Global and Hemispherical Interannual Variation of Total Column Ozone from TOMS and OMI Data
- 1 Universidad Autónoma de Zacatecas, (UAEN), Ciprés 10, Fracc. La Peñuela, Zacatecas, México
- 2 Universidad Autónoma de Zacatecas, (UAEN), Ciprés 10, Fracc. La Peñuela, Zacatecas, México
- 3 Universidad Autónoma de Zacatecas, (UAEN), Ciprés 10, Fracc. La Peñuela, Zacatecas, México
- 4 Universidad Autónoma de Zacatecas, (UAEN), Ciprés 10, Fracc. La Peñuela, Zacatecas, México
- 5 Universidad Autónoma de Zacatecas, (UAEN), Ciprés 10, Fracc. La Peñuela, Zacatecas, México
Abstract
Daily Total Column Ozone (TCO) measurements compiled from Total Ozone Mapping Spectrometer (TOMS) and Ozone Monitoring Instruments (OMI) were used to analyze the global and hemispherical TCO interannual variations. Two periods of TCO measurements were analyzed separately covering full years. For the 1978-1994 period, the TCO showed a global decade decrease rate of 13.45 DU (about -4.3%). For the Northern Hemisphere(NH) the decade decrease rate was of 12.96 DU (-4.0%), while in the Southern Hemisphere (SH) was of 13.57 DU (-4.5%). These decreases in ozone trends, using the totality of TOMS and OMI satellite measurements, are greater than those reported in literature. The 1998-2014 period global TCO decade decrease rate was of 1.56 DU, corresponding 0.94 DU and 0.138 DU for the NH and SH, respectively. The global TCO variations must show a double annual periodicity, the first one with maxima in March due to the Northern Hemisphere (NH) and the second one during September due to the Southern Hemisphere (SH). However, the maxima due to SH TCO interannual variations have gradually vanished. A disturbance in the SH TCO interannual variations has appeared since 1980; graphically the periodicity brakes down and transforms to a double peak from 1985 and on. This effect can be attributed to the hemispheric impact of the ozone hole at the South Pole. Between October 1, 2004 and December 14, 2005 TOMS and OMI have recorded this disturbance unequivocally. We conclude that the disturbance in SH TCO has an irreversible character.
- Measurements. Report of the International Ozone Trends Panel 1988, 1, Chapter 4. http://www.esrl.noaa.gov/csd/assessments/ozone/1988/report.html.
- Molina, M.J. and Rowland, F.S. (1974) Stratospheric Sink for Chlorofluoro-methanes: Chlorine Atom-Catalyzed Destruction of Ozone. Nature, 249, 810-812. https://doi.org/10.1038/249810a0
- Farman, J.C., Gardiner, B.G. and Shanklin, J.D. (1985) Large Losses of Total Ozone in Antarctica reveal Seasonal Cl0x/NOx Interaction. Nature, 315, 207-210. https://doi.org/10.1038/315207a0
- WMO (1990) Scientific Assessment of Stratospheric Ozone: 1989, NO. 20.
- WMO (1995) Observed Changes in Ozone and Source Gases. Scientific Assessment of Ozone Depletion: 1994, NO. 37.
- WMO (2007) Global Ozone Research and Monitoring Project. Scientific Assessment of Ozone Depletion: 2006, NO. 50.
- WMO (2014) Assessment for Decision-Makers. Scientific Assessment of Ozone Depletion: Global Ozone Research and Monitoring Project, NO. 56.
- Nair, P.J., Godin-Beekmann, S., Kuttippurath, J., Ancellet, G., Goutail, F., Pazmino, A., Froidevaux, L., Zawodny, J.M., Evans, R.D. and Pastel, M. (2013) Ozone Trends Derived from the Total Column and Vertical Profiles at a Northern Mid-Latitude Station. Atmospheric Chemistry and Physics, 13, 10373-10384. https://doi.org/10.5194/acp-13-10373-2013
- Chehade, W., Weber, M. and Burrows, J.P. (2014) Total Ozone Trends and Variability during 1979-2012 from Merged Data Sets of Various Satellites. Atmospheric Chemistry and Physics, 14, 7059-7074. https://doi.org/10.5194/acp-14-7059-2014
- Douglass, A. and Fioletov, V. (2011) Stratospheric Ozone and Surface Ultraviolet Radiation. Scientific Assessment of Ozone Depletion: 2010. Global Ozone Research and Monitoring Project, Report No. 52, Chapter 2, WMO.
- Pinedo, J.L., Mireles-García, F., Ríos, C., García-Saldivar, V.M., Dávila-Rangel, J.I. and Espinosa, J.R. (2013) Assessment of the Latitudinal Behavior of Total Column Ozone at Nine Discrete 1o-Wide Latitude Bands, from TOMS and OMI Data. The Open Atmospheric Science Journal, 7, 92-108. https://doi.org/10.2174/1874282301307010092
- Cunnold, D.M., Yang, E.S., Newchurch, M.J., Reinsel, G.C., Zawodny, J.M and Russell III, J.M. (2004) Comment on ‘‘Enhanced Upper Stratospheric Ozone: Sign of Recovery or Solar Cycle Effect?’’ by Steinbrecht, W. et al. Journal of Geophysical Research, 109, D14305. https://doi.org/10.1029/2004jd004826