Search Results

1 - 10 of 51 items :

  • "dendroclimatology" x
Clear All

.M.L., Briffa K.R., Jones P.D. 1984. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Climate and Applied Meteorology 23: 201-213. Zając M., Zając A. (eds.) 1997. Atlas rozmieszczenia roślin naczyniowych chronionych w Polsce. Pracownia Chorologii Komputerowej Instytutu Botaniki Uniwersytetu Jagiellońskiego, Kraków, 99 s. Zając M., Zając A. (eds.) 2001. Atlas rozmieszczenia roślin naczyniowych w Polsce. Pracownia Chorologii Komputerowej Instytutu Botaniki Uniwersytetu Jagiellońskiego, Kraków, 99 s.

value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Climate and Applied Meteorology , 23, 201–213. Wilczyński, S. 2004. Specyficzność regionów górskich. In: Dendrochronologia (eds.: A. Zielski, M. Krąpiec). Państwowe Wydawnictwo Naukowe, Warszawa, 267–268. Wilczyński, S. 2010. Determinants of radial growth in some tree species on Kielecka Upland in light of dendroclimatological analyses (in Polish). Zeszyty Naukowe Uniwersytetu Rolniczego im. Hugona Kołłątaja w Krakowie . Rozprawy, 464 (341), 1–221. Wilczyński

(Tables of volume and growth of stands for major forest tree species). PWRiL, Warszawa (in Polish). [45] Tang CQ, Yang Y, Ohsawa M, Momohara A, Hara M, Cheng S and Fan S, 2011. Population structure of relict Metasequoia glyptostroboides and its habitat fragmentation and degradation in south-central China. Biological Conservation 144(1): 279–289, DOI 10.1016/j.biocon.2010.09.003. http://dx.doi.org/10.1016/j.biocon.2010.09.003 [46] Wigley TML, Briffa KR and Jones PD, 1984. On the Average Value of Correlated Time Series, with Applications in Dendroclimatology and

-7-1127. Parker ML and Henoch WES, 1971. Increment core planer for X-ray densitometric sample preparation. Wood Science 11(1): 33-36. Polge H, 1970. The use of X-ray densitometric methods in dendrochronology. Tree-Ring Bulletin 30: 1-10. Schweingruber FH, Fritts HC, Bräker OU, Drew LG and Schär E, 1978. The X-ray technique as applied to dendroclimatology. Tree-Ring Bulletin 38: 61-91. Stokes MA and Smiley TL, 1968. An introduction to tree-ring dating. Chicago, University of Chicago Press: 111pp. Wang LL, Duan JP, Chen J, Huang L and Shao XM, 2009. Temperature

.V., Jónsson, T. 2001. Nordklim data set 1.0 - description and illustrations. - DNMI - REPORT 08/01. Norwegian Meteorological Institute, Oslo, 1-27. Varmola, M., Salminen, H., Timonen, M. 2004. Thinning response and growth trends of seeded Scots pine stands at the arctic timberline. - Silva Fennica, 38, 71-83. Wigley, T.M.L., Briffa, K.R., Jones, P.D. 1984. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. - Journal of Climate and Applied Meteorology, 23, 201-213. Yamaguchi, D.K. 1991. A simple method for crossdating

Journal of Polish Agricultural Universities, series Forestry 4(2). Wilczyński S and Skrzyszewski J, 2003. Dendrochronology of Scots pine ( Pinus sylvestris L.) in the mountains of Poland. Journal Forest Science 3: 95-103. Wilczyński S, 1999. Dendroklimatologia sosny zwyczajnej ( Pinus sylvestris L.) z wybranych stanowisk w Polsce (Dendroclimatology of Scots pine from selected sites in Poland). Dissertation - manuscript, Katedra Klimatologii Leśnej, Akademia Rolnicza w Krakowie , 85pp (in Polish). Wilczyński S, Krąpiec M, Szychowska-Krąpiec E and Zielski A, 2001

need, a warning of some pitfalls, and suggested improvements in its application. In: Hughes MK, Swetnam TW, Diaz HF, eds., Dendroclimatology: progress and prospects. Springer, Dordrecht: 113–145. http://dx.doi.org/10.1007/978-1-4020-5725-0_5 [14] Bronisz A, Bijak S, Bronisz K and Zasada M, 2012. Climate influence on radial increment of oak (Quercus sp.) in central Poland. Geochronometria 39(4): 276–284, DOI 10.2478/s13386-012-0011-7. http://dx.doi.org/10.2478/s13386-012-0011-7 [15] Catton HA, St George S and Remphrey WR, 2007. An evaluation of bur oak (Quercus

[1] Akkemik U, 2000. Dendroclimatology of Umbrella pine (Pinus pinea L.) in Istanbul, Turkey. Tree-Ring Bullettin 56:17–20. [2] Aniol RW, 1983. Tree-ring analysis using CATRAS. Dendrochronologia 1: 45–53. [3] Aniol RW, 1987. A new device for computer assisted measurement of tree-ring widths. Dendrochronologia 5:135–141. [4] Ashmann H, 1973. Distribution and Peculiarity of Mediterranean Ecosystems. In Mediterranean Type Ecosystems — Origin and Structure, di Castri F. and Mooney H.A., eds, Berlin, Springer: 11–19. http://dx.doi.org/10.1007/978-3-642-65520-3_2 [5

programu TCS. Program TCS do obliczania lat wskaźnikowych. Kraków. Wigley T.M.L., Briffa K.R., Jones P.D. 1984. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Climate and Applied Meteorology 23: 201–213. Wilczyński S., Krąpiec M., Szychowska-Krąpiec E., Zielski A. 2001. Regiony dendroklimatyczne sosny zwyczajnej ( Pinus sylvestris L.) w Polsce. Sylwan 8: 53–61. Wilczyński S. 2010. Uwarunkowania przyrostu radialnego wybranych gatunków drzew z Wyżyny Kieleckiej w świetle analiz

with VLA at both sites, but temperatures in March and May probably cause nonlinear reactions in VLA. Advanced ML algorithms can use this information and model the relationship between climate and VLA more accurately. ML methods such as ANN should, therefore, become a more standard approach in dendroclimatology. Despite the obvious outperformance of ANN over all the other regression methods used in our study, we recommend testing several different regression algorithms and selecting the optimal one for climate reconstruction. In a related study, Jevšenak et al