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2 - Silvics of the circumpolar boreal forest tree species

Published online by Cambridge University Press:  12 January 2010

Herman H. Shugart
Affiliation:
University of Virginia
Gordon B. Bonan
Affiliation:
National Center for Atmospheric Research, Boulder, Colorado
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Summary

Introduction

The development of mechanistic approaches in the study of forest ecosystem dynamics over the past 16 years has increasingly drawn scientific attention to autecological characteristics of forest tree species. Model exercises have shown that emergent properties of forest ecosystems are predictable from interactions of species-specific life history attributes (e.g. Shugart 1984). This chapter presents silvical data for the dominant boreal tree species in the northern hemisphere to be used with ecosystem analysis and modeling studies of the circumpolar boreal forests. The selection of the species is based on distribution maps provided by Sokolov, Svyaseva & Kubly (1977) for the Eurasian species and by Fowells (1965) for the North American ones, as well as on boreal zone maps by Hämet-Ahti (1981). Fourteen tree species have been found to dominate the boreal zone in Fennoscandia and the USSR (Fig. 2.1); fifteen dominate North America. Section 2 of this chapter presents autecological reviews for the boreal tree species in Eurasia. Detailed reviews for the North American boreal tree species have been omitted since they are already available (e.g. Fowells 1965; Harlow, Harrar & White 1979) and because of publication limitations. However, North American boreal tree species have been included in Section 3 of this chapter, which provides species life-history data for parametrization of boreal forest simulation models. Data for silvics of the Eurasian boreal tree species have been extracted from both published and unpublished literature sources in six languages (Bulgarian, English, Finnish, German, Russian and Swedish) and have been collected according to the following scheme.

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Publisher: Cambridge University Press
Print publication year: 1992

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