Millennial reconstruction of the global terrestrial climate: New approaches to the available data

The main aim of the work was to reliably reconstruct the change in global temperature for the last 1000 years using new methods. We have considered two approaches to obtaining composite series based on symbolic analysis and on the so-called “principle of witnesses,” respectively. Based on the first approach, it has been indicated that the known reconstruction proposed by Moberg et al. is preferable in the scope of the accepted symbolic analysis variant among the available reconstructions. An approach based on the eyewitness principle made it possible to reveal the years when five different reconstructions give coordinated data on a 1000-year scale. The obtained new reconstructions are in good agreement with instrumental series data on the consistent time interval of their existence.

[1]  K. Briffa Annual climate variability in the Holocene: interpreting the message of ancient trees , 2000 .

[2]  Wolfram Bunk,et al.  Characterizing synchronization in time series using information measures extracted from symbolic representations. , 2008, Physical review. E, Statistical, nonlinear, and soft matter physics.

[3]  M. Hughes,et al.  Northern hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations , 1999 .

[4]  Leonard A. Smith,et al.  Combining dynamical and statistical ensembles , 2003 .

[5]  S. Lovejoy,et al.  Fractal characterization of inhomogeneous geophysical measuring networks , 1986, Nature.

[6]  Yu. A. Nagovitsyn,et al.  ESAI database and some properties of solar activity in the past , 2004 .

[7]  K. Briffa Erratum to “Annual climate variability in the Holocene: interpreting the message of ancient trees” [Quaternary Science Reviews, 19 (2000) 87–105] ☆ , 2000 .

[8]  P. Jones,et al.  Hemispheric and large-scale land-surface air temperature variations: An extensive revision and an update to 2010: LAND-SURFACE TEMPERATURE VARIATIONS , 2012 .

[9]  L. Karimovaa,et al.  Fractal and topological dynamics for the analysis of paleoclimatic records , 2006 .

[10]  T. P. Barnett,et al.  High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with General Circulation Model control-run temperatures , 1998 .

[11]  P. Jones,et al.  Hemispheric and Large-Scale Surface Air Temperature Variations: An Extensive Revision and an Update to 2001. , 2003 .

[12]  Crowley,et al.  Atmospheric science: Methane rises from wetlands , 2011, Nature.

[13]  K. Holmgren,et al.  Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data , 2005, Nature.

[14]  Edward R. Cook,et al.  Low-Frequency Signals in Long Tree-Ring Chronologies for Reconstructing Past Temperature Variability , 2002, Science.