Abstract
This paper presents a comparison of principal component (PC) regression and regularized expectation maximization (RegEM) to reconstruct European summer and winter surface air temperature over the past millennium. Reconstruction is performed within a surrogate climate using the National Center for Atmospheric Research (NCAR) Climate System Model (CSM) 1.4 and the climate model ECHO-G 4, assuming different white and red noise scenarios to define the distortion of pseudoproxy series. We show how sensitivity tests lead to valuable “a priori” information that provides a basis for improving real world proxy reconstructions. Our results emphasize the need to carefully test and evaluate reconstruction techniques with respect to the temporal resolution and the spatial scale they are applied to. Furthermore, we demonstrate that uncertainties inherent to the predictand and predictor data have to be more rigorously taken into account. The comparison of the two statistical techniques, in the specific experimental setting presented here, indicates that more skilful results are achieved with RegEM as low frequency variability is better preserved. We further detect seasonal differences in reconstruction skill for the continental scale, as e.g. the target temperature average is more adequately reconstructed for summer than for winter. For the specific predictor network given in this paper, both techniques underestimate the target temperature variations to an increasing extent as more noise is added to the signal, albeit RegEM less than with PC regression. We conclude that climate field reconstruction techniques can be improved and need to be further optimized in future applications.
Similar content being viewed by others
References
Ammann C, Joos F, Schimel D, Otto-Bliesner B, Tomas R (2007) Solar influence on climate during the past millennium: results from transient simulations with the NCAR Climate System Model. Proc Natl Acad Sci USA 104:3713–3718
Briffa K, Wigley T, Jones P, Pilcher J, Hughes M (1987) Patterns of tree-growth and related pressure variability in Europe. Dendrochronologia 5:35–59
Briffa K, Osborn T, Schweingruber F, Harris I, Jones P, Shiyatov S, Vaganov E (2001) Low-frequency temperature variations from a northern tree ring density network. J Geophys Res 106:2929–2942
Brohan P, Kennedy J, Harris I, Tett S, Jones P (2006) Uncertainty estimates in regional and global observed temperature changes: a new dataset from 1850. J Geophys Res 111:D12106
Buerger G, Cubasch U (2005) Are multiproxy climate reconstructions robust? Geophys Res Lett 32:L23711
Buerger G, Cubasch U (2007) On the verification of climate reconstructions. Clim Past 3:397–409
Casty C, Handorf D, Sempf M (2005a) Combined winter climate regimes over the North Atlantic/European sector 1766–2000. Geophys Res Lett 32:L13801
Casty C, Wanner H, Luterbacher J, Esper J, Bohm R (2005b) Temperature and precipitation variability in the European Alps since 1500. Int J Climatol 25:1855–1880
Casty C, Raible C, Stocker T, Wanner H, Luterbacher J (2007) European climate pattern variability since 1766. Clim Dyn 29:791–805
Cook E, Briffa K, Jones P (1994) Spatial regression methods in dendroclimatology: a review and comparison of two techniques. Int J Climatol 14:379–402
Esper J, Cook E, Schweingruber F (2002) Low-Frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science 295:2250–2253
Esper J, Wilson R, Frank D, Moberg A, Wanner H, Luterbacher J (2005) Climate: past ranges and future changes. Q Sci Rev 24:2164–2166
Esper J, Frank D, Buentgen U, Verstege A, Luterbacher J, Xoplaki E (2007) Long-term drought severity variations in Morocco. Geophys Res Lett 34:L17702
Fischer E, Luterbacher J, Zorita E, Tett S, Casty C, Wanner H (2007) European climate response to tropical volcanic eruptions over the last half millennium. Geophys Res Lett 34:L05707
González-Rouco J, Beltrami H, Zorita E, von Storch H (2006) Simulation and inversion of borehole temperature profiles in surrogate climates: Spatial distribution and surface coupling. Geophys Res Lett 33:L01703
Guiot J, Nicault A, Rathgeber C, Edouard J, Guibal F, Pichard G, Till C (2005) Last-millennium summer-temperature variations in western Europe based on proxy data. Holocene 15:489–500
Hegerl G, Crowley T, Hyde W, Frame D (2006) Climate sensitivity constrained by temperature reconstructions over the past seven centuries. Nature 440:1029–1032
