Impact of twilight gradients on the retrieval of mesospheric ozone from HALOE

Journal of Geophysical Research Atmospheres

Volumn 110, Issue 13, 2005, Pages

  Natarajan, Murali ^a   Deaver, Lance E ^a   Thompson, Earl ^b   Magill, Brian ^b  

^a NASA LANGLEY RESEARCH CENTER   (United States)

^b GATS INC   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ALGORITHMS; CONCENTRATION (PROCESS); MATHEMATICAL MODELS; MIXING; OZONE; PHOTOCHEMICAL REACTIONS;

ALGORITHM; MESOSPHERE; NITROGEN DIOXIDE; NITROGEN OXIDES; NUMERICAL METHOD; NUMERICAL MODEL; OZONE; SOLAR ACTIVITY; TWILIGHT;

EID: 33750445976     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/2004JD005719     Document Type: Article

References (15)

1. Allen, M., J. I. Lunine, and Y. L. Yung (1984), The vertical distribution of ozone in the mesosphere and lower thermosphere, J. Geophys. Res., 89, 4841-4872.
2. Boughner, R. E., J. C. Larsen, and M. Natarajan (1980), The influence of NO and CIO variations at twilight on the interpretation of solar occultation measurements, Geophys. Res. Lett., 7, 231-234.
3. Brühl, C., et al. (1996), Halogen Occultation Experiment ozone channel validation, J. Geophys. Res., 101, 10,217-10,240.
4. Byrne, G. D., and A. C. Hindmarsh (1975), A polyalgorithm for the numerical solution of ordinary differential equations, ACM Trans. Math. Soft., 1(1), 71-96.
5. Callis, L. B., M. Natarajan, J. D. Lambeth, and R. E. Boughner (1997), On the origin of midlatitude ozone changers: Data analysis and simulations for 1979-1993, J. Geophys. Res., 102, 1215-1228.
6. DeMore, W. B., et al. (1997), Chemical kinetics and photochemical data for use in stratospheric modeling, Evaluation number 12, JPL Publ., 97-4.
7. Gordley, L. L., et al. (1996), Validation of nitric oxide and nitrogen dioxide measurements made by the halogen occultation experiment for UARS platform, J. Geophys. Res., 101, 10,241-10,266.
8. McHugh, M., et al. (2003), Improved mesospheric temperature, water vapor and polar mesospheric cloud extinctions from HALOE, Geophys. Res. Lett., 30(8), 1440, doi:10.1029/2002GL016859.
9. Natarajan, M., E. E. Remsberg, and L. L. Gordley (2002), Ozone budget in the upper stratosphere: Model studies using the reprocessed LIMS and the HALOE data sets, Geophys. Res. Lett., 29(7), 1152, doi:10.1029/2001GL014262.
10. Newchurch, M. J., et al. (1996), Stratospheric NO and NO2 abundances from ATMOS solar-occultation measurements, Geophys. Res. Lett., 23, 2373-2376.
11. Russell, J. M., III, et al. (1988), Measurements of odd nitrogen compounds in the stratosphere by the ATMOS experiment on Spacelab 3, J. Geophys. Res., 93, 1718-1736.
12. Russell, J. M., III, et al. (1993), The halogen occultation experiment, J. Geophys. Res., 98, 10,777-10,797.
13. Sander, S. P., et al. (2000), Chemical kinetics and photochemical data for use in stratospheric modeling, Supplement to evaluation 12: Update of key reactions, Evaluation number 13, JPL Publ., 00-3.
14. Thomason, L. W., L. R. Poole, and T. Deshler (1997), A global climatology of stratospheric aerosol surface area density deduced from Stratospheric Aerosol and Gas Experiment II measurements: 1984-1994, J. Geophys. Res., 102, 8967-8976.
15. World Meteorological Organization (WMO) (1998), Scientific assessment of ozone depletion: 1998, Rep. 44, Global Ozone Res. and Monit. Proj., NASA Off. of Earth Sci., Washington, D. C.