2012
DOI: 10.1007/s00468-012-0776-6
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Climate–growth analysis of Qilian juniper across an altitudinal gradient in the central Qilian Mountains, northwest China

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Cited by 40 publications
(16 citation statements)
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References 33 publications
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“…As a consequence of these rapid asymmetrical changes, statistical correlations of growth with basic weather data are becoming less reliable (Briffa et al 1998;Gao et al 2013) and much more variable (Zhang and Wilmking 2010). As an alternative to conventional dendrochronological analysis, process-based modeling may offer a more holistic interpretation (Evans et al 2006).…”
Section: Introductionmentioning
confidence: 99%
“…As a consequence of these rapid asymmetrical changes, statistical correlations of growth with basic weather data are becoming less reliable (Briffa et al 1998;Gao et al 2013) and much more variable (Zhang and Wilmking 2010). As an alternative to conventional dendrochronological analysis, process-based modeling may offer a more holistic interpretation (Evans et al 2006).…”
Section: Introductionmentioning
confidence: 99%
“…In contrast, the present study found consistent patterns of Qilian juniper growth at the high-and low-elevation sites. Consistent growth at high-and low-elevation sites has been reported in other parts of the Qinghai-Tibetan Plateau (Gao et al 2013;Yang et al 2013). Water stress was the main climatic factor that caused homogeneous tree growth across an altitudinal gradient in the western of the Qilian Mountains .…”
Section: Discussionmentioning
confidence: 87%
“…The growth decline were mainly caused by the warming-induced water limitations, especially the warmer spring (Wu et al 2012(Wu et al , 2013; while, previous autumn and winter temperature improved the speedup of tree growth in the Tianshan Mountains (Qi et al 2015). Previous researches using dendroclimatological methods have demonstrated that temperatures during the previous winter played a dominant role in growth of Qilian juniper in the middle of the Qilian Mountains Gao et al 2013). In addition, precipitation during the previous winter (mostly in the form of snow) also contributed to the recent enhancement of tree growth (Fig.…”
Section: Divergent Response To the Warming Of Different Regionsmentioning
confidence: 99%
“…Warmer spring temperatures would advance the onset of growing season by increasing the melting of snow cover and warming soil and stem meristems at higher elevations [35]. However, at lower elevations, a higher growing season Forests 2018, 9, 248 9 of 11 temperature could negatively impact the growth of A. fargesii through enhanced evapotranspiration leading to drought stress and reducing the rate of cambium division during xylogenesis [38,39], as has been described in drought-prone mountain forest environments [40,41]. Notably, the precipitation showed an earlier (April) and stronger negative impact on the growth of A. fargesii than L. chinensis in the pre-growing season.…”
Section: Discussionmentioning
confidence: 92%