Jansen E, coauthors (2007) Paleoclimate. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the International Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York
Jones P, Mann M (2004) Climate over past millennia. Rev Geophys 42:RG2002
Klimenko V, Klimanov V, Sirin A, Sleptsov A (2001) Climate changes in Western European Russia in the late Holocene. Doklady Earth Sci 377:190–194
Kuettel M, Luterbacher J, Zorita E, Xoplaki E, Riedeyl N, Wanner H (2007) Testing a European winter surface temperature reconstruction in a surrogate climate. Geophys Res Lett 34:L07710
Lee TCL, Zwiers FW, Tsao M (2007) Evaluation of proxy-based millennial reconstruction methods. Clim Dyn. doi:10.1007/s00382-007-0351-9
Li B, Nychka D, Ammann C (2007) The hockey stick and the 1990s: a statistical perspective on reconstructing hemispheric temperatures. Tellus 59A:591–598
Luterbacher J, Dietrich D, Xoplaki E, Grosjean M, Wanner H (2004) European seasonal and annual temperature variability, trends, and extremes since 1500. Science 303:1499–1503
Luterbacher J, et al. (2006) Mediterranean climate variability over the last centuries: a review. In: Lionello P, Malanotte-Rizzoli P, Boscolo R (eds) The Mediterranean Climate: an overview of the main characteristics and issues. Elsevier, Amsterdam, pp 27–148
Luterbacher L, Liniger M, Menzel A, Estrella N, Della-Marta P, Pfister C, Rutishauser T, Xoplaki E (2007) The exceptional European warmth of Autumn 2006 and Winter 2007: historical context, the underlying dynamics and its phenological impacts. Geophys Res Lett 34:L12704
Mangini A, Spötl C, Verdes P (2005) Reconstruction of temperature in the Central Alps during the past 2000 yr from a δ18O stalagmite record. Earth Planet Sci Lett 235:741–751
Mann M, Rutherford S (2002) Climate reconstruction using Pseudoproxies. Geophys Res Lett 29:1501
Mann M, Bradley R, Hughes M (1998) Global-scale temperature patterns and climate forcing over the past six centuries. Nature 392:779–787
Mann M, Bradley R, Hughes M (1999) Northern hemisphere temperatures during the past millennium: inferences, uncertainties, and limitations. Geophys Res Lett 26:759–762
Mann M, Gille E, Bradley R, Hughes M, Overpeck J, Keimig F, Gross W (2000) Global temperature patterns in pastcenturies: an interactive presentation. Earth Interact 4(1234):1–29
Mann M, Rutherford S, Wahl E, Ammann C (2005) Testing the fidelity of methods used in proxy-based reconstructions of past climate. J Clim 18:4097–4107
Mann M, Rutherford S, Wahl E, Ammann C (2007) Robustness of proxy-based climate field reconstruction methods. J Geophys Res 112:D12109
Moberg A, Sonechkin D, Holmgren K, Datsenko N, Karlen W (2005) Highly variable Northern Hemisphere temperatures reconstructed from low-and high-resolution proxy data. Nature 433:613–617
Moberg A, Mohammad R, Mauritsen T (2008) Analysis of the Moberg et al. (2005) hemispheric temperature reconstruction. Clim Dyn (accepted)
Pauling A, Luterbacher J, Wanner H (2003) Evaluation of proxies for European and North Atlantic temperature field reconstructions. Geophys Res Lett 30:1787
Pauling A, Luterbacher J, Casty C, Wanner H (2006) Five hundred years of gridded high-resolution precipitation reconstructions over Europe and the connection to large-scale circulation. Clim Dyn 26(4):387–405
Proctor C, Baker A, Barnes W (2002) A three thousand year record of North Atlantic climate. Clim Dyn 19:449–454
Rutherford S, Mann M, Osborn T, Bradley R, Briffa K, Hughes M, Jones P (2005) Proxy-Based Northern Hemisphere surface temperature reconstructions: sensitivity to method, predictor network, target season, and target domain. J Clim 18:2308–2329
Schneider T (2001) Analysis of incomplete climate data: estimation of mean values and covariance matrices and imputation of missing values. J Clim 14:853–871
Shabalova M, van Engelen A (2003) aluation of a reconstruction of winter and summer temperatures in the low countries, AD 764–1998. Clim Change 58:219–242
Shindell D, Schmidt G, Mann M, Rind D, Waple A (2001) Solar forcing of regional climate change during the maunder minimum. Science 294:2149–2152
Shindell D, Schmidt G, Miller R, Mann M (2003) Volcanic and solar forcing of climate change during the preindustrial era. J Clim 16:4094–4107
Shindell D, Schmidt G, Mann M, Faluvegi G (2004) Dynamic winter climate response to large tropical volcanic eruptions since 1600. J Geophys Res 109:D05104
