The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain

24 cm The growth/climate response of Norway spruce in the timberline ecotone of Babia Góra Mountain was examined. Based on a pool of 708 trees from 10 sites, the influence of age, exposure, and method of computingchronology, was assessed. Gridded data and 12 instrumental series were used to study th...

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Published in:Forest Ecology and Management
Main Authors: Kaczka, Ryszard J., Czajka, Barbara, Łajczak, Adam
Format: Text
Language:English
Published: IGiPZ PAN 2015
Subjects:
Babia Góra Mountain
Carpathians
climate
dendrochronology
Norway spruce
tree-rings
Babia Góra
Karpaty
klimat
dendrochronologia
świerk norweski
przyrosty drzew
Norway
Arctic
Online Access:https://rcin.org.pl/dlibra/publication/edition/54616/content
id ftrcin:oai:rcin.org.pl:54616
record_format openpolar
institution Open Polar
collection Digital Repository of Scientific Institutes (RCIN)
op_collection_id ftrcin
language English
topic Babia Góra Mountain
Carpathians
climate
dendrochronology
Norway spruce
tree-rings
Babia Góra
Karpaty
klimat
dendrochronologia
świerk norweski
przyrosty drzew
spellingShingle Babia Góra Mountain
Carpathians
climate
dendrochronology
Norway spruce
tree-rings
Babia Góra
Karpaty
klimat
dendrochronologia
świerk norweski
przyrosty drzew
Kaczka, Ryszard J.
Czajka, Barbara
Łajczak, Adam
The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain
topic_facet Babia Góra Mountain
Carpathians
climate
dendrochronology
Norway spruce
tree-rings
Babia Góra
Karpaty
klimat
dendrochronologia
świerk norweski
przyrosty drzew
description 24 cm The growth/climate response of Norway spruce in the timberline ecotone of Babia Góra Mountain was examined. Based on a pool of 708 trees from 10 sites, the influence of age, exposure, and method of computingchronology, was assessed. Gridded data and 12 instrumental series were used to study the spatiotemporal relationship of the tree growth and climate. Temperature mainly controls the growth of the Norway spruce in thetimberline ecotone at Babia Góra Mountain. The most important factors were the June and July temperatures (r = 0.57) and of the entire growing season April-September (r = 0.52). The precipitation of late winter (Marchand correspondingly the January-March season) had a positive influence on the tree growth. The previously reported negative correlation with the summer precipitation was found but it was less important. The maturetrees growing on the northern slope showed a response to the summer temperature in a stronger manner than all the other groups. The low-frequency SPL chronologies (detrended using the cubic smoothing splinesmethod) performed better than the RCS (regional curve standardisation) of the high-frequency SPL. A strong correlation was found with Obidowa, the nearest located instrumental data (a distance of 35 km), and theHala Gąsienicowa, the station located at a similar elevation a.s.l. (1508 m a.s.l.), but also with the Krakow located farther away and at a lower elevation (237 m a.s.l.). The TRW/temperature correlation was temporallymost stable in the case of Zakopane. 24 cm The growth/climate response of Norway spruce in the timberline ecotone of Babia Góra Mountain was examined. Based on a pool of 708 trees from 10 sites, the influence of age, exposure, and method of computingchronology, was assessed. Gridded data and 12 instrumental series were used to study the spatiotemporal relationship of the tree growth and climate. Temperature mainly controls the growth of the Norway spruce in thetimberline ecotone at Babia Góra Mountain. The most important factors were the ...
format Text
author Kaczka, Ryszard J.
Czajka, Barbara
Łajczak, Adam
author_facet Kaczka, Ryszard J.
