 Bands of 14N16O2,” J. Mol. Spectrosc. 95, 72 (1982).
[CrossRef]

A. Perrin, J.-M. Flaud, C. Camy-Peyret, “Calculated Line Positions and Intensities for the ν1 + ν3 and ν1 + ν2 + ν3 − ν2 Bands of 14N16O2,” Infrared Phys. 22, 343, (1982).
[CrossRef]

V. Malathy Devi et al., “Tunable Diode Laser Spectroscopy of NO2 at 6.2 μm,” J. Mol. Spectrosc. 93, 179 (1982).
[CrossRef]

V. Malathy Devi, B. Fridovich, G. D. Jones, D. G. S. Snyder, A. Neuendorffer, “Temperatures Dependence of the Widths of N2-Broadened Lines of the ν3 Band of 14N16O2,” Appl. Opt. 21, 1537 (1982).
[CrossRef]

1981

M. T. Coffey, W. G. Mankin, A. Goldman, “Simultaneous Spectroscopic Determination of the Latitudinal, Seasonal and Diurnal Variability of Stratospheric N2O, NO, NO2, and HNO3,” J. Geophys. Res. 86, 7331 (1981).
[CrossRef]

1978

W. G. Mankin, “Airborne Fourier Transform Spectroscopy of the Upper Atmosphere,” Opt. Eng. 17, 39 (1978).
[CrossRef]

A. Goldman, F. G. Fernald, W. J. Williams, D. G. Murcray, “Vertical Distribution of NO2 in the Stratosphere as Determined from Balloon Measurements of Solar Spectra in the 4500 Å Region,” Geophys. Res. Lett. 5, 257 (1978).
[CrossRef]

1970

P. J. Crutzen, “The Influence of Nitrogen Oxides on the Atmospheric Ozone Content,” Q. J. R. Meteorol. Soc. 96, 320 (1970).
[CrossRef]

Camy-Peyret, C.

C. Camy-Peyret, J.-M. Flaud, J. Laurent, G. M. Stokes, “First Infrared Measurements of Atmospheric NO2 from the Ground,” Geophys. Res. Lett. 10, 35 (1983).
[CrossRef]

C. Camy-Peyret, J.-M. Flaud, A. Perrin, K. Narahari Rao, “Improved Line Parameters for the ν3 and ν2 + ν3 − ν2 Bands of 14N16O2,” J. Mol. Spectrosc. 95, 72 (1982).
[CrossRef]

A. Perrin, J.-M. Flaud, C. Camy-Peyret, “Calculated Line Positions and Intensities for the ν1 + ν3 and ν1 + ν2 + ν3 − ν2 Bands of 14N16O2,” Infrared Phys. 22, 343, (1982).
[CrossRef]

Coffey, M. T.

M. T. Coffey, W. G. Mankin, A. Goldman, “Simultaneous Spectroscopic Determination of the Latitudinal, Seasonal and Diurnal Variability of Stratospheric N2O, NO, NO2, and HNO3,” J. Geophys. Res. 86, 7331 (1981).
[CrossRef]

Crutzen, P. J.

P. J. Crutzen, “The Influence of Nitrogen Oxides on the Atmospheric Ozone Content,” Q. J. R. Meteorol. Soc. 96, 320 (1970).
[CrossRef]

Fernald, F. G.

A. Goldman, F. G. Fernald, W. J. Williams, D. G. Murcray, “Vertical Distribution of NO2 in the Stratosphere as Determined from Balloon Measurements of Solar Spectra in the 4500 Å Region,” Geophys. Res. Lett. 5, 257 (1978).
[CrossRef]

Flaud, J.-M.

C. Camy-Peyret, J.-M. Flaud, J. Laurent, G. M. Stokes, “First Infrared Measurements of Atmospheric NO2 from the Ground,” Geophys. Res. Lett. 10, 35 (1983).
[CrossRef]

C. Camy-Peyret, J.-M. Flaud, A. Perrin, K. Narahari Rao, “Improved Line Parameters for the ν3 and ν2 + ν3 − ν2 Bands of 14N16O2,” J. Mol. Spectrosc. 95, 72 (1982).
[CrossRef]

A. Perrin, J.-M. Flaud, C. Camy-Peyret, “Calculated Line Positions and Intensities for the ν1 + ν3 and ν1 + ν2 + ν3 − ν2 Bands of 14N16O2,” Infrared Phys. 22, 343, (1982).
[CrossRef]

Fridovich, B.

Goldman, A.

M. T. Coffey, W. G. Mankin, A. Goldman, “Simultaneous Spectroscopic Determination of the Latitudinal, Seasonal and Diurnal Variability of Stratospheric N2O, NO, NO2, and HNO3,” J. Geophys. Res. 86, 7331 (1981).
[CrossRef]

A. Goldman, F. G. Fernald, W. J. Williams, D. G. Murcray, “Vertical Distribution of NO2 in the Stratosphere as Determined from Balloon Measurements of Solar Spectra in the 4500 Å Region,” Geophys. Res. Lett. 5, 257 (1978).
[CrossRef]

Jones, G. D.

Laurent, J.

C. Camy-Peyret, J.-M. Flaud, J. Laurent, G. M. Stokes, “First Infrared Measurements of Atmospheric NO2 from the Ground,” Geophys. Res. Lett. 10, 35 (1983).
[CrossRef]

Malathy Devi, V.

Mankin, W. G.

