Climate influence on radial increment of oak (Quercus SP.) in central Poland

[1] Bednarz Z, 1987. A 225-year tree-ring chronology of oak Quercus robur L. in the Niepołomice Forest near Kraków. Dendrochronologia 5: 59–68. Search in Google Scholar

[2] Bednarz Z and Ptak J, 1990. The influence of temperature and precipitation on ring widths of oak (Quercus robur L.) in the Niepołomice Forest near Cracow, Southern Poland. Tree-Ring Bulletin 50: 1–10. Search in Google Scholar

[3] Bednarz Z, 1994. Niedobory wody przyczyną depresji przyrostowych u dębu (Quercus robur L.) w Puszczy Niepołomickiej (Water deficit limits tree-ring widths of the Oak (Quercus robur L.) in the Niepołomice Forest, Southern Poland). Sylwan 138(10): 29–39 (in Polish). Search in Google Scholar

[4] Bijak Sz, 2009. North Atlantic Oscillation signal in tree-rings of oak in Poland. In: Kaczka RJ et al., eds., TRACE — Tree Rings in Archeology, Climatology and Ecology 7: 28–35. Search in Google Scholar

[5] Biondi F and Waikul K, 2004. DendroClim2002: A C++ 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. http://dx.doi.org/10.1016/j.cageo.2003.11.00410.1016/j.cageo.2003.11.004Search in Google Scholar

[6] Boratyńska K, Filipiak M and Boratyński A, 2006. Budowa morfologiczna i zmienność (Morphological characteristics and variability). In: Bugała W, ed., Dęby Nasze Drzewa leśne 11. Bogucki Wydawnictwo Naukowe, Poznań-Kórnik: 63–84 (in Polish). Search in Google Scholar

[7] Boryczka J, Stopa-Boryczka M, Bijak Sz, Cebulski R, Błażek E and Skrzypczuk J, 2007. Atlas współzależności parametrów meteorologicznych i geograficznych w Polsce cz. XX–XXI Cykliczne zmiany klimatu Europy w ostatnim tysiącleciu według badań dendrologicznych (Atlas of correlations between meteorological and geographical parameters in Poland pt. 20–21. Cyclic changes of European climate in last millennium according to dendrological research). Wydawnictwo Uniwersytet Warszawski, Warszawa (in Polish). Search in Google Scholar

[8] Bruchwald A and Dmyterko E, 1999. Reakcja przyrostowa dębu w powiązaniu ze stopniem uszkodzenia korony (Growth response of oak as connected with the crown damage level). Sylwan 2: 47–57 (in Polish). Search in Google Scholar

[9] Büntgen U, Tegel W, Nicolussi K., McCormick M, Frank D, Trouet, V, Kaplan J, Herzig F, Heussner U, Wanner H, Luterbacher J and Esper J, 2011. 2500 years of European climate variability and human susceptibility. Science 331: 578–582, DOI 10.1126/science.1197175. http://dx.doi.org/10.1126/science.119717510.1126/science.1197175Search in Google Scholar

[10] Cedro A, 2004. Zmiany klimatyczne na Pomorzu Zachodnim w świetle analizy sekwencji przyrostów rocznych sosny zwyczajnej, daglezji zielonej i rodzimych gatunków dębów (Climatic changes in Western Pomerania basing on the analysis of tree-ring sequences of Scots pine, Douglas fir and native species of oak). PhD thesis, the University of Szczecin (in Polish). Search in Google Scholar

[11] Cedro A, 2007. Tree-ring chronologies of downy oak (Quercus pubescens) pedunculate oak (Q. robur) and sessile oak (Q. petraea) in the Bielinek Nature Reserve: comparison of the climatic determinats of tree-ring width. Geochronometria 26: 29–45. DOI 10.2478/v10003-007-0005-2. http://dx.doi.org/10.2478/v10003-007-0005-210.2478/v10003-007-0005-2Search in Google Scholar

[12] Cook ER, 1985. A time series analysis approach to tree-ring standardization. PhD thesis, University of Arizona. Search in Google Scholar