Czajka, Barbara
Łajczak, Adam
author_sort Kaczka, Ryszard J.
title The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain
title_short The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain
title_full The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain
title_fullStr The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain
title_full_unstemmed The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain
title_sort tree-ring growth responses to climate in the timberline ecotone of babia góra mountain
publisher IGiPZ PAN
publishDate 2015
url https://rcin.org.pl/dlibra/publication/edition/54616/content
geographic Norway
geographic_facet Norway
genre Arctic
genre_facet Arctic
op_source CBGiOS. IGiPZ PAN, call nos.: Cz.2085, Cz.2173, Cz.2406
http://195.187.71.2/ipac20/ipac.jsp?profile=geogpan&index=BOCLC&term=ee95400564
CBGiOS. IGiPZ PAN, sygn.: Cz.2085, Cz.2173, Cz.2406
op_relation Geographia Polonica
1. BEBI P., KULAKOWSKI D., RIXEN C., 2009. Snow avalanche disturbances in forest ecosystems – State of research and implications for management. Forest Ecology and Management, vol. 257, no. 9, pp. 1883-1892.
http://dx.doi.org/10.1016/j.foreco.2009.01.050 -
2. Bednarz Z., 1996. June-July temperature variation for the Babia Góra National Park, Southern Poland, for the period 1650-1910 [in:] B. Obrębska-Starklowa, T. Niedźwiedź (eds.), Proceedings of the International conference on climate dynamics and the global change perspective, Kraków, 17-20 październik 1995, Zeszyty Naukowe Uniwersytetu Jagiellońskiego. Prace Geograficzne, 102, pp. 523-529.
3. Bednarz Z., Jaroszewicz B., Ptak J., Szwagrzyk J., 1999. Dendrochronology of Norway Spruce (Picea Abies (L. Karst) in the Babia Gora National Park, Poland. Dendrochronologia, 16, pp. 45-55.
4. BEDNARZ Z., HOLEKSA J., RÓŻAŃSKI W., SZWAGRZYK J., WILCZEK Z., ŻYWIEC M., 2009. Altitudinal ranges of forest and shrub communities in the Babia Góra Massif (West Carpathians) [in:] J. Holeksa, B. Babczyńska-Sendek, S. Wika (eds.), The role of geobotany in biodiversity conservation, Katowice: University of Silesia, pp. 71-80.
5. BEDNORZ F., 2000. Der Abbau der organischen Substanz im Waldgrenzökoton am Stillberg (Dischmatal/Schweiz). Arbeiten aus dem Institut für Landschaftsökologie 7, Münster: Institut für Landschaftsökologie.
6. Briffa K.R., Schweingruber F.H., Jones P.D., OSBORN T.J., SHIYATOV S.G., VAGANOV E.A., 1998. Reduced sensitivity of recent tree-growth to temperature at high northern latitudes. Nature, vol. 391, no. 6668, pp. 678-682.
http://dx.doi.org/10.1038/35596 -
7. Briffa K.R., Osborn T.J., Schweingruber F.H., Jones P.D., Shiyatov S.G., Vaganov E.A., 2002. Tree-ring width and density data around the Northern Hemisphere: Part 1, local and regional climate signals. The Holocene, vol. 12, no. 6, pp. 737-757.
http://dx.doi.org/10.1191/0959683602hl588rp -
http://dx.doi.org/10.1191/0959683602hl587rp -
8. Büntgen U., Frank D.C., Kaczka R.J., Verstege A., Zwijacz-Kozica T., Esper J., 2007. Growth responses to climate in a multi-species tree-ring network in the Western Carpathian Tatra Mountains, Poland and Slovakia. Tree Physiology, vol. 27, no. 5, pp. 689-702.
http://dx.doi.org/10.1093/treephys/27.5.689 -
9. Büntgen U., Frank D.C., Wilson R., Career M., Urbinati C., Esper J., 2008. Testing for tree-ring divergence in the European Alps. Global Change Biology, vol. 14, no. 10, pp. 2433-2453.
http://dx.doi.org/10.1111/j.1365-2486.2008.01640.x -
10. Büntgen U., Tegel W., Heussner K.U., HOFMANN J., KONTIC R., KYNCL T., COOK E.R., 2012. Effects of sample size in dendroclimatology. Climate Research, 53, pp. 263-269.
11. Carrer M., Urbinati C., 2001. Assessing climate- -growth relationships: A comparative study between linear and non-linear methods. Dendrochronologia, 19, pp. 57-65.
