Dendroclimatic studies were carried out in the experimental stands composed of many tree species situated in the Polish part of the Baltic sea-coast. Increment cores were taken from a 100-years old trees of 2 native species: Norway spruce (Picea abies (L.) Karst.), and Scots pine (Pinus sylvestris L.) and 3 nonnative species: Douglas fir (Pseudotsuga menziesii (Mirb.) Franco), Sitka spruce (Picea sitchensis (Bong.) Carr.) and Silver fir (Abies alba Mill.). Thirty trees of each species were cored. The relationships between the diameter increment and the thermal and pluvial conditions during the period from 1925 to 2005 were analyzed on the basis of standardized tree-ring chronologies and climatic data. It was found that precipitation and temperature of the growing season and months preceding that season affected the annual diameter increment of all investigated tree species. The current year winter and early spring temperatures as well as February and August precipitation had a similar effect on the variation of diameter increment of trees. On the other hand thermal and pluvial conditions of the current year June differentiated the increment rhythm of individual species. A very strong negative effect on diameter growth of trees was observed in the case of winter and early spring frosts. Norway spruce turned out to be a species most resistant to low temperatures. The investigated tree species, especially Norway spruce, was susceptible to water deficiency in the soil during spring and summer. In the case of Scots pine a high precipitation in June stimulated its growth. The diameter increments of Douglas fir, Sitka spruce, Scots pine, and Silver fir were more strongly connected with air temperature than with precipitation. So called all-species chronology of tree-ring width, constructed during this study, permitted to verify the factors having a similar effect on growth response of the investigated tree species. It reflected the mutual characteristics of diameter increments of trees of various species.
Six Douglas fir (Pseudotsuga menziesii Franco) stands were selected in both the Sudety Mountains and the Great Poland Lowland. These two regions are distinctly different with regard to thermal and pluvial conditions. In each stand, two increment cores per tree were extracted from 20 approximately 100-year-old trees and the tree-ring widths measured. It is clear from the different growth reactions of the study trees to the climatic conditions that the Sudety Mountains and the Great Poland Lowland are two dendrochronologically separate regions. The tree-ring width chronologies form homogeneous groups for each region. The tree ring-climate models for Douglas fir in both regions indicate similarities and differences. The similarities among chronologies are attributed to winter temperature. The differences are attributed to rainfall (which changes with longitude and altitude of sites) during the vegetation season.
This paper presents results concerning climatic conditions affecting diameter growth of Sitka spruce introduced to Baltic Pomerania (Sławno Forest District). A relatively high homogeneity of tree-ring series permitted to construct on their basis the tree-ring chronology of Sitka spruce. A significant positive correlation was found between radial increments of Sitka spruce and air temperatures of winter and spring months (January-April) and a negative relationship between radial increments and temperature of May. This study also showed a distinctly positive correlation between diameter growth and precipitation in July and November of the previous year, and precipitation in February and in summer season (June-August) of the current year. During years with low precipitation in summer or low temperatures in winter and spring all trees produced narrow tree-rings. The proportion of air temperature and precipitation in variation of radial increment of Sitka spruce, expressed by the coefficient of multiple determination, was 52%.
Abstract:In Poland, 50 sites of Douglas fir were selected for which tree-ring chronologies were computed. Douglas fir in different parts of Poland has a specific increment rhythm, on the basis of which the four homogeneous dendrochronological zones were distinguished. The first zone (I) comprises Pomerania, Baltic coast, Warmia, and Mazuria (lowlands of northern Poland), the second zone (II) -Great Poland, Lower Silesia (lowlands of central Poland), the third zone (III) -the Sudetes and the Carpathian mountains, and the fourth zone (IV) -foothills of the Carpathians Mts., Roztocze, and the Świętokrzyskie Mts. (uplands of southern Poland). These areas are called the dendroclimatic zones because different thermo-pluvial conditions of the summer season were a cause of diversification of the Douglas fir increment rhythm, and in consequence of its chronology. A high similarity of site chronologies of a given region permitted to construct regional tree-ring chronologies for respective zones. Thermal conditions of the winter season (February -March) were the factor most strongly and similarly affecting radial increment of Douglas fir populations in the entire territory of Poland. This factor caused that all chronologies showed many similar traits in their progress. This fact permitted to construct the supra-regional (all-Polish) tree-ring chronology for this tree species. It comprises the period from 1900 to 2000, and it is a good standard for dating Douglas fir wood samples originating from the area of Poland.
ABSTRACT:Changes in radial increment of Norway spruce in 25 stands more than 100 years old were analysed. Stands were growing on sites of different exposure situated at 450-1,200 m above sea level in the Polish Western Beskids Mountains. In the mid-1990s a considerable increase in annual ring width was observed. The greatest increase occurred in trees growing at the highest altitudes. This phenomenon occurred after a long period of increment decrease at the turn of the 1970s. After 1990 as the annual ring width was increasing, the variation and amplitude of ring width also increased. The cause of a long-term increase in radial increment was the improvement of thermal and pluvial conditions during late winter and early spring having a substantial effect on Norway spruce growth. In the 1990s the period of rapid changes in thermal and pluvial conditions of summer began. After moist and cold summers there were hot and dry summers. This resulted in increased variations and amplitude of the growth responses of Norway spruce and contributed to the weakening of trees above 100 years of age. The increasing break-up of Norway spruce stands growing in the lower mountain zone of the Polish Western Beskids Mountains, observed in recent years, is the final effect of this process.Keywords: tree-ring; ring width variation; Norway spruce; Polish Beskids Mountains JOURNAL OF FOREST SCIENCE, 51, 2005 (12) altitude of its localities in the lower mountain zone, and thus to find possible climatic reasons for the decline of its population in the Beskids (FELIKSIK, WILCZYŃSKI 2003a;WILCZYŃSKI, FELIKSIK 2004;HOLUŠA 2004).During these investigations a specific variation of radial increments of Norway spruces, and especially its untypical disturbances, were noticed. Therefore a study reported in this paper was undertaken in order to determine the character and probable causes of this interesting response of trees. MATERIAL AND METHODSThe study material originated from 25 Norway spruce stands growing on sites of different exposure and situated at different altitudes (from 450 m to 1,200 m a.s.l.) in the Polish Western Beskids (Fig. 1). The sites represented Norway spruce populations growing on high mountain coniferous forest sites, mountain mixed coniferous forest sites, mountain broadleaved forest sites and mountain mixed broadleaved forest sites. The sites were located in stands above 100 years of age in which the spruce was a dominant species. From selected 25 dominant and co-dominant trees in each stand the increment cores were taken with Pressler's increment borer; 1.5 m above the ground. We took one sample along the diameter parallel to the slope.The width of annual rings was measured on the cores. As a resultant 625-time tree-ring series were obtained. The correctness of ring dating was checked using the program COFECHA (HOLMES 1986).To assess the variability of the growth behaviour of Norway spruce trees during 1920-2003 the variation of their annual ring width and the course of tree-ring chronologies on individual sites were analy...
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