[13] Cook ER and Kairukstis LA, 1990. Methods of dendrochronology: applications in the environmental sciences. IIASA, Kluwer Academic Publishers, Boston. Search in Google Scholar

[14] Cropper JP, 1979. Tree-ring skeleton plotting by computer. Tree-ring Bulletin 39: 47–59. Search in Google Scholar

[15] Čufar K, de Luis M, Eckstein D and Kajfež-Bogataj L, 2008. Recon-structing dry and wet summers in SE Slovenia from oak tree-ring series. International Journal of Biometeorology 52(7): 607–615, DOI 10.1007/s00484-008-0153-8. http://dx.doi.org/10.1007/s00484-008-0153-810.1007/s00484-008-0153-8Search in Google Scholar

[16] Dekadowy Biuletyn Agrometeorologiczny 2001–2002, IMiGW a. Insty-tut Meteorologii i Gospodarki Wodnej, Warszawa. Search in Google Scholar

[17] Biuletyn Państwowej Służby Hydrologiczno-Meteorologicznej 2003–2007, IMiGW b. Instytut Meteorologii i Gospodarki Wodnej, Warszawa. Search in Google Scholar

[18] Desprez-Loustau ML, Marcais B, Nageleisen LM, Piou D and Vannini A, 2006. Interactive effects of drought and pathogens in forest trees. Annals of Forest Science 63(6): 597–612, DOI 10.1051/forest:2006040. http://dx.doi.org/10.1051/forest:200604010.1051/forest:2006040Search in Google Scholar

[19] Eckstein D and Bauch J, 1969. Ein Beitrag zur Rationalisierung eines dendrochronologishen Verfahrens und zur Analyse seiner Aussagesicherheit. Forstwiss. Centralbl. 88: 230–250. http://dx.doi.org/10.1007/BF0274177710.1007/BF02741777Search in Google Scholar

[20] Eilmann B, Weber P, Rigling A and Eckstein D, 2006. Growth reactions of Pinus sylvestris L. and Quercus pubescens Willd. to drought years at a xeric site in Valais, Switzerland. Dendrochronologia 23(3): 121–132, DOI 10.1016/j.dendro.2005.10.002. http://dx.doi.org/10.1016/j.dendro.2005.10.00210.1016/j.dendro.2005.10.002Search in Google Scholar

[21] Ermich K, 1953. Wpływ czynników klimatycznych na przyrost dębu szypułkowego (Quercus robur L.) oraz sosny zwyczajnej (Pinus silvestris L.) próba analizy zagadnienia. (The influence of climatic conditions on growth of Quercus robur and Pinus sylvestris). Prace Rolniczo-Leśne PAU 68: 1–61 (in Polish). Search in Google Scholar

[22] Ermich K, 1959. Badania nad sezonowym przebiegiem przyrostu grubości pnia u Pinus sylvestris L. i Quercus robur L (Studies on the seasonal course of growth of Pinus sylvestris L and Quercus robur L.). Acta Societatis Botanicorum Poloniae 28: 15–63 (in Polish). 10.5586/asbp.1959.002Search in Google Scholar

[23] Fritts HC, 1976. Tree rings and climate. Academic Press, London-New York-San Francisco. Search in Google Scholar

[24] Gonzalez IG, 2001. Weiser: a computer program to identify event and pointer years in dendrochronological series. Dendrochronologia 19(2): 239–244. Search in Google Scholar

[25] Gray BM and Pilcher JR, 1983. Testing the significance of summary response functions. Tree-Ring Bulletin 43: 31–37. Search in Google Scholar

[26] Grissino-Mayer HD, 2001. Evaluating cross-dating accuracy: a manual and tutorial for the computer program COFECHA. Tree Ring Research 57: 205–221. Search in Google Scholar

[27] Holmes RL, 1999. Dendrochronology Program Library (DPL) Users Manual. LTRR University of Arizona, Tucson. Search in Google Scholar