Smerdon J, Kaplan A (2007) Comments on testing the fidelity of methods used in proxy-based reconstructions of past climate: the role of the standardization interval. J Clim 20(22):5666–5670
Thejll P, Schmith T (2005) Limitations on regression analysis due to serially correlated residuals: application to climate reconstruction from proxies. J Geophys Res 110:D18103
von Storch H, Zorita E, Jones J, Dimitriev Y, Gonzalez-Rouco F, Tett S (2004) Reconstructing past climate from noisy data. Science 306:679–682
von Storch H, Zorita E, Jones J, Gonzalez-Rouco F, Tett S (2006) Response to comment on reconstructing past climate from noisy data. Science 312:529–529
von Storch H, Zorita E, Gonzalez-Rouco F (2008) Assessment of three temperature reconstruction methods in the virtual reality of a climate simulation. Int J Earth Sci (submitted)
Wahl E, Ammann C (2007) Robustness of the Mann, Bradley, Hughes reconstruction of the Northern hemisphere surface temperatures: examination of criticisms based on the nature and processing of proxy climate evidence. Clim Change 85:33–69
Waple A, Mann M, Bradley R (2002) Long-term patterns of solar irradiance forcing in model experiments and proxy based surface temperature reconstructions. Clim Dyn 18:563–578
Wilks D (1995) Statistical methods in the atmospheric sciences. Academic Press, San Diego
Xoplaki E, Luterbacher J, Paeth H, Dietrich D, Steiner N, Grosjean M, Wanner H (2005) European spring and autumn temperature variability and change of extremes over the last half millennium. Geophys Res Lett 32:L15713
Acknowledgments
This work has been supported by the Swiss National Science Foundation (SNSF) through its National Center of Competence in Research on Climate (NCCR Climate) project PALVAREX 2. Publication cost contributions are kindly provided by the Foundation Marchese Francesco Medici del Vascello. We thank Caspar Ammann and Fortunat Joos for making available the NCAR CSM 1.4 results, as well as Fidel Gonzalez Rouco and Eduardo Zorita for providing the ECHO-G 4 simulation results. We also thank Scott Rutherford, Eugene Wahl and Michael E. Mann for the RegEM code and for their helpful comments and inputs. Finally, we wish to thank the reviewers for their constructive criticism and suggestions, which helped to improve the quality of this study.
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
382_2008_395_MOESM1_ESM.eps
Supplementary Figure 3 for ECHO-G 4. European summer average temperature anomalies (30-year running mean) wrt 1900 to 1990 AD, for PC regression (top) and RegEM (bottom), using 30 pseudoproxies (see Fig. 1) with varying white noise added to the signal. The target (black line) is compared to the reconstruction results (colored lines). (EPS 3.25 mb)
382_2008_395_MOESM7_ESM.eps
Supplementary Figure 5 for ECHO-G 4. European summer average temperatures anomalies (30-year running mean) for PC regression (top) and RegEM (bottom). The white noise scenario SNR 1 (red line) is compared with two different red noise scenarios (orange and magenta lines); the target is shown in black. (EPS 3.15 mb)
382_2008_395_MOESM9_ESM.eps
Supplementary Figure 7 for ECHO-G 4. Spatial skill patterns of the European summer temperature reconstructions using PC regression (left) and RegEM (right) with white noise scenarios SNR ∞, SNR 1, and SNR 0.5. The skill is defined by the average of the bias (reconstructed values - target values) [shaded] and RE [contours] calculated for each gridpoint over the verification period from 1001 to 1899 AD. The scale refers to the bias, i.e. differences in temperature anomalies for winter and summer separately. Colors indicate reconstructed values that are about (greenish blue and green), higher (light green, yellow to red) or lower (light blue to violet) than the target values. (EPS 5.67 mb)
382_2008_395_MOESM10_ESM.eps
Supplementary Figure 8 for ECHO-G 4. As supplementary Figure 7, but for winter. Colors indicate reconstructed values that are about (light blue and greenish blue), higher (light green to green, yellow, red) or lower (dark blue to violet) than the target values. (EPS 6.45 mb)
Rights and permissions
About this article
Cite this article
Riedwyl, N., Küttel, M., Luterbacher, J. et al. Comparison of climate field reconstruction techniques: application to Europe. Clim Dyn 32, 381–395 (2009). https://doi.org/10.1007/s00382-008-0395-5
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-008-0395-5