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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)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The research was conducted in selected 80- to 110-year-old spruce stands in the south-eastern 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, 1976 and 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 years when over 80% of the analysed trees responded by a sharp decrease in increment, mainly in years 1976 and 1992. We can usually find values of monthly precipitation or monthly temperature average which can explain or help explain these falls in the radial growth. The correlations of diameter increments with average monthly precipitation gain only positive statistically significant values, namely for the months of May, June, July and August of the particular year. The correlations of diameter increments with average monthly temperatures gain only negative statistical-ly significant values, namely for the months of June, July and September of the previous year and January and August of the particular year. In the examined area there is a significant negative correlation between average temperatures and monthly precipitation in July, August and September. The results of the habitual diagnostics show that with respect to the climatic conditions the health condition of the monitored stands is relatively good. On average, the defoliation does not exceed the values as-certained in different territories of the Czech Republic.
Wydawca
Czasopismo
Rocznik
Strony
149--157
Opis fizyczny
Bibliogr. 43 poz., wykr.
Twórcy
autor
autor
autor
  • Department of Wood Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 3, 613 00 Brno, Czech Republic, michalryb@email.cz
Bibliografia
  • Aakala T and Kuuluvainen T, 2011. Summer droughts depress radial growth of Picea abies in pristine taiga of the Arkhangelsk prov-ince, northwestern Russia, Dendrochronologia 29(2): 67-75, DOI 10.1016/j.dendro.2010.07.001.
  • Affolter P, Bűntgen U, Esper J, Rigling A, Weber P, Luterbacher J and Frank D, 2010. Inner Alpine conifer response to 20th century drought swings. European Journal of Forest Research 129(3): 289-298, DOI 10.1007/s10342-009-0327-x.
  • Barber VA, Juday GP and Finney BP, 2000. Reduced growth of Alas-kan white spruce in the twentieth century from temperature-induced drought stress. Nature 405(6787): 668-673, DOI 10.1038/35015049.
  • Biondi F, 1997. Evolutionary and moving response functions in dendro-climatology. Dendrochronologia 15: 139-150.
  • Biondi F and Waikul K, 2004. DendroClim2002: AC++ program for statistical calibration of climate signals in tree ring chronologies. Computers and Geosciences 30(3): 303-311, DOI 10.1016/j.cageo.2003.11.004.
  • Bouriaud O and Popa I, 2009. Comparative dendroclimatic study of Scots pine, Norway spruce, and silver fir in the Vrancea Range, Eastern Carpathian Mountains. Trees – Structure and Function 23(1): 95-106, DOI 10.1007/s00468-008-0258-z.
  • 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 dendrocli-matic studies. Tree Ring Bulletin 41: 45-53.
  • Cudlín P, Novotný R, Moravec I and Chmelíková E, 2001. Retrospec-tive evaluation of the response of montane forest ecosystems to multiple stress. Ekológia 20: 108-124.
  • D’Arrigo RD, Kaufmann RK, Davi N, Jacoby GC, Laskowski C, Myneni RB and Cherubini P, 2004. Thresholds for warming-induced growth decline at elevational tree line in the Yukon Terri-tory, Canada. Global Biogeochemical Cycles 18: GB3021, DOI 10.1029/2004GB002249.
  • Desplanque C, Rolland C and Schweingruber FH, 1999. Influence of species and abiotic factors on extreme tree ring modulation: Picea abies and Abies alba in Tarentaise and Maurienne (French Alps). Trees 13: 218-227.
  • Feliksik E and Wilczyński S, 2009. The Effect of Climate on Tree-Ring Chronologies of Native and Nonnative Tree Species Growing Un-der Homogenous Site Conditions. Geochronometria 33: 49-57, DOI 10.2478/v10003-009-0006-4.
  • Feliksik E, Wilczyński S and Wałecka M, 1994. Klimatyczne uwarun-kowania przyrostów kambialnych świerka pospolitego (Picea abies (L.) Karst.) w leśnictwe Pierściec (Climatic conditions of the cam-bial tree-rings of spruce (Picea abies Karst.) in the forest district of Pierściec). Acta Agraria et Silvestria. Series Silvestris 32: 53-59 (in Polish).
  • Fritts HC, 1966. Growth-rings of trees: Their correlation with climate. Science 154: 973-979, DOI 10.1126/science.154.3752.973.
  • Fritts HC, 1976. Tree-rings and Climate. London, New York, San Francisco, Academic Press: 567 pp.
  • Fritts HC, Mosimann JE and Bottorff CP, 1969. A Revised Computer Program for Standardizing Tree – Ring Series. Tree Ring Bulletin 29: 15-20.
  • Grabařová S and Martinková M, 2000. Changes of Norway spruce (Picea abies /L./ Karst.) growth characteristics under the impact of drought. Ekológia (Bratislava) 19, Supplement 1/2000: 81-103.