[28] Ingot S, 1968. Zjawiska klimatyczno-meteorologiczne na Śląsku od XVI do połowy XIX wieku (Climatic events in Silesia from the 16th to the middle of the 19th century). In: Świętochowski B, ed., Z badań nad wpływem posuchy na rolnictwo na Dolnym Śląsku. PWN, Wrocław: 9–29 (in Polish). Search in Google Scholar

[29] Krąpiec M, 1998. Oak dendrochronology of the Neoholocene in Poland. Folia Quaternaria 69: 5–133. Search in Google Scholar

[30] Krąpiec M, 2001. Holocene dendrochronological standars for subfossil oaks from the area of Southern Poland. Studia Quaternaria 69: 135–150. Search in Google Scholar

[31] Krąpiec M and Szychowska-Krąpiec E, 2004. Standardy dendrochronologiczne sosny zwyczajnej (Pinus sylvestris L.) i dębu szypułkowego (Quercus robur L.) z północnowschodniej Polski (Dendrochronological standards of Scots pine (Pinus sylvestris L.) and English oak (Quercus robur L.) from northeastern Poland). Sylwan 148(7): 11–19 (in Polish). Search in Google Scholar

[32] Lebourgeois F, Cousseau G and Ducos Y, 2004. Climate-tree-growth relationships of Quercus petraea Mill. stand in the Forest of Bercé (’Futaie des Clos’, Sarthe, France). Annals of Forest Science 61(4): 361–372, DOI 10.1051/forest:2004029. http://dx.doi.org/10.1051/forest:200402910.1051/forest:2004029Search in Google Scholar

[33] Lorenc H, ed., 2005. Altas klimatu Polski. Instytut Meteorologii i Gospodarki Wodnej, Warszawa (in Polish). Search in Google Scholar

[34] Mager P, Kuźnicka M, Krępińska-Kasprzak M and Farat R, 1999. Zmiany natężenia i częstotliwości pojawiania się susz w Polsce (1891–1995) (Changes in intensity and frequency of occurrence of droughts in Poland (1891–1995)). Proceedings of the conference Zmiany i zmiennośĆ klimatu Polski: 156–164 ( in Polish). Search in Google Scholar

[35] Mäkinen H and Vanninen P, 1999. Effect of sample selection on the environmental signal derived from tree-ring series. Forest Ecology and Management 113(1): 83–89, DOI 10.1016/S0378-1127(98)00416-2. http://dx.doi.org/10.1016/S0378-1127(98)00416-210.1016/S0378-1127(98)00416-2Search in Google Scholar

[36] Methy M, Damesin C, Rambal S, 1996. Drought and photosystem II activity in two Mediterranean oaks. Annals of Forest Science 53(2–3): 255–262, DOI 10.1051/forest:19960208. 10.1051/forest:19960208Search in Google Scholar

[37] Mitchell TD and Jones P, 2005. An improved method of constructing a database of monthly climate observations and associated high-resolution grids. International Journal of Climatology 25(6): 693–712, DOI 10.1002/joc.1181. http://dx.doi.org/10.1002/joc.118110.1002/joc.1181Search in Google Scholar

[38] Pilcher JR and Gray B, 1982. The relationships between oak tree growth and climate in Britain. Journal of Ecology 70(1): 297–304. http://dx.doi.org/10.2307/225988010.2307/2259880Search in Google Scholar

[39] Rozas V, 2001. Detecting the impact of climate and disturbances on tree-rings of Fagus sylvatica L. and Quercus robur L. in a lowland forest in Cantabria, Northern Spain. Annals of Forest Science 58(3): 237–251, DOI 10.1051/forest:2001123. http://dx.doi.org/10.1051/forest:200112310.1051/forest:2001123Search in Google Scholar

[40] Santini A, Bottacci A and Gellini R, 1994. Preliminary dendroecological survey on pedunculate oak (Quercus robur L) stands in Tuscany, Italy. Annales des Sciences Forestieres 51(1): 1–10, DOI 10.1051/forest:19940101. http://dx.doi.org/10.1051/forest:1994010110.1051/forest:19940101Search in Google Scholar

