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References

Austin, J., A three-dimensional coupled chemistry-climate model simulation of past stratospheric trends, J. Atmos. Sci., Submitted, 2000.

Austin, J., J.R. Knight, and N. Butchart, 2000a: Three-dimensional chemical model simulations of the ozone layer: 1979-2015. Q. J. R. Meteorol. Soc., 126, 1533-1556.

Austin, J., J.R. Knight, and N. Butchart, 2000b: Three-dimensional chemical model simulations of the ozone layer: 2015-2055. Q. J. R. Meteorol. Soc., In press.

Butchart, N., J. Austin, J.R. Knight, A.A. Scaife, and M.L. Gallani, 2000: The response of the stratospheric climate to projected changes in the concentrations of the well-mixed greenhouse gases from 1992 to 2051, J. Climate, 13, 2142-2159.

Cullen, M.J.P., 1993: The unified forecast/climate model, Meteorol. Mag., 122, 81-94.

Forster, P.M de F. and K.P. Shine, 1999: Stratospheric water vapour changes as a possible contributor to observed stratospheric cooling. Geophys. Res. Lett., 26, 3309-3312.

Gates, W.L. et al., 1999: An overview of the results of the Atmospheric Model Intercomparison Project (AMIP). Bull. Amer. Meteor. Soc., 80, 29-55.

Houghton,J.T., L.G. Meira Filho, B.A. Callander, N. Harris, A. Kattenberg, and K. Maskell (eds.)., 1996: Climate Change 1995, The Science of Climate Change, Cambridge University Press, Cambridge.

Langematz, U., 2000: An estimate of the impact of observed ozone losses on stratospheric temperature. Geophys. Res. Lett., 27, 2077-2080.

Oltmans, S.J. and D.J. Hofmann, 1995: Increase in lower-stratospheric water vapour at a mid-latitude northern hemisphere site from 1981-1994. Nature, 374, 146-149.

Pawson, S. et al., 2000: The GCM-reality intercomparison project for SPARC (GRIPS): Scientific issues and initial results. Bull. Am. Met. Soc., 81, 781-796.

Randel, W.J. and F. Wu. 1999: Cooling of the Arctic and Antarctic polar stratospheres due to ozone depletion. J. Clim., 12, 1467-1479.

Randel, W.J., F. Wu, J.M. Russell III, and A. Roche, 1998: Seasonal cycles and QBO variations in stratospheric CH$_4$ and H$_2$O observed in UARS HALOE data. J. Atmos. Sci., 55, 163-185.

Rosier, S. and K. Shine, 2000: The effect of two decades of ozone change on stratospheric temperature as indicated by a general circulation model. Geophys. Res. Lett., 27, In press.

Scaife, A.A., J. Austin, N. Butchart, S. Pawson, M. Keil, J. Nash, and I.N. James, 2000: Seasonal and interannual variability of the stratosphere diagnosed from UKMO TOVS analyses. Q.J.R. Meteorol. Soc., 126, 2585-2604.

Solomon, S., R.W. Portmann, R.R. Garcia, W. Randel, F. Wu, R. Nagatani, J. Gleason, L. Thomason, L.R. Poole, and M.P. McCormick, 1998: Ozone depletion at mid-latitudes: Coupling of volcanic aerosols and temperature variability to anthropogenic chlorine. Geophys. Res. Lett., 25, 1871-1874.

Stolarski, R.S., 1993: Monitoring stratospheric ozone from space. In: The role of the stratosphere in climate change. NATO ASI I8, Springer Verlag, 319-346.

World Meteorological Organization (WMO)/United Nations Environment Programme (UNEP), 1999: Scientific Assessment of Ozone Depletion: 1998, World Meteorological Organisation, Global Ozone Research and Monitoring Project -- Report No. 44, obtainable from WMO GLobal Ozone Observing System, PO Box 2300, 1211-Geneva-2, Switzerland.


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