Abstract
The hypothetico-deductive modelling framework introduced in Chap. 2 is applied to examining the effects of climatic change on the annual cycle of boreal and temperate trees. Most emphasis is devoted to the paradoxical hypothesis that climatic warming will increase the incidence of frost damage in these trees. According to early computer simulations, trees in boreal conditions in particular would deharden and even start to grow during such mild spells in winter as are commonly projected to prevail in the future climate, so that serious damage would result during subsequent periods of frost. Empirical tests of the frost damage hypothesis suggest that the catastrophic frost damage projected in the early computer simulations will not be realised. Even so, the frost damage hypothesis cannot be ruled out. Available experimental evidence remains limited, and theoretical work with computer simulations has shown that relatively small changes in the ecophysiological traits of trees may cause premature dehardening and growth onset during mild spells in the scenario climate. There have also been several reports of considerable frost damage to boreal and temperate trees and other plants in natural conditions after unseasonally warm spells in winter even in the present climate. For these reasons, nothing conclusive can be said about the frost damage hypothesis. However, the research discussed in this and other chapters of the present volume has pointed out not only the ecophysiological traits of the trees that are critical for the frost damage hypothesis but also the experimental designs that facilitate the determining of those traits in any tree population. Overall, the importance of ecophysiological realism and continuous critical testing of the models are emphasised. Finally, the implications of the effects of climatic change on tree seasonality to the stand and ecosystem level are briefly discussed.
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Notes
- 1.
- 2.
The approach is similar to that presented in Sect. 6.3.4, where the adaptation of different tree genotypes to the current climate was examined.
- 3.
In these diagnostic simulations, carried out at the whole-tree level only, the effects of the projected frost damage on the subsequent development of the trees were not addressed. Instead, a new annual cycle of frost hardiness was simulated even in cases where lethal frost damage had been projected. This diagnostic approach is mainly followed throughout this chapter. It goes without saying that when frost hardiness models are used as sub-models of large stand and ecosystem models, mortality and other, less drastic effects of frost damage on the subsequent development of the trees need to be addressed explicitly (Kellomäki et al. 1995; Kramer and Hänninen 2009; Chap. 7, Sect. 8.5.2).
- 4.
- 5.
- 6.
- 7.
- 8.
- 9.
In order to check the consistency of the results, a sensitivity analysis was carried out by using, in addition to the −8 °C, five alternative temperatures in the range of −5 to −10 °C as the threshold for killing frost. Use of the alternative threshold temperatures did not change the conclusions of the study.
- 10.
The contribution of Heikki Smolander is acknowledged here. He made this important point though he did not otherwise participate in the study.
- 11.
Unfortunately, Leinonen’s (1996) model has not been subjected to any such test in elevated temperature conditions as falsified Kellomäki et al.’s (1992, 1995) model (Fig. 8.16). However, a preliminary version of Leinonen’s (1996) model was found to predict the needle frost hardiness quite accurately in elevated temperature conditions, too (Leinonen et al. 1996). This provides some support for the projection of Leinonen’s (1996) model, i.e., for the projection that climatic warming will not increase the incidence of frost damage in boreal coniferous trees. It goes without saying, though, that ultimately the projections of Leinonen’s (1996) model, too, should be examined by testing the model in elevated temperature conditions.
- 12.
The valuation of environmental changes is ultimately a philosophical, not a scientific issue. Many environmentalists consider any human-induced environmental change negative by definition.
- 13.
The model of the annual cycle of photosynthetic capacity is discussed in Sect. 4.2.1.2.
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Hänninen, H. (2016). The Annual Cycle Under Changing Climatic Conditions. In: Boreal and Temperate Trees in a Changing Climate. Biometeorology. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-7549-6_8
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