12. Carrer M., Urbinati C., 2004. Age-dependent tree-ring growth responses to climate in Larix decidua and Pinus cembra. Ecology, vol. 85, no. 3, pp. 730-740.
http://dx.doi.org/10.1890/02-0478 -
13. COOK E.R., PETERS K., 1981. The smoothing spline: a new approach to standardizing forest interior tree-ring width series for dendroclimatic studies. Tree-Ring Bulletin, 41, pp. 45-53
14. COOK E.R., HOLMES R.L., 1986. User's manual for computer program ARSTAN [in:] R.L. Holmes, R.K. Adams, H.C. Fritts (eds.), Tree ring chronologies of western North America: California, eastern Oregon and northern Great Basin, Chronology Ser. 6., Tucson: Univeristy of Arizona, pp. 50-56.
15. Czajka B., 2012. Wpływ wysokości n.p.m. na wrażliwość klimatyczną świerka pospolitego w masywie Babiej Góry. Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej, vol. 1, no. 30, pp. 91-97
16. CZAJKA B., KACZKA R.J. 2014. Dendrochronologiczna charakterystyka górnej granicy lasu na Babiej Górze w strefie jej progresu. Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej, vol.16, no. 40, pp. 42-52.
17. CZAJKA B., ŁAJCZAK A., KACZKA R.J., 2015. The dynamics of the timberline ecotone on the asymmetric ridge of the Babia Góra Massif, Western Carpathians. Geographia Polonica, vol. 88, no. 2, pp. 85-102.
18. D'Arrigo R., Wilson R., Liepert B., Cherubini P., 2008. On the 'divergence problem' in northern forests: A review of the tree-ring evidence and possible causes. Global and Planetary Change, vol. 60, no. 3, pp. 289-305.
http://dx.doi.org/10.1016/j.gloplacha.2007.03.004 -
19. Daubenmire R., 1954. Alpine timberlines in the Americas and their interpretation. Butler University Botanical Studies, 2, pp. 119-136.
20. ESPER J., COOK E.R., KRUSIC P.J., PETERS K., SCHWEINGRUBER F.H., 2003. Tests of the RCS method for preserving low-frequency variability in long treering chronologies. Tree-ring research. vol. 59, no. 2, pp. 81-98.
21. Esper J., Niederer R., Bebi P., Frank D., 2008. Climate signal age effects – evidence from young and old trees in the Swiss Engadin. Forest Ecology and Management, vol. 25, no. 11, pp. 3783-3789.
http://dx.doi.org/10.1016/j.foreco.2008.03.015 -
22. Esper, J., Frank, D.C., 2009. Divergence pitfalls in tree-ring research. Climatic Change, vol. 94, no. 3, pp. 261-266.
http://dx.doi.org/10.1007/s10584-009-9594-2 -
23. Esper J., Frank D., Büntgen U., Verstege A., Hantemirov R.M., Kirdyanov A.V., 2010. Trends and uncertainties in Siberian indicators of 20th century warming. Global Change Biology, vol. 16, no. 1, pp. 386-398.
http://dx.doi.org/10.1111/j.1365-2486.2009.01913.x -
24. Frank D., Esper J., 2005. Characterization and climate response patterns of a high-elevation, multi-species tree-ring network for the European Alps. Dendrochronologia, 22, pp. 107-121.
http://dx.doi.org/10.1016/j.dendro.2005.02.004 -
25. FRIES T.C.E., 1913. Botanische Untersuchungen im nördlichsten Schweden: Ein Beitrag zur Kenntnis der alpinen und subalpinen Vegetation in Torne Lappmark. Vetenskapliga och praktiska undersökningar i Lappland, Flora ich Fauna, vol. 2, 361 pp.
26. Fritts, H.C. 1976. Tree rings and climate. London: Academic Press.
27. Grace J., 1977. Plant response to wind. London: Academic Press.
28. Grissino-Mayer H.D., 2001. Evaluating crossdating accuracy: A manual and tutorial for the computer program COFECHA. Tree-Ring Research, vol. 57, no. 2, pp. 205-221.
