Abstract

We conducted dendroclimatological study on three dominant conifer tree species, Pinus koraiensis, Larix olgensis, and Picea jezoensis, in northeastern China for a better understanding of climate change impacts on temperate forest growth, by discussing the radial growth relationships of these tree species and projecting their radial growth trends under the future climate change scenarios. Based on the tree-ring samples collected from the upper altitude of Changbai Mountain, ring width chronologies were built to examine the growth relationships, and regression equations were established to project the future growth of the species under future climate change projected by the five general circulation models (GCMs) and four representative concentration pathway (RCP) scenarios. Although both temperature and precipitation showed varying degrees of relationships with growth of these three tree species, the limiting climate factors were species-specific. The tree-ring growth of P. koraiensis was limited by the summer temperature and precipitation at the end of growth, namely, significant positive correlations with the current July temperature and the previous September precipitation. Growth of L. olgensis was limited by the temperature before growing season, for its chronology was negatively correlated with the current February and previous December temperature (p < 0.05). The climatic conditions before and after growing season seemed to be the limiting factors of P. jezoensis growth, which was negatively correlated with the current February to April temperature and the current September temperature (p < 0.05), and positively correlated with the current August precipitation (p < 0.05). Under the gradual increasing of temperature predicted by the five GCMs and four RCP scenarios, the radial growth of P. Koraiensis will relatively increase, while that of L. olgensis and P. jezoensis will relatively decrease comparing to the base-line period (1981–2010). The specific growth–climate relationships and the future growth trends are species dependent. P. Koraiensis was the more suitable tree species for the forestation to maintain the sustainable forest in Changbai Mountain.

Highlights

  • Global warming and its influences on the structure, function, and growth of the forest ecosystem have been observed and recognized (Lindner et al, 2010; Intergovernmental Panel on Climate Change (IPCC), 2013; Rahman et al, 2017; Russell and Parton, 2020)

  • L. olgensis, and P. jezoensis chosen in this study were the three typical and representative conifer tree species of Changbai Mountain

  • Due to the vertical zonality of Changbai Mountain, the microclimate is different (Editorial Committee for Forestry of Jilin, 1988), which further leads to the influence of altitude on the radial growth-climate relationships for the individual tree species

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Summary

Introduction

Global warming and its influences on the structure, function, and growth of the forest ecosystem have been observed and recognized (Lindner et al, 2010; IPCC, 2013; Rahman et al, 2017; Russell and Parton, 2020). Tree-ring can be used as an important data source to study impacts of climate change on tree growth, for tree-ring recording the tree growth process and reflecting the effect of tree growth climate conditions. Many studies on tree growth-climate relationships have been widely carried out by dendroclimatological method using this proxy data (Fritts, 1976; Lebourgeois et al, 2012; Housset et al, 2018; Zhang et al, 2018)

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