Modeling and understanding persistence of climate variability

[1] In this study, two parsimonious statistical representations of climate variability on interannual to multidecadal timescales are compared: the short-memory first order autoregressive representation (AR1) and the long-memory “power law” representation. Parameters for each statistical representation are fitted to observed surface air temperature at each spatial point. The parameter estimates from observations are found in general to be captured credibly in the Coupled Model Intercomparison Project 3 (CMIP3) simulations. The power law representation provides an upper bound and the AR1 representation provides a lower bound on persistence as measured by the lag-one autocorrelation. Both representations fit the data equally well according to goodness-of-fit-tests. Comparing simulations with and without external radiative forcings shows that anthropogenic forcing has little effect on the measures of persistence considered (for detrended data). Given that local interannual to multi decadal climate variability appears to be more persistent than an AR1 process and less persistent than a power law process, it is concluded that both representations are potentially useful for statistical applications. It is also concluded that current climate simulations can well represent interannual to multidecadal internal climate persistence in the absence of natural and anthropogenic radiative forcing, at least to within observational uncertainty.

[1]  Christian Franzke,et al.  Nonlinear Trends, Long-Range Dependence, and Climate Noise Properties of Surface Temperature , 2012 .

[2]  Peter J. Brockwell,et al.  Time Series , 2011, International Encyclopedia of Statistical Science.

[3]  Christian L. E. Franzke,et al.  Long-Range Dependence and Climate Noise Characteristics of Antarctic Temperature Data , 2010 .

[4]  D. Vyushin Statistical Approximation of Natural Climate Variability , 2010 .

[5]  T. Shepherd,et al.  On the statistical modeling of persistence in total ozone anomalies , 2010 .

[6]  Paul J. Kushner,et al.  On the origins of temporal power‐law behavior in the global atmospheric circulation , 2009 .

[7]  Paul J. Kushner,et al.  Power-Law and Long-Memory Characteristics of the Atmospheric General Circulation , 2009 .

[8]  Hans von Storch,et al.  Long‐term memory in 1000‐year simulated temperature records , 2008 .

[9]  Theodore G. Shepherd,et al.  Impact of long‐range correlations on trend detection in total ozone , 2007 .

[10]  S. Solomon The Physical Science Basis : Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change , 2007 .

[11]  K. Trenberth,et al.  Observations: Surface and Atmospheric Climate Change , 2007 .

[12]  A. Robertson,et al.  The Physical Basis for Predicting Atlantic Sector Seasonal-to-Interannual Climate Variability* , 2006 .

[13]  Klaus Fraedrich,et al.  Millennial climate variability: GCM‐simulation and Greenland ice cores , 2006 .

[14]  Peter Huybers,et al.  Links between annual, Milankovitch and continuum temperature variability , 2005, Nature.

[15]  A. Sterl,et al.  The ERA‐40 re‐analysis , 2005 .

[16]  Shlomo Havlin,et al.  Volcanic forcing improves Atmosphere‐Ocean Coupled General Circulation Model scaling performance , 2004, physics/0401143.

[17]  Klaus Fraedrich,et al.  Long time memory in global warming simulations , 2003 .

[18]  Klaus Fraedrich,et al.  Scaling of atmosphere and ocean temperature correlations in observations and climate models. , 2003, Physical review letters.

[19]  A Bunde,et al.  Power-law persistence and trends in the atmosphere: a detailed study of long temperature records. , 2003, Physical review. E, Statistical, nonlinear, and soft matter physics.

[20]  John M. Wallace,et al.  Stratospheric Connection to Northern Hemisphere Wintertime Weather: Implications for Prediction , 2002 .

[21]  A. Brix,et al.  Long memory in surface air temperature: detection, modeling, and application to weather derivative valuation , 2002 .

[22]  Donald B. Percival,et al.  Interpretation of North Pacific Variability as a Short- and Long-Memory Process* , 2001 .

[23]  S. Havlin,et al.  Detecting long-range correlations with detrended fluctuation analysis , 2001, cond-mat/0102214.

[24]  S. Feldstein The Timescale, Power Spectra, and Climate Noise Properties of Teleconnection Patterns , 2000 .

[25]  David B. Stephenson,et al.  Is the North Atlantic Oscillation a random walk , 2000 .

[26]  Makiko Sato,et al.  GISS analysis of surface temperature change , 1999 .

[27]  J. Elsner,et al.  Long-Range Correlations in the Extratropical Atmospheric Circulation: Origins and Implications , 1999 .

[28]  Jon D. Pelletier,et al.  Analysis and Modeling of the Natural Variability of Climate , 1997 .

[29]  Syukuro Manabe,et al.  Low-Frequency Variability of Surface Air Temperature in a 1000-Year Integration of a Coupled Atmosphere-Ocean-Land Surface Model , 1996 .

[30]  P. Robinson Gaussian Semiparametric Estimation of Long Range Dependence , 1995 .

[31]  Jan Beran,et al.  Statistics for long-memory processes , 1994 .

[32]  D. Nychka,et al.  Climate spectra and detecting climate change , 1992 .

[33]  J. Beran A Goodness‐Of‐Fit Test for Time Series with Long Range Dependence , 1992 .

[34]  P. Bloomfield Trends in global temperature , 1992 .

[35]  Richard A. Davis,et al.  Time Series: Theory and Methods (2nd ed.). , 1992 .

[36]  A test of fit in time series models , 1981 .

[37]  K. Hasselmann,et al.  Stochastic climate models , Part I 1 Application to sea-surface temperature anomalies and thermocline variability , 2010 .

[38]  K. Hasselmann Stochastic climate models Part I. Theory , 1976 .

[39]  H. E. Hurst,et al.  Long-Term Storage Capacity of Reservoirs , 1951 .