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Adial growth and health condition of norway spruce (Picea abies (L.) Karst.) Stands in relation to climate (Silesian Beskids, Czech Republic)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The research was conducted in selected spruce stands of the Silesian Beskids aged over 70 at altitudes from 403 m a.s.l. to 794 m a.s.l. in 2008. The samples were taken and processed in compliance with standard dendrochronological methodology. Tree rings were measured and the treering curves were synchronized using the PAST4 application. The age trend was removed in the ARSTAN application and the climatic influences were modelled in the DendroClim application. The regional standard tree-ring chronology shows an obvious decrease in the radial increment from the beginning of the 1970s to the mid-1990s. The gradual increase in radial increment which followed in the second half of the 1990s was interrupted in 2000, 2003, and 2006. Most of the years with the decreased radial increment have been confirmed by the analysis of significant negative years. The radial increment statistically significantly correlates with the precipitation in July and September of the previous year, precipitation in June of the year in question and precipitation during the vegetation period. Moreover, the growth of spruce is statistically significantly affected by temperatures in October of the previous year and March of the year in question. Additionally, the paper includes habitual monitoring of trees and the volume of salvage cutting in these districts. The condition of the habit of trees and the development of salvage cuttings agree with the hypothesis about strong stress load or its considerable increase in 2003 and the following years.
Wydawca
Czasopismo
Rocznik
Tom
Strony
9--16
Opis fizyczny
Bibliogr. 27 poz., rys., tab.
Twórcy
autor
autor
autor
  • Mendel University in Brno, Faculty of Forestry and Wood Technology, Zemědělská 3, 613 00 Brno, Czech Republic, michalryb@email.cz
Bibliografia
  • Biondi F, 1997. Evolutionary and moving response functions in dendroclimatology. Dendrochronologia 15: 139-150.
  • Biondi F and Waikul K, 2004. DendroClim2002: AC++ program for statistical calibration of climate signals in tree ring chronologie. Computers and Geosciences 30(3): 303-311, DOI 10.1016/j.cageo.2003.11.004.
  • Büntgen U, Frank DC, Kaczka RJ, Verstege A, Zwijacz-Kozina T and Esper J, 2007. Growth responses to climate in a multi-species treering network in the Western Carpathian Tatra Mountains, Poland and Slovakia. Tree Physiology 27(5): 689-702, DOI 10.1093/treephys/27.5.689.
  • Cook ER and Kairiukstis LA, 1990. Methods of Dendrochronology – Applications in the Environmental Sciences. Kluwer Academic Publisher and International Institute for Applied Systems Analysis, Dordrecht, Boston, London: 394pp.
  • Cook ER and Peters K, 1981. The smoothing spline: a new approach to standardizing forest interior tree–ring width series for dendroclimatic studies. Tree Ring Bulletin 41: 45-53.
  • Cudlín P, Novotný R, Moravec I and Chmelíková E, 2001. Retrospective evaluation of the response of montane forest ecosystems to multiple stress. Ekológia 20: 108–124.
  • Desplanque C, Rolland C and Schweingruber FH, 1999. Influence ofspecies and abiotic factors on extreme tree ring modulation: Picea abies and Abies alba in Tarentaise and Maurienne (French Alps). Trees 13(4): 218-227, DOI 10.1007/s004680050236.
  • Feliksik E, 1993. Wpływ klimatu na Wielkość przyrostów radialnych lasotwórczych gatunków, występujących na terenie leśnictwa Bukowiec (The effects of climate on the radial increments of the forest tree species occurring in the Bukowiec Forest district). Acta Agraria et Silvestria, Series Silvestris 31: 39-46 (in Polish).
  • Feliksik E, Wilczyński S and Wałecka M, 1994. Klimatyczne uwarunkowania przyrostów kambialnych świerka pospolitego (Picea abies Karst.) w leśnictwie Pierściec (Climatic conditions of the cambial tree-rings of spruce (Picea abies Karst.) in the forest district of Pierściec). Acta Agraria et Silvestria. Series Silvestris 32: 53-59 (in Polish).
  • Feliksik E and Wilczyński S, 2000. Dendroclimatological analysis of the Norway spruce (Picea abies (L.) Karst.) from the Beskid Śląski Mountains. Zpravodaj Beskydy 13: 161-170.
  • Fritts HC, Mosimann JE and Bottorff CP, 1969. A Revised Computer Program for Standardizing Tree – Ring Series. Tree Ring Bulletin 29: 15-20.