29. GUZIK M., 2008. Analiza wpływu czynników naturalnych i antropogenicznych na kształtowanie się zasięgu lasu i kosodrzewiny w Tatrach. Kraków: Uniwersytet Rolniczy im. Hugona Kołłątaja. Wydział Leśny. Katedra Botaniki Leśnej i Ochrony Przyrody [PhD thesis].
30. Haylock M.R., Hofstra N., Klein Tank A.M.G., Klok E.J., Jones P.D., New M., 2008. A European daily high-resolution gridded dataset of surface temperature and precipitation. Journal of Geophysical Research: Atmospheres, vol. 113, D20119.
31. Hess M., 1965. Piętra klimatyczne w polskich Karpatach Zachodnich. Zeszyty Naukowe Uniwersytetu Jagiellońskiego. Prace Instytutu Geograficznego 33, Kraków: Uniwersytet Jagielloński.
32. Hoch G., Popp M., Körner Ch., 2002. Altitudinal increase of mobile carbon pools in Pinus cembra suggests sink limitation of growth at the Swiss treeline. Oikos, vol. 98, no. 3, pp. 361-374.
http://dx.doi.org/10.1034/j.1600-0706.2002.980301.x -
33. Holtmeier F.K., 1973. Geoecological aspects of timberline in northern and central Europe. Arctic and Alpine Researches, vol. 5, no. 3, pp. 45-54.
34. Holtmeier F.K., 1974. Geooekologische Beobachtungen und Studienan der subarktischen und alpinen Waldgrenze in vergleichender Sicht. Wiesbaden: Franz Steiner.
35. Imhof E., 1900. Die Waldgrenze in der Schweiz, Gerlands Beitr. Geophysik, 4, pp. 241-330.
36. Kaczka R.J., Büntgen U., 2006. Spatial autocorrelation and growth/climate response of a high elevation spruce network along the Carpathian arc. TRACE, 6, pp. 103-112.
op_rights Creative Commons Attribution BY-ND 3.0 PL license
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spelling ftrcin:oai:rcin.org.pl:54616 2023-05-15T14:28:28+02:00 The tree-ring growth responses to climate in the timberline ecotone of Babia Góra Mountain Geographia Polonica Vol. 88 No. 2 (2015) Kaczka, Ryszard J. Czajka, Barbara Łajczak, Adam 2015 File size 3,5 MB application/pdf Rozmiar pliku 3,5 MB https://rcin.org.pl/dlibra/publication/edition/54616/content eng eng IGiPZ PAN Geographia Polonica 1. BEBI P., KULAKOWSKI D., RIXEN C., 2009. Snow avalanche disturbances in forest ecosystems – State of research and implications for management. Forest Ecology and Management, vol. 257, no. 9, pp. 1883-1892. http://dx.doi.org/10.1016/j.foreco.2009.01.050 - 2. Bednarz Z., 1996. June-July temperature variation for the Babia Góra National Park, Southern Poland, for the period 1650-1910 [in:] B. Obrębska-Starklowa, T. Niedźwiedź (eds.), Proceedings of the International conference on climate dynamics and the global change perspective, Kraków, 17-20 październik 1995, Zeszyty Naukowe Uniwersytetu Jagiellońskiego. Prace Geograficzne, 102, pp. 523-529. 3. Bednarz Z., Jaroszewicz B., Ptak J., Szwagrzyk J., 1999. Dendrochronology of Norway Spruce (Picea Abies (L. Karst) in the Babia Gora National Park, Poland. Dendrochronologia, 16, pp. 45-55. 4. BEDNARZ Z., HOLEKSA J., RÓŻAŃSKI W., SZWAGRZYK J., WILCZEK Z., ŻYWIEC M., 2009. Altitudinal ranges of forest and shrub communities in the Babia Góra Massif (West Carpathians) [in:] J. Holeksa, B. Babczyńska-Sendek, S. Wika (eds.), The role of geobotany in biodiversity conservation, Katowice: University of Silesia, pp. 71-80. 