  • Grabařová S and Martinková M, 2001. Changes in mineral nutrition of Norway spruce (Picea abies /L./ Karst.) under the impact of drought. Ekológia (Bratislava) 20, Supplement 1/2001: 46-60.
  • 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.
  • Gryc V, Vavrčík H and Vichrová G, 2011. Monitoring of xylem for-mation in Norway spruce in the Czech republic 2009. Wood re-search 56 (4): 467-478.
  • Gryc V, Hcura J, Vavrčík H, Urban J and Gebauer R, 2012. Monitoring of xylem formation in Picea abies under drought stress influence. Dendrobiology 67(1): 15-24.
  • Holmes RL, Adams RK and Fritts HC, 1986. Tree–Ring Chronologies of Western North America: California, Eastern Oregon and North-ern Great Basin with Procedures Used in the Chronology Devel-opment 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 ecological gradients and the potential of single-year analyses. Canadian Journal of Forest Research 17(7): 683-696, DOI 10.1139/x87-111.
  • Knibbe B, 2004. PAST 4 - Personal Analysis System for Treering Research, Instruction Manual, Version 4, SCIEM: 141pp.
  • Koprowski M and Zielski A, 2006. Dendrochronology of Norway spruce (Picea abies (L.) Karst.) from two range centres in lowland Poland. Trees – Structure and Function 20(3): 383-390, DOI 10.1007/s00468-006-0051-9.
  • Kozlowski TT, 2002. Acclimation and adaptive responses of woody plants to environmental stresses. Botanical Review 68: 270-334.
  • 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 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/x00-005.
  • 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.
  • Miyamoto Y, Griesbauer HP and Green DS, 2010. Growth responses of three coexisting conifer species to climate across wide geographic and climate ranges in Yukon and British Columbia. Forest Ecolo-gy and Management 259: 514-523.
  • Rybníček M, Čermák P, Kolář T, Přemyslovská E, Žid T, 2009. Influ-ence of Temperatures and Precipitation on Radial Increment of Or-licke Mountains Spruce Stands in Altitudes over 800 m above Sea Level. Journal of Forest Science 55(6): 257-263.
  • Rybníček M, Čermák P, Kolář T and Žid T, 2010a. Radial Growth and Health Condition of Norway Spruce (Picea abies (L.) Karst.) Stands in Relation to Climate (Silesian Beskids, Czech Republic). Geochronometria 36: 9-16, DOI 10.2478/v10003-010-0017-1.
  • Rybníček M, Koňas P and Kolář T, 2010b. The Benefits of Tree-Ring Curves Detrending for Dating Archaeological Wood. Geochrono-metria 35: 85-90, DOI 10.2478/v10003-010-0004-6.
  • Rybníček M, Čermák P, Hadaš P, Kolář T and Žid T, 2012. Dendro-chronological Analysis and Habitual Stress Diagnostic Assessment of Norway Spruce (Picea abies) Stands in the Drahany Highlands. Wood Research 57 (2), In press.
  • Savva J, Oleksyn J, Reich PB, Tjoelker MG. Vaganov EA and Mo-drzynski J, 2006. Interannual growth response of Norway spruce to climate along an altitudinal gradient in the Tatra Mountains, Po-land. Trees – Structure and Function 20(6): 735-746, DOI 10.1007/s00468-006-0088-9.
  • Schweingruber FH, 1996. Tree Rings and Environment Dendroecology. Birmensdorf, Swiss Federal Institute for Forest, Snow and Land-scape Research, Berne, Stuttgart, Vienna: 609pp.
  • Szczepanek M, Pazdur A, Pawełczyk S, Böttger T, Haupt T, Hałas S, Bednarz Z, Kr?piec M and Szychowska-Krąpiec E, 2006. Hydro-gen, carbon and oxygen isotopes in pine and oak tree rings from southern Poland as climatic indicators in years 1900–2003. Geo-chronometria 25: 67-76.
  • Štěpánek P, 2007. ProClimDB – software for processing climatological datasets. CHMI, regional office Brno. http://www.climahom.eu/ProcData.html.
  • Viewegh J, Kusbach A and Mikeska M, 2003. Czech forest ecosystem classification. Journal of Forest Science 49(2): 85-93.
  • Vitas A, 2004. Tree rings of Norway spruce (Picea abies (L.) Karst.) in Lithuania as drought indicators: dendroecological approach. Polish Journal of Ecology 52(2): 201-210.
  • Vinš B. et al., 1997. Impacts of a Potential Climate Change on Forests of the Czech Republic. Praha, Národní lesnický komitét (National Forestry Committee): 142pp.
  • Žid T and Čermák P, 2007. Health condition of spruce stands in the Orlické hory Mts. in relation to climatic, anthropogenic and stand factors. Journal of Forest Science 53(1): 1-12.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BWMA-0008-0004
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