2012
DOI: 10.2478/s13386-012-0003-7
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Growth responses of Norway spruce (Picea abies (L.) Karst.) to the climate in the south-eastern part of the Českomoravská Upland (Czech Republic)

Abstract: Abstract:The research was conducted in selected 80-to 110-year-old spruce stands in the southeastern part of the Českomoravská Upland at altitudes from 350 m a.s.l. to 465 m a.s.l. The regional standard tree-ring chronology shows very low increments for years 1974, 1976and 1992 . After 1992 there is a sharp rise in increments with a climax in 1997. Afterwards, increments gradually decrease, reaching minima in 2003 and 2008. The years with low increments were also confirmed by the analysis of negative pointer y… Show more

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Cited by 18 publications
(20 citation statements)
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References 27 publications
(36 reference statements)
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“…Although numerous studies regarding the drought tolerance and resilience of forest trees in relation to their site conditions exist [29,31,37,[70][71][72], the behavior of urban trees to drought is rarely researched [33,38,39]. However, urban trees are of great benefit to the climate of a city and the well-being of its citizens.…”
Section: Tree Ring Analysis: Quantification Of Growth Of Urban Trees mentioning
confidence: 99%
“…Although numerous studies regarding the drought tolerance and resilience of forest trees in relation to their site conditions exist [29,31,37,[70][71][72], the behavior of urban trees to drought is rarely researched [33,38,39]. However, urban trees are of great benefit to the climate of a city and the well-being of its citizens.…”
Section: Tree Ring Analysis: Quantification Of Growth Of Urban Trees mentioning
confidence: 99%
“…Foresters fear that the growth decline of European beech is likely to become more dramatic in the coming decades (Gerard and Breda 2014), leading to crucial fluctuations in the distribution limits (e.g., geographical/ecological range, altitudinal shift) (Tegel et al 2014). Our study was motivated by the following hypotheses: 1) temperature is the key climate factor controlling leaf phenology; 2) based on the results of previous studies of Norway spruce (Rybníček et al 2012) and sessile oak (Rybníček et al 2015) in this area, we assumed that TRW growth is driven by precipitation and water availability in the soil; and 3) the extended phenological growing season significantly influences the TRW.…”
Section: Introductionmentioning
confidence: 99%
“…Sequences that were the least similar to the standard pattern in the site included WP2, WP12, WP25, WP49, WP50, WP51 and WP53 were excluded from further analysis (Bijak, 2013). ARSTAN software was used to create raw data chronology, indexed chronology by the elimination of the trend and long-term fluctuations, and highlighting the short-term variations, and residual chronology by removing autocorrelations from the series of tree ring indexes (Cook & Holmes, 1999;Poljanšek et al, 2012;Rybníček et al, 2012).…”
Section: Methodsmentioning
confidence: 99%
“…when tree ring widths in all or most of the surveyed trees at a given site are greater or smaller than in the previous year (Cedro, 2012). A pointer year may sometimes be the same for different species (Okoński et al, 2014b), and its territorial range may cover not only a single site, but also a region or even an entire continent (Pourtahmasi et al, 2007;Bronisz et al, 2012;Rybníček et al, 2012;De Ridder et al, 2014). Analysis based on pointer years makes it possible to evaluate the course of meteorological conditions in a given year, characterized by a unique combination of conditions, in contrast to statistical analyses that evaluate the relationship between weather and tree ring widths over a multi-year period (Wilczyński, 2004).…”
Section: Introductionmentioning
confidence: 99%