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Northern Scandinavian Temperatures of the Past 2000 Years

Reference
Esper, J., Frank, D.C., Timonen, M., Zorita, E., Wilson, R.J.S., Luterbacher, J., Holzkamper S., Fischer, N., Wagner, S., Nievergelt, D., Verstege, A. and Buntgen, U. 2012. Orbital forcing of tree-ring data. Nature Climate Change: DOI 10.1038/NCLIMATE1589.
In a game-changing paper published in the online version of Nature Climate Change, Esper et al. (8 July 2012) provide convincing evidence that both the Medieval and Roman Warm Periods of 1000 and 2000 years ago, respectively, were warmer than the Current Warm Period has been to date, in spite of the fact that today's atmospheric CO2 concentration is some 40% greater than it was during those two earlier periods.

In setting the stage for their paradigm-altering work, the twelve researchers - hailing from Finland, Germany, Scotland and Switzerland - write that "solar insolation changes, resulting from long-term oscillations of orbital configurations (Milankovitch, 1941), are an important driver of Holocene climate," referencing the studies of Mayewski et al. (2004) and Wanner et al. (2008). In addition, they state that this forcing has been "substantial over the past 2000 years, up to four times as large as the 1.6 W/m2 net anthropogenic forcing since 1750," as suggested by the work of Berger and Loutre (1991). And on the basis of "numerous high-latitude proxy records," as they describe it, they note that "slow orbital changes have recently been shown to gradually force boreal summer temperature cooling over the common era," citing Kaufman et al. (2009).

Fast-forwarding to the present, Esper et al. describe how they developed "a 2000-year summer temperature reconstruction based on 587 high-precision maximum latewood density (MXD) series from northern Scandinavia," which feat was accomplished "over three years using living and subfossil pine (Pinus sylvestris) trees from 14 lakes and 3 lakeshore sites above 65°N, making it not only longer but also much better replicated than any existing MXD time series." Then, after calibrating the pine MXD series against regional June-July-August mean temperature over the period 1876-2006, they obtained their final summer temperature history for the period stretching from 138 BC to AD 2006, as depicted in the graph below.


Figure 1. The summer (June-July-August) temperature reconstruction of Esper et al. (2012), adapted from their paper.

As determined from the relationship depicted in the figure above, Esper et al. calculate a long-term cooling trend of -0.31 ± 0.03°C per thousand years, which cooling they say is "missing in published tree-ring proxy records" but is "in line with coupled general circulation models (Zorita et al., 2005; Fischer and Jungclaus, 2011)," which computational results portray, as they describe it: substantial summer cooling over the past two millennia in northern boreal and Arctic latitudes.

"These findings," as the European researchers continue, "together with the missing orbital signature in published dendrochronological records, suggest that large-scale near-surface air temperature reconstructions (Mann et al., 1999; Esper et al., 2002; Frank et al., 2007; Hegerl et al., 2007; Mann et al., 2008) relying on tree-ring data may underestimate pre-instrumental temperatures including warmth during Medieval and Roman times," although they suggest that the impacts of the omitted long-term trend in basic tree-ring data may "diminish towards lower Northern Hemisphere latitudes, as the forcing and radiative feedbacks decrease towards equatorial regions."

And so it is that the question for our day ought to be: Why was much of the CO2-starved world of Medieval and Roman times decidedly warmer (by about 0.3 and 0.5°C, respectively) than it was during the peak warmth of the 20th century? Clearly, the greenhouse effect of atmospheric CO2 - if it has not been grossly over-estimated - must currently be being significantly tempered by some unappreciated CO2- and/or warming-induced negative-feedback phenomenon (possibly of biological origin) to the degree that the basic greenhouse effect of Earth's rising atmospheric CO2 concentration cannot fully compensate for the decrease in solar insolation experienced over the past two millennia as a result of the "long-term oscillations of orbital configurations" cited by Esper et al. (2012).

Additional References
Berger, A. and Loutre, M.F. 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10: 297-317.

Esper, J., Cook, E. and Schweingruber, F. 2002. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science 295: 2250-2253.

Fischer, N. and Jungclaus, J.H. 2011. Evolution of the seasonal temperature cycle in a transient Holocene simulation: Orbital forcing and sea-ice. Climate of the Past 7: 1139-1148.

Frank, D., Esper, J. and Cook, E.R. 2007. Adjustment for proxy number and coherence in a large-scale temperature reconstruction. Geophysical research Letters 34: 10.1029/2007GL030571.

Hegerl, G.C., Crowley, T.J., Allen, M., Hyde, W.T., Pollack, H.N., Smerdon, J.E. and Zorita, E. 2007. Detection of human influence on a new, validated 1500-year temperature reconstruction. Journal of Climate 20: 650-666.

Kaufman, D.S., Schneider, D.P., McKay, N.P., Ammann, C.M., Bradley, R.S., Briffa, K.R., Miller, G.H., Otto-Bliesner, B.L., Overpeck, J.T., Vinther, B.M. and Arctic Lakes 2k Project Members. 2009. Recent warming reverses long-term Arctic cooling. Science 325: 1236-1239.

Mann, M.E., Bradley, R.S. and Hughes, M.K. 1999. Northern Hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations. Geophysical Research Letters 26: 759-762.

Mann, M.E., Zhang, Z.H., Hughes, M.K., Bradley, R.S., Miller, S.K., Rutherford, S. and Ni, F. 2008. Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia. Proceedings of the National Academy of Sciences USA 105: 13,252-13,257.

Mayewski, P.A., Rohling, E.E., Stager, J.C., Karlen, W., Maasch, K.A., Meeker, L.D., Meyerson, E.A., Gasse, F., van Kreveld, S., Holmgren, K., Lee-Thorp, J., Rosqvist, G. Rack, F., Staubwasser, M., Schneider, R.R. and Steig, E.J. 2004. Holocene climate variability. Quaternary Research 62: 243-255.

Milankovitch, M. 1941. Kanon der Erdbestrahlung und seine Anwendung auf das Eiszeitenproblem. Koniglich Serbische Akademie.

Wanner, H., Beer, J., Butikofer, J., Crowley, T.J., Cubasch, U., Fluckiger, J., Goosse, H., Grosjean, M., Joos, F., Kaplan, J.O., Kuttel, M., Muller, S.A., Prentice, I.C., Solomina, O., Stocker, T.F., Tarasov, P., Wagner, M. and Widmann, M. 2008. Mid- to late Holocene climate change: An overview. Quaternary Science Reviews 27: 1791-1828.

Zorita, E., Gonzlez-Rouco, F., von Storch, H., Montavez, J.P. and Valero, F. 2005. Natural and anthropogenic modes of surface temperature variations in the last thousand years. Geophysical Research Letters 32: 10.1029/2004GL021563.

Archived 1 August 2012