Abstract

The divergence problem, which manifests as an unstable response relationship between tree-ring growth and climatic factors under the background of global warming, poses a challenge to both the traditional theory of dendroclimatology and the reliability of climatic reconstructions based on tree-ring data. Although Schrenk spruce, as the dominant tree species in the Tianshan Mountains, is frequently applied in the dendrochronological studies, the understanding of the divergence problem of this tree species is still limited. This study conducted correlation analysis between climatic factors and tree-ring width chronologies from 51 living and healthy specimens of Schrenk spruce at sites of high and low elevation in the Alatau Mountains to determine the stability of the response. The results revealed that the tree-ring width of the spruce specimens was correlated positively with precipitation and correlated negatively with temperature. Although the variations of the two tree-ring chronologies were similar, the radial growth of the spruce at the low elevation was found more sensitive to climatic factors. Furthermore, the sensitivity of tree growth to climate demonstrated an obvious increase after an abrupt change of climate under the background of the recent warming and wetting trend. Increased drought stress, calculated based on climatic data, was regarded as the main reason for this phenomenon. The results supply the gap of the stability of climatic response of tree growth in Central Asia to some extent.

Highlights

  • The effect of climate conditions to forest ecosystem is a hot research spot under the background of globe warming [1,2,3]

  • Characteristics of the Meteorological Data period of highest temperature in the study area is in summer (June–August) and that the Variation Characteristics of the Meteorological Data maximum temperature is in July (18.34 °C) (Figure 2a)

  • The stability of the response of the radial growth of Schrenk spruce to climate was verified based on two tree-ring width chronologies at high and low elevation sites in the Alatau Mountains

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Summary

Introduction

The effect of climate conditions to forest ecosystem is a hot research spot under the background of globe warming [1,2,3]. Atmosphere 2019, 10, 473 studies in high latitude and high elevation regions of the Northern Hemisphere have revealed that the sensitivity of tree growth to the main climatic limiting factor has changed under the effects of global warming [4,5,6]. Briffa et al [7] noticed that the temperature-sensitive of tree-ring-density in different regions of the northern boreal forest has an obvious reduction after 1960. This variability in climatic response has been found to extend to coniferous forests in middle–low elevation regions [8]

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