Presentation on theme: "Annular Modes of Extra- tropical Circulation Judith Perlwitz CIRES-CDC, University of Colorado."— Presentation transcript:
Annular Modes of Extra- tropical Circulation Judith Perlwitz CIRES-CDC, University of Colorado
Outline Definition and Perspective The Northern Hemisphere Annular Mode- signatures in atmospheric and surface variables The stratospheric connection The Southern Hemisphere Annular Mode Annular Modes and climate change Summary
What are modes of variability? Monthly or annular average of meteorological parameter like temperature, pressure or wind speed taken at observation stations worldwide Remove long-term mean =>Recurrent spatial patterns. These patterns, called modes, are believed to be the signatures of distinctive dynamical interactions.
Sea level pressure Northern Hemisphere Annular Mode pattern Time series
Perspectives North Atlantic Oscillation (NAO) Zonal Index Cycle (Annular Mode) 1st Empirical Orthogonal Function of SLP (Arctic Oscillation) Walker and Bliss (1932) Loon and Rogers (1978) Hurrell (1995) Rossby (1939) Namias (1950) Lorenz (1951) Kutzbach (1970) Trenberth (1981) Wallace and Gutzler (1981) Regional (pressure difference between stations in Portugal and Island ) Hemispheric (zonal mean wind at 55N) Hemispheric
SLP Portugal-Island NAO index Zonal wind 55N index Leading EOF SLP index Correlation between SLP at each grid point and:
Different Temporal Behavior of Annular Modes in Northern and Southern Hemisphere (Thompson and Wallace, 2000) Polar cap geopotential heights (north of 70N and 65N) for 50hPa and tropospheric fields respectively
Unprecedented Southern Hemisphere Major Sudden Warming in 2002
Annular Modes and natural and anthropogenic climate forcings
Observed and modeled trends of 500hPa heights [m] 1950 -1999 (Hoerling et al. 2001) About 50 % of the observed trend can be explained by slow, tropical ocean warming.
Change in tropospheric wave forcing Change in stratospheric meridional temperature gradient via Stratospheric volcanic aerosol Polar ozone depletion Increased greenhouse effect Lecture M. Wallace
NAM index in observation and in transient climate change simulations (Shindell et al, 1999) Significant increase of surface NAM index was found in the Middle Atmosphere (MA)- GCM, but not in a model without full stratospheric dynamics
Response to stratospheric ozone loss in the Southern Hemisphere (Gillett and Thompson, 2003) Strengthening of westerly flow from the stratosphere to the troposphere Cooling in the troposphere occurs one to two month after the maximum cooling in the stratosphere Model response agrees well with observations. Z 500hPa [m] DJF Z [m] T [K]
Summary Together with El Nino, the Northern and Southern Hemisphere annular modes have emerged as the leading patterns of variability of the global atmosphere. The annular modes are primarily extra- tropical phenomena with a deep barotropic, zonally symmetric structure. There is a strong coupling between the tropospheric and stratospheric annular modes. Future predictions indicate a trend towards positive phase of the Annular Mode indices due to increasing greenhouse effect and stratospheric polar depletion.
References Lecture M. Wallace: http://jisao.washington.edu/wallace/ncar_notes/http://jisao.washington.edu/wallace/ncar_notes/ Miller, R.L., G.A. Schmidt, and D.T. Shindell 2006. Forced annular variations in the 20th century Intergovernmental Panel on Climate Change Fourth Assessment Report models. J. Geophys. Res. 111, D18101, doi:10.1029/2005JD006323. Shindell, D.T., R.L. Miller, G.A. Schmidt, and L. Pandolfo 1999. Simulation of recent northern winter climate trends by greenhouse-gas forcing. Nature 399, 452-455, doi:10.1038/20905. Thompson, D. W. J., and J. M. Wallace, 2000: Annular modes in the extratropical circulation. Part I: Month-to-month variability. J. Climate, 13, 1000-1016. Thompson, D. W. J., and S. Solomon, 2002: Interpretation of Recent Southern Hemisphere Climate Change. Science, 296, 895-899. Gillett, N.P., and D.W.J. Thompson, 2003: Simulation of Recent Southern Hemisphere Climate Change. SCIENCE, 302(5643), 273-275, 10.1126/science.1087440. Baldwin, M. P., and T. J. Dunkerton, 1999: Propagation of the Arctic Oscillation from the stratosphere to the troposphere. J. Geophys. Res., 104, 30 937-30 946. Baldwin, M.P., and T.J. Dunkerton, 2001: Stratospheric Harbingers of Anomalous Weather Regimes. Science, 294, 581-584. Hoerling, M.P., J.W. Hurrell, and T. Xu, 2001: Tropical Origins for Recent North Atlantic Climate Change. Science, 292, 90-92. Thompson, D.W.J., M.P. Baldwin, and S. Solomon, 2005: Stratosphere-troposphere coupling in the Southern Hemisphere. J. Atmos. Sci., 62(3), 708-715. Thompson, D. W. J, and J. M. Wallace, 1998: The Arctic Oscillation signature in the wintertime geopotential height and temperature fields. Geophys. Res. Lett., 25, 1297-1300. Annular Mode web page: http://www.atmos.colostate.edu/ao/