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First Stage of Upper-stratospheric Ozone Recovery

First Stage of Upper-stratospheric Ozone Recovery. Mike Newchurch/UAH Eun-Su Yang/Georgia Tech Derek Cunnold/Georgia Tech Greg Reinsel/U Wisconsin, Madison Joe Zawodny/LaRC Jim Russell/Hampton U Presented at AGU Fall Meeting San Francisco, CA 12 December, 2003.

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First Stage of Upper-stratospheric Ozone Recovery

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  1. First Stage of Upper-stratospheric Ozone Recovery Mike Newchurch/UAH Eun-Su Yang/Georgia Tech Derek Cunnold/Georgia Tech Greg Reinsel/U Wisconsin, Madison Joe Zawodny/LaRC Jim Russell/Hampton U Presented at AGU Fall Meeting San Francisco, CA 12 December, 2003

  2. In the upper stratosphere, it’s the chlorine 25 yrs Stratospheric ballooning (Europe, Canada, USA) + Space Lab-3 ATMOS (1985) + ATLAS 1, 2, 3 (1992,3,4: ATMOS, MAS, SSBUV, SUSIM) + 30 yrs laboratory kinetics measurements + 30 yrs photochemical modeling + NASA, ESA, Japanese, Canada satellites (BUV, SBUV, SAGE I/II, TOMS, UARS, ADEOS, GOME, ACE, ENVISAT) + 50 yrs Ground-based RS: Dobson/Umkehr, many others + 20 yrs Ground-based in situ CFC & HCFC obs + Lower Stratospheric aircraft obs (ER2 campaigns) + 1000s of scientists thoughts and analyses → A very good understanding of Upper stratospheric chemistry: The Protocol is working on Chlorine

  3. Fahey et al., 20 questions, 2003 http://www.unep.org/ozone/faq.shtml

  4. Chlorine turning over @ sfc, slowing down @ 40 km Newchurch et al., 2003 Fahey et al., 20 questions, 2003 http://www.unep.org/ozone/faq.shtml See also Montzka, Cunnold, Remsberg

  5. What do we expect in ozone? 5 Stages of Recovery 1: Slowdown in loss rate 2: Minimum 3: Increasing ozone 4: Slowdown in increase 5: Full recovery WMO Ozone Assessment, 2003, fig 4-43

  6. Sensitivity of Future Changes in Ozone to Cly, H2O, and CH4. 50 Cly CH4 Cly  Cly  H2O 40 Altitude (km) Cly T 30 4 6 –2 2 0 Percent Change in Ozone circa 2010 (relative to 2000) Model Forcings Cly15% H2O1.0 ppm  CH4 0.1 ppm  T ~2 K  All forcings are based on an extrapolation of present trends. This extrapolation is perhaps most uncertain for H2O and CH4. Jucks and Salawitch, AGU Monographs, 2000

  7. The ozone trend model [O3]t =  + t + [Seasonal terms] + [QBO periodic terms] + γ [F10.7]t + Nt  is the mean level,  is a linear trend coefficient, the seasonal terms represent the 12-, 6-, 4-, and/or 3-months cosine terms each with a time lag See poster A41D-0718 by Yang et al. AGU Fall Meeting, 2003

  8. The ozone trend model [O3]t =  + t + [Seasonal terms] + [QBO periodic terms] + γ [F10.7]t + Nt  is the mean level,  is a linear trend coefficient, the seasonal terms represent the 12-, 6-, 4-, and/or 3-months cosine terms each with a time lag The Quasi Biennial Oscillation periodic terms consist of cosines with time lags to represent QBO signal with periods between 3 and 30 months excluding 12-, 6-, 4-,and/or 3-months terms. The traditional approach of using Singapore winds with a fitted lag produces similar results, but with less precise trend estimates and more fluctuations in the residuals.

  9. The ozone trend model [O3]t =  + t + [Seasonal terms] + [QBO periodic terms] + γ [F10.7]t + Nt  is the mean level,  is a linear trend coefficient, the seasonal terms represent the 12-, 6-, 4-, and/or 3-months cosine terms each with a time lag The QBO periodic terms consist of cosines with time lags to represent QBO signal with periods between 3 and 30 months excluding 12-, 6-, 4-,and/or 3-months terms. The traditional approach of using Singapore winds with a fitted lag produces similar results, but with less precise trend estimates and more fluctuations in the residuals. [F10.7]t is the F10.7-cm radio flux density which is used to provide a solar variation proxy. γ is a solar signal regression coefficient. Nt is the autocorrelated error term, for which a first order autoregressive process is assumed (Nt = a1Nt-1 + t). The t residuals, after removing the autoregressive component, a1Nt-1, are the residuals that are used to compute the cumulative sums of residuals described in Appendix B.