  • Grissino-Mayer HD, Holmes R and Fritts HC, 1992. International tree–ring data bank program library. Version 1.1. Laboratory of Tree–Ring Research, University of Arizona, Tucson. Holmes RL, Adams RK and Fritts HC, 1986. Tree–Ring Chronologies of Western North America: California, Eastern Oregon and Northern Great Basin with Procedures Used in the Chronology Development Work Including Users Manuals for Computer programs Cofecha and Arstan. – Chronology Series VI. Laboratory of Tree – Ring Research, University of Arizona, Tuscon, AZ, USA: 50-56.
  • Kienast F, Schweingruber FH, Bräker OU and Schär E, 1987. Tree ring studies on conifers along eco-logical gradients and the potential of single-year analyses. Canadian Journal of Forest Research 17(7): 683-696, DOI 10.1139/x87-111.
  • Koprowski M and Zielski A, 2006. Dendrochronology of Norway spruce (Picea abies (L.) Karst.) from two range centres in lowland Poland. Trees 20(3): 383-390, DOI 10.1007/s00468-006-0051-9.
  • Kroupová M, 2002. Dendroecological study of spruce growth in regions under long-term air pollution load. Journal of Forest Science 48(12): 536-548.
  • Lesinski JA and Landman G, 1995. Crown and branch malformation in conifers related to forest decline. In Cape JN and Mathy P, (eds.) Scientific basis of forest decline symptomatology, Air Pollution Research Report 15: 95-105.
  • Mäkinen H, Nöjd P and Mielikäinen K, 2000. Climatic signal in annual growth variation in damaged and healthy stands of Norway spruce (Picea abies) along a transect from central Finland to the Arctic timberline. Canadian Journal of Forest Research 30(5): 769-777, DOI 10.1139/cjfr-30-5-769.
  • Mäkinen H, Nöjd P and Mielikäinen K, 2001. Climatic signal in annual growth variation in damaged and healthy stands of Norway spruce [Picea abies (L.) Karst.] in southern Finland. Trees 15(3): 177-185, DOI 10.1007/s004680100089.
  • Mäkinen R, Nöjd P, Kahle HP, Neumann U, Tveite B, Mielikäinen K, Röhle H and Spiecker H, 2002. Radial growth variation of Norway spruce (Picea abies (L.) Karst.) across latitudinal and altitudinal gradients in central and northern Europe. Forest Ecology and Management 171(3): 243-259, DOI 10.1016/S0378-1127(01)00786-1.
  • MZe ČR, VÚLHM 2004. Monitoring stavu lesa v České republice 1984–2003 (Forest Condition Monitoring in the Czech Republic, 1984–2003). MZe ČR, VÚLHM, Praha, 432 pp (in Czech).
  • Pichler P and Oberhuber W, 2007. Radial growth response of coniferous forest trees in an inner Alpine environment to heat-wave in 2003. Forest Ecology and Management 242(2-3): 688-699, DOI 10.1016/j.foreco.2007.02.007.
  • Rybníček M, Koňas P and Kolář T, 2010: The Benefits of Tree-Ring Curves Detrending for Dating Archaeological Wood. Geochronometria 35: 85-90, DOI 10.2478/v10003-010-0004-6.
  • Savva J, Oleksyn J, Reich PB., Tjoelker MG, Vaganov EA and Modrzynski J, 2006. Interannual growth response of Norway spruce to climate along an altitudinal gradient in the Tatra Mountains, Poland. Trees 20(6): 735-746, DOI 10.1007/s00468-006-0088-9.
  • Šmelko Š and Wolf J, 1977. Štatistické metódy v lesníctve (Statistical Methods in Forestry). Príroda: 330pp (in Slovak).
  • Šrámek V, Vejpustková M, Novotný R and Hellebrandová K, 2008. Yellowing of Norway spruce stands in the Silesian Beskids – damage extent and dynamics. Journal of Forest Science 54(2): 55-63.
  • Vitas A, 2004. Tree rings of Norway spruce (Picea abies (L.) Karsten) in Lithuania as drought indicators: dendroecological approach. Polish Journal of Ecology 52(2): 201-210.
  • Wilczyński S and Feliksik E, 2005. Disturbances in variation of theannual ring width of Norway spruce in the Polish Western Beskids Mountains. Journal of Forest Science 51(12): 539-547.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BATA-0012-0019
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