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Crutzen, P.J.1
Grooß, J.-U.2
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Müller, R.4
Russell III, J.M.5
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10
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0000460015
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R. T. Clancy et al., J. Geophys. Res. 92, 3067 (1987); D. F. Strobel et al., ibid., p. 6691; J. Eluszkiewicz and M. Allen, ibid. 98, 1069 (1993).
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Clancy, R.T.1
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R. T. Clancy et al., J. Geophys. Res. 92, 3067 (1987); D. F. Strobel et al., ibid., p. 6691; J. Eluszkiewicz and M. Allen, ibid. 98, 1069 (1993).
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J. Geophys. Res.
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Strobel, D.F.1
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R. T. Clancy et al., J. Geophys. Res. 92, 3067 (1987); D. F. Strobel et al., ibid., p. 6691; J. Eluszkiewicz and M. Allen, ibid. 98, 1069 (1993).
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Eluszkiewicz, J.1
Allen, M.2
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0028564064
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R. L. Miller et al., Science 265, 1831 (1994); J. M. Price et al., Chem. Phys. 175, 83 (1993); T. G. Slanger, L. E. Jusinski, G. Black, G. E. Gadd, Science 241, 945 (1988).
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Miller, R.L.1
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15
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Price, J.M.1
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16
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0024219945
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R. L. Miller et al., Science 265, 1831 (1994); J. M. Price et al., Chem. Phys. 175, 83 (1993); T. G. Slanger, L. E. Jusinski, G. Black, G. E. Gadd, Science 241, 945 (1988).
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Slanger, T.G.1
Jusinski, L.E.2
Black, G.3
Gadd, G.E.4
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19
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1842322413
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The systematic errors for the MAHRSI OH observations are estimated to be +23%, -20%
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The systematic errors for the MAHRSI OH observations are estimated to be +23%, -20%.
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-
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21
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1842271503
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The HALOE team has done extensive checks on the version 18 data to determine the effects of data smoothing, transmission calculation errors, and other more subtle factors on the high-altitude feature, and they have found no reason to question their reality
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The HALOE team has done extensive checks on the version 18 data to determine the effects of data smoothing, transmission calculation errors, and other more subtle factors on the high-altitude feature, and they have found no reason to question their reality.
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23
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1842391948
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note
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3 observations above ∼55 km begin to be influenced by non-LTE (non-local thermodynamic equilibrium) effects, and the observations at 50 km altitude are currently near the highest altitude at which non-LTE effects can be safely ignored in the retrievals.
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-
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24
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1842314701
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3 data are estimated to be 15 to 20% at the present stage of data evaluation, whereas the precision of the data is estimated to be better than ±3%
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3 data are estimated to be 15 to 20% at the present stage of data evaluation, whereas the precision of the data is estimated to be better than ±3%.
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25
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1842385096
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3 is 8% or ∼0.2 ppmv
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3 is 8% or ∼0.2 ppmv.
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-
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27
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1842318541
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in preparation
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D. E. Siskind et al., in preparation.
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Siskind, D.E.1
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32
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1842355264
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We thank NASA for providing UARS Guest Investigator funding and C. Aellig for providing the MAS data. Supported in part by the Office of Naval Research and by the Atmospheric Remote Sensing and Assessment Project of the Strategic Environmental Research and Development Program
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We thank NASA for providing UARS Guest Investigator funding and C. Aellig for providing the MAS data. Supported in part by the Office of Naval Research and by the Atmospheric Remote Sensing and Assessment Project of the Strategic Environmental Research and Development Program.
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