Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.

Research on the influence of temperatures and precipitation on radial increment was carried out in spruce stands over ninety years old in the surroundings of Anenský vrch in the Orlické hory Mts. at altitudes over 800 m above sea level. To model diameter increment in dependence on climatic condition...

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Main Authors: M. Rybníček, P. Čermák, T. Kolář, E. Přemyslovská, T. Žid
Format: Article
Language:English
Published: Czech Academy of Agricultural Sciences 2009-06-01
Series:Journal of Forest Science
Subjects:
Online Access:https://jfs.agriculturejournals.cz/artkey/jfs-200906-0002_influence-of-temperatures-and-precipitation-on-radial-increment-of-orlicke-hory-mts-spruce-stands-at-altitudes.php
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author M. Rybníček
P. Čermák
T. Kolář
E. Přemyslovská
T. Žid
author_facet M. Rybníček
P. Čermák
T. Kolář
E. Přemyslovská
T. Žid
author_sort M. Rybníček
collection DOAJ
description Research on the influence of temperatures and precipitation on radial increment was carried out in spruce stands over ninety years old in the surroundings of Anenský vrch in the Orlické hory Mts. at altitudes over 800 m above sea level. To model diameter increment in dependence on climatic conditions, the standard tree-ring and correlation analysis together with the analysis of negative pointer years were used. The diameter increment has a statistically significant correlation with temperatures in July of each year in question. The growth of spruce is also affected to a statistically significant degree by precipitation in July of the previous year and by precipitation in February and March of the year in question. The standard tree-ring chronology shows an obvious decrease in radial increments starting at the beginning of the 1970s and ending at the end of the 1980s. The lowest increments were recorded for 1974, 1980, 1984 and 1986. These years with low increments were also confirmed by the analysis of negative pointer years. In the following period there is an increase in increments, with slight decreases in 1996 and 2000, which, however, according to the analysis of negative pointer years do not demonstrate any significant reduction of increments. Another decrease was recorded starting in 2003 and this lasted until the studied period, i.e. 2007. The current condition of spruce stands is certainly the result of more stressors but it appears that with the current air pollution load the climatic conditions are the factor determining the resulting effect of the synergic influence of the stressors on the stands.
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spelling doaj.art-7b28b50d67dd433dbad6b4c8ccb863f72023-02-23T03:42:04ZengCzech Academy of Agricultural SciencesJournal of Forest Science1212-48341805-935X2009-06-0155625726310.17221/90/2008-JFSjfs-200906-0002Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.M. Rybníček0P. Čermák1T. Kolář2E. Přemyslovská3T. Žid4Faculty of Forestry and Wood Technology, Mendel University of Agriculture and Forestry in Brno, Brno, Czech RepublicFaculty of Forestry and Wood Technology, Mendel University of Agriculture and Forestry in Brno, Brno, Czech RepublicFaculty of Forestry and Wood Technology, Mendel University of Agriculture and Forestry in Brno, Brno, Czech RepublicFaculty of Forestry and Wood Technology, Mendel University of Agriculture and Forestry in Brno, Brno, Czech RepublicFaculty of Forestry and Wood Technology, Mendel University of Agriculture and Forestry in Brno, Brno, Czech RepublicResearch on the influence of temperatures and precipitation on radial increment was carried out in spruce stands over ninety years old in the surroundings of Anenský vrch in the Orlické hory Mts. at altitudes over 800 m above sea level. To model diameter increment in dependence on climatic conditions, the standard tree-ring and correlation analysis together with the analysis of negative pointer years were used. The diameter increment has a statistically significant correlation with temperatures in July of each year in question. The growth of spruce is also affected to a statistically significant degree by precipitation in July of the previous year and by precipitation in February and March of the year in question. The standard tree-ring chronology shows an obvious decrease in radial increments starting at the beginning of the 1970s and ending at the end of the 1980s. The lowest increments were recorded for 1974, 1980, 1984 and 1986. These years with low increments were also confirmed by the analysis of negative pointer years. In the following period there is an increase in increments, with slight decreases in 1996 and 2000, which, however, according to the analysis of negative pointer years do not demonstrate any significant reduction of increments. Another decrease was recorded starting in 2003 and this lasted until the studied period, i.e. 2007. The current condition of spruce stands is certainly the result of more stressors but it appears that with the current air pollution load the climatic conditions are the factor determining the resulting effect of the synergic influence of the stressors on the stands.https://jfs.agriculturejournals.cz/artkey/jfs-200906-0002_influence-of-temperatures-and-precipitation-on-radial-increment-of-orlicke-hory-mts-spruce-stands-at-altitudes.phporlické hory mts.tree-ring analysisspruceclimateradial increments
spellingShingle M. Rybníček
P. Čermák
T. Kolář
E. Přemyslovská
T. Žid
Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.
Journal of Forest Science
orlické hory mts.
tree-ring analysis
spruce
climate
radial increments
title Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.
title_full Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.
title_fullStr Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.
title_full_unstemmed Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.
title_short Influence of temperatures and precipitation on radial increment of Orlické hory Mts. spruce stands at altitudes over 800 m a.s.l.
title_sort influence of temperatures and precipitation on radial increment of orlicke hory mts spruce stands at altitudes over 800 m a s l
topic orlické hory mts.
tree-ring analysis
spruce
climate
radial increments
url https://jfs.agriculturejournals.cz/artkey/jfs-200906-0002_influence-of-temperatures-and-precipitation-on-radial-increment-of-orlicke-hory-mts-spruce-stands-at-altitudes.php
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