  10. The ozone trend model [O3]t =  + t + [Seasonal terms] + [QBO periodic terms] + γ [F10.7]t + Nt The ability to determine trend changes early with high confidence depends on: Data quality (ozone and proxies) Density of data coverage Quality of the model fitting

  11. Upper Stratosphere Lower Stratosphere Southern latitudes Tropics Northern latitudes

  12. Measurements above projected trend SAGE observations Northern Midlatitude Upper Stratosphere HALOE observations 2-σ confidence envelope Tropics Upper Stratosphere Southern Midlatitude Upper Stratosphere

  13. Presented at the National Press ClubWashington, D.C. July 29, 2003>100 news storiesLive TV, radio interviewsAll time high hit AGU, #1 2003 AAAS EurekAlert 40k hits (2x #2 story)Top 100 Discover story

  14. Conclusions • Ozone measurements by satellites and international ground stations show compelling evidence of the BEGINNING of the recovery of the ozone in the UPPER stratosphere.

  15. Conclusions • Ozone measurements by satellites and international ground stations show compelling evidence of the BEGINNING of the recovery of the ozone in the UPPER stratosphere. • The ozone amount is still DECREASING, but more slowly than before 1997.

  16. Conclusions • Ozone measurements by satellites and international ground stations show compelling evidence of the BEGINNING of the recovery of the ozone in the UPPER stratosphere. • The ozone amount is still DECREASING, but more slowly than before 1997. • The chlorine amounts (from CFC releases at the surface) are decreasing at Earth’s surface and increasing more slowly in the upper stratosphere as a result of the Montreal Protocol and its amendments.

  17. Conclusions • Ozone measurements by satellites and international ground stations show compelling evidence of the BEGINNING of the recovery of the ozone in the UPPER stratosphere. • The ozone amount is still DECREASING, but more slowly than before 1997. • The chlorine amounts (from CFC releases at the surface) are decreasing at Earth’s surface and increasing more slowly in the upper stratosphere as a result of the Montreal Protocol and its amendments. • Because Chlorine chemistry controls a significant amount of the ozone loss in the upper stratosphere, the Protocol is having the DESIRED EFFECT on the ozone layer, but full recovery is still decades away.

  18. Conclusions • Ozone measurements by satellites and international ground stations show compelling evidence of the BEGINNING of the recovery of the ozone in the UPPER stratosphere. • The ozone amount is still DECREASING, but more slowly than before 1997. • The chlorine amounts (from CFC releases at the surface) are decreasing at Earth’s surface and increasing more slowly in the upper stratosphere as a result of the Montreal Protocol and its amendments. • Because Chlorine chemistry controls a significant amount of the ozone loss in the upper stratosphere, the Protocol is having the DESIRED EFFECT on the ozone layer, but full recovery is still decades away. • Access to highly calibrated, long-term satellite measurements and international ground-based measurements was essential to detecting these small but important changes.

  19. Conclusions • Ozone measurements by satellites and international ground stations show compelling evidence of the BEGINNING of the recovery of the ozone in the UPPER stratosphere. • The ozone amount is still DECREASING, but more slowly than before 1997. • The chlorine amounts (from CFC releases at the surface) are decreasing at Earth’s surface and increasing more slowly in the upper stratosphere as a result of the Montreal Protocol and its amendments. • Because Chlorine chemistry controls a significant amount of the ozone loss in the upper stratosphere, the Protocol is having the DESIRED EFFECT on the ozone layer, but full recovery is still decades away. • Access to highly calibrated, long-term satellite measurements and international ground-based measurements was essential to detecting these small but important changes. • We are not out of the woods yet. We have been surprised before by atmospheric changes and must continue to carefully measure our atmosphere to avoid being surprised again, perhaps by climate-change interactions.

  20. Future ? • Is ozone recovering in the lower stratosphere? • What are the effects of global climate change on ozone recovery? • What observational capacity is necessary to adequately answer #1 and #2? • Measure ozone evolution • Measure climate changes

  21. http://nsstc.uah.edu/atmchem/ Support from NASA Earth Science Enterprise

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