M. T. Coffey, W. G. Mankin, A. Goldman, “Simultaneous Spectroscopic Determination of the Latitudinal, Seasonal and Diurnal Variability of Stratospheric N2O, NO, NO2, and HNO3,” J. Geophys. Res. 86, 7331 (1981).
[CrossRef]

W. G. Mankin, “Airborne Fourier Transform Spectroscopy of the Upper Atmosphere,” Opt. Eng. 17, 39 (1978).
[CrossRef]

Murcray, D. G.

A. Goldman, F. G. Fernald, W. J. Williams, D. G. Murcray, “Vertical Distribution of NO2 in the Stratosphere as Determined from Balloon Measurements of Solar Spectra in the 4500 Å Region,” Geophys. Res. Lett. 5, 257 (1978).
[CrossRef]

Narahari Rao, K.

C. Camy-Peyret, J.-M. Flaud, A. Perrin, K. Narahari Rao, “Improved Line Parameters for the ν3 and ν2 + ν3 − ν2 Bands of 14N16O2,” J. Mol. Spectrosc. 95, 72 (1982).
[CrossRef]

Neuendorffer, A.

Perrin, A.

A. Perrin, J.-M. Flaud, C. Camy-Peyret, “Calculated Line Positions and Intensities for the ν1 + ν3 and ν1 + ν2 + ν3 − ν2 Bands of 14N16O2,” Infrared Phys. 22, 343, (1982).
[CrossRef]

C. Camy-Peyret, J.-M. Flaud, A. Perrin, K. Narahari Rao, “Improved Line Parameters for the ν3 and ν2 + ν3 − ν2 Bands of 14N16O2,” J. Mol. Spectrosc. 95, 72 (1982).
[CrossRef]

Roscoe, H. K.

H. K. Roscoe et al., “Intercomparison of Remote Measurements of Stratospheric NO and NO2,” in preparation, (1986).

Rothman, L. S.

Snyder, D. G. S.

Stokes, G. M.

C. Camy-Peyret, J.-M. Flaud, J. Laurent, G. M. Stokes, “First Infrared Measurements of Atmospheric NO2 from the Ground,” Geophys. Res. Lett. 10, 35 (1983).
[CrossRef]

Williams, W. J.

A. Goldman, F. G. Fernald, W. J. Williams, D. G. Murcray, “Vertical Distribution of NO2 in the Stratosphere as Determined from Balloon Measurements of Solar Spectra in the 4500 Å Region,” Geophys. Res. Lett. 5, 257 (1978).
[CrossRef]

Appl. Opt.

Geophys. Res. Lett.

A. Goldman, F. G. Fernald, W. J. Williams, D. G. Murcray, “Vertical Distribution of NO2 in the Stratosphere as Determined from Balloon Measurements of Solar Spectra in the 4500 Å Region,” Geophys. Res. Lett. 5, 257 (1978).
[CrossRef]

C. Camy-Peyret, J.-M. Flaud, J. Laurent, G. M. Stokes, “First Infrared Measurements of Atmospheric NO2 from the Ground,” Geophys. Res. Lett. 10, 35 (1983).
[CrossRef]

Infrared Phys.

A. Perrin, J.-M. Flaud, C. Camy-Peyret, “Calculated Line Positions and Intensities for the ν1 + ν3 and ν1 + ν2 + ν3 − ν2 Bands of 14N16O2,” Infrared Phys. 22, 343, (1982).
[CrossRef]

J. Geophys. Res.

M. T. Coffey, W. G. Mankin, A. Goldman, “Simultaneous Spectroscopic Determination of the Latitudinal, Seasonal and Diurnal Variability of Stratospheric N2O, NO, NO2, and HNO3,” J. Geophys. Res. 86, 7331 (1981).
[CrossRef]

J. Mol. Spectrosc.

C. Camy-Peyret, J.-M. Flaud, A. Perrin, K. Narahari Rao, “Improved Line Parameters for the ν3 and ν2 + ν3 − ν2 Bands of 14N16O2,” J. Mol. Spectrosc. 95, 72 (1982).
[CrossRef]

V. Malathy Devi et al., “Tunable Diode Laser Spectroscopy of NO2 at 6.2 μm,” J. Mol. Spectrosc. 93, 179 (1982).
[CrossRef]

Opt. Eng.

W. G. Mankin, “Airborne Fourier Transform Spectroscopy of the Upper Atmosphere,” Opt. Eng. 17, 39 (1978).
[CrossRef]

Q. J. R. Meteorol. Soc.

P. J. Crutzen, “The Influence of Nitrogen Oxides on the Atmospheric Ozone Content,” Q. J. R. Meteorol. Soc. 96, 320 (1970).
[CrossRef]

Other

“Atmospheric Ozone1985, WMO Global Ozone Research and Monitoring Report, No. 16, (Geneva, World Meteorological Organization), see especially Appendix B: Spectroscopic Database, Infrared to Microwave.”

H. K. Roscoe et al., “Intercomparison of Remote Measurements of Stratospheric NO and NO2,” in preparation, (1986).

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Figures (2)

Fig. 1
Fig. 1

Observed spectra: (a) 2915-cm−1 region, (b) 1605-cm−1 region with spectral features used for analysis marked. The intensity scale is arbitrary.

Fig. 2
Fig. 2

NO2 column amounts above 12 km determined from sunset observations. Each point represents the average from an entire flight, typically twenty spectra. Error bars on the 2915-cm−1 observations represent one standard deviation; the standard deviations of the 1605-cm−1 observations are substantially smaller and fall within the plotted symbol.

Tables (1)

Tables Icon

Table I Details of the Apr. 1985 Aircraft Observations

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