5. BEDNORZ F., 2000. Der Abbau der organischen Substanz im Waldgrenzökoton am Stillberg (Dischmatal/Schweiz). Arbeiten aus dem Institut für Landschaftsökologie 7, Münster: Institut für Landschaftsökologie. 6. Briffa K.R., Schweingruber F.H., Jones P.D., OSBORN T.J., SHIYATOV S.G., VAGANOV E.A., 1998. Reduced sensitivity of recent tree-growth to temperature at high northern latitudes. Nature, vol. 391, no. 6668, pp. 678-682. http://dx.doi.org/10.1038/35596 - 7. Briffa K.R., Osborn T.J., Schweingruber F.H., Jones P.D., Shiyatov S.G., Vaganov E.A., 2002. Tree-ring width and density data around the Northern Hemisphere: Part 1, local and regional climate signals. The Holocene, vol. 12, no. 6, pp. 737-757. http://dx.doi.org/10.1191/0959683602hl588rp - http://dx.doi.org/10.1191/0959683602hl587rp - 8. Büntgen U., Frank D.C., Kaczka R.J., Verstege A., Zwijacz-Kozica T., Esper J., 2007. Growth responses to climate in a multi-species tree-ring network in the Western Carpathian Tatra Mountains, Poland and Slovakia. Tree Physiology, vol. 27, no. 5, pp. 689-702. http://dx.doi.org/10.1093/treephys/27.5.689 - 9. Büntgen U., Frank D.C., Wilson R., Career M., Urbinati C., Esper J., 2008. Testing for tree-ring divergence in the European Alps. Global Change Biology, vol. 14, no. 10, pp. 2433-2453. http://dx.doi.org/10.1111/j.1365-2486.2008.01640.x - 10. Büntgen U., Tegel W., Heussner K.U., HOFMANN J., KONTIC R., KYNCL T., COOK E.R., 2012. Effects of sample size in dendroclimatology. Climate Research, 53, pp. 263-269. 11. Carrer M., Urbinati C., 2001. Assessing climate- -growth relationships: A comparative study between linear and non-linear methods. Dendrochronologia, 19, pp. 57-65. 12. Carrer M., Urbinati C., 2004. Age-dependent tree-ring growth responses to climate in Larix decidua and Pinus cembra. Ecology, vol. 85, no. 3, pp. 730-740. http://dx.doi.org/10.1890/02-0478 - 13. COOK E.R., PETERS K., 1981. The smoothing spline: a new approach to standardizing forest interior tree-ring width series for dendroclimatic studies. Tree-Ring Bulletin, 41, pp. 45-53 14. COOK E.R., HOLMES R.L., 1986. User's manual for computer program ARSTAN [in:] R.L. Holmes, R.K. Adams, H.C. Fritts (eds.), Tree ring chronologies of western North America: California, eastern Oregon and northern Great Basin, Chronology Ser. 6., Tucson: Univeristy of Arizona, pp. 50-56. 15. Czajka B., 2012. Wpływ wysokości n.p.m. na wrażliwość klimatyczną świerka pospolitego w masywie Babiej Góry. Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej, vol. 1, no. 30, pp. 91-97 16. CZAJKA B., KACZKA R.J. 2014. Dendrochronologiczna charakterystyka górnej granicy lasu na Babiej Górze w strefie jej progresu. Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej, vol.16, no. 40, pp. 42-52. 17. CZAJKA B., ŁAJCZAK A., KACZKA R.J., 2015. The dynamics of the timberline ecotone on the asymmetric ridge of the Babia Góra Massif, Western Carpathians. Geographia Polonica, vol. 88, no. 2, pp. 85-102. 18. D'Arrigo R., Wilson R., Liepert B., Cherubini P., 2008. On the 'divergence problem' in northern forests: A review of the tree-ring evidence and possible causes. Global and Planetary Change, vol. 60, no. 3, pp. 289-305. http://dx.doi.org/10.1016/j.gloplacha.2007.03.004 - 19. Daubenmire R., 1954. Alpine timberlines in the Americas and their interpretation. Butler University Botanical Studies, 2, pp. 119-136. 