[41] Szczepanek M, Pazdur A, Pawełczyk S, Böttger T, Haupt M, Hałas S, Bednarz Z, Krąpiec M and Szychowska-Krąpiec E, 2006. Hydrogen, carbon and oxygen isotopes in pine and oak tree rings from Southern Poland as climatic indicators in years 1900–2003. Geochronometria 25: 67–76. Search in Google Scholar

[42] Schweingruber FH, 1996. Tree rings and environment. Paul Haupt, Bern. Search in Google Scholar

[43] Siwecki R, 1994. Globalne zmiany klimatyczne a zamieranie debów (Oaks’ decline related to global climate change). Sylwan 138(10): 43–59 (in Polish). Search in Google Scholar

[44] Tardif JC and Conciatori F, 2006. A comparison of ring-width and event-year chronologies derived from white oak (Quercus alba) and northern red oak (Quercus rubra), Southwestern Quebec, Canada. Dendrochronologia 23(3): 133–138, DOI 10.1016/j.dendro.2005.10.001. http://dx.doi.org/10.1016/j.dendro.2005.10.00110.1016/j.dendro.2005.10.001Search in Google Scholar

[45] Tessier L, Nola P and Serre-Bachet F, 1994. Deciduous Quercus in the Mediterranean region: tree-ring/climate relationships. New Phytologist 126(2): 355–367, DOI 10.1111/j.1469-8137.1994.tb03955.x. http://dx.doi.org/10.1111/j.1469-8137.1994.tb03955.x10.1111/j.1469-8137.1994.tb03955.xSearch in Google Scholar

[46] Ufnalski K, 2001. Porównanie dynamiki przyrostu dębu szypułkowego i bezszypułkowego ze szczególnym uwzględnieniem okresów zamierania (Comparisson of growth of pedunculat and sessile oaks with special regard to decline periods). PhD thesis, Institute of Dendrology Polish Academy of Sciences (in Polish). Search in Google Scholar

[47] Van der Werf GW, Sass-Klassen UGW and Mohren GMJ, 2007. The impact of the 2003 summer drought on the intra-annual growth pattern of beech (Fagus sylvatica L.) and oak (Quercus robur L.) on a dry site in the Netherlands. Dendrochronologia 25(2): 103–112, DOI 10.1016/j.dendro.2007.03.004. http://dx.doi.org/10.1016/j.dendro.2007.03.00410.1016/j.dendro.2007.03.004Search in Google Scholar

[48] Vannini A, Valentini R and Luisi N, 1996. Impact of drought and Hypoxylon mediterraneum on oak decline in the Mediterranean region. Annals of Forest Science 53(2–3): 753–760, DOI 10.1051/forest:19960251. 10.1051/forest:19960251Search in Google Scholar

[49] Ważny T, 1990. Aufbau und Anwendung der Dendrochronologie fur Eichenholz in Polen. Phd thesis, Universitaet Hamburg (in German). Search in Google Scholar

[50] Ważny T, 2006. Dendrochronologia dębu (Dendrochronology of oak). In: Boratyński A, ed., Dęby. Quercus robur L. Quercus petraea (Matt.) Nasze drzewa leśne. Monografie Popularnonaukowe, Poznań-Kórnik: 39–61 (in Polish). Search in Google Scholar

[51] Ważny T and Eckstein D, 1991. The dendrochronological signal of oak (Quercus spp.) in Poland. Dendrochronologia 9: 35–49. Search in Google Scholar

[52] Weber P, Rigling A and Bugmann H, 2005. Differences in drought response of Pinus sylvestris L. and Quercus pubescens Willd. in the Swiss Rhone valley. In: Jansma E, Brauning A, Gartner H, Schleser G, eds., TRACE 2: 48–52. Search in Google Scholar

[53] Zielski A and Krąpiec M, 2004. Dendrochronologia (Dendrochronology). Wydawnictwo Naukowe PWN Warszawa (in Polish). Search in Google Scholar