20. ESPER J., COOK E.R., KRUSIC P.J., PETERS K., SCHWEINGRUBER F.H., 2003. Tests of the RCS method for preserving low-frequency variability in long treering chronologies. Tree-ring research. vol. 59, no. 2, pp. 81-98. 21. Esper J., Niederer R., Bebi P., Frank D., 2008. Climate signal age effects – evidence from young and old trees in the Swiss Engadin. Forest Ecology and Management, vol. 25, no. 11, pp. 3783-3789. http://dx.doi.org/10.1016/j.foreco.2008.03.015 - 22. Esper, J., Frank, D.C., 2009. Divergence pitfalls in tree-ring research. Climatic Change, vol. 94, no. 3, pp. 261-266. http://dx.doi.org/10.1007/s10584-009-9594-2 - 23. Esper J., Frank D., Büntgen U., Verstege A., Hantemirov R.M., Kirdyanov A.V., 2010. Trends and uncertainties in Siberian indicators of 20th century warming. Global Change Biology, vol. 16, no. 1, pp. 386-398. http://dx.doi.org/10.1111/j.1365-2486.2009.01913.x - 24. Frank D., Esper J., 2005. Characterization and climate response patterns of a high-elevation, multi-species tree-ring network for the European Alps. Dendrochronologia, 22, pp. 107-121. http://dx.doi.org/10.1016/j.dendro.2005.02.004 - 25. FRIES T.C.E., 1913. Botanische Untersuchungen im nördlichsten Schweden: Ein Beitrag zur Kenntnis der alpinen und subalpinen Vegetation in Torne Lappmark. Vetenskapliga och praktiska undersökningar i Lappland, Flora ich Fauna, vol. 2, 361 pp. 26. Fritts, H.C. 1976. Tree rings and climate. London: Academic Press. 27. Grace J., 1977. Plant response to wind. London: Academic Press. 28. Grissino-Mayer H.D., 2001. Evaluating crossdating accuracy: A manual and tutorial for the computer program COFECHA. Tree-Ring Research, vol. 57, no. 2, pp. 205-221. 29. GUZIK M., 2008. Analiza wpływu czynników naturalnych i antropogenicznych na kształtowanie się zasięgu lasu i kosodrzewiny w Tatrach. Kraków: Uniwersytet Rolniczy im. Hugona Kołłątaja. Wydział Leśny. Katedra Botaniki Leśnej i Ochrony Przyrody [PhD thesis]. 30. Haylock M.R., Hofstra N., Klein Tank A.M.G., Klok E.J., Jones P.D., New M., 2008. A European daily high-resolution gridded dataset of surface temperature and precipitation. Journal of Geophysical Research: Atmospheres, vol. 113, D20119. 31. Hess M., 1965. Piętra klimatyczne w polskich Karpatach Zachodnich. Zeszyty Naukowe Uniwersytetu Jagiellońskiego. Prace Instytutu Geograficznego 33, Kraków: Uniwersytet Jagielloński. 32. Hoch G., Popp M., Körner Ch., 2002. Altitudinal increase of mobile carbon pools in Pinus cembra suggests sink limitation of growth at the Swiss treeline. Oikos, vol. 98, no. 3, pp. 361-374. http://dx.doi.org/10.1034/j.1600-0706.2002.980301.x - 33. Holtmeier F.K., 1973. Geoecological aspects of timberline in northern and central Europe. Arctic and Alpine Researches, vol. 5, no. 3, pp. 45-54. 34. Holtmeier F.K., 1974. Geooekologische Beobachtungen und Studienan der subarktischen und alpinen Waldgrenze in vergleichender Sicht. Wiesbaden: Franz Steiner. 35. Imhof E., 1900. Die Waldgrenze in der Schweiz, Gerlands Beitr. Geophysik, 4, pp. 241-330. 36. Kaczka R.J., Büntgen U., 2006. Spatial autocorrelation and growth/climate response of a high elevation spruce network along the Carpathian arc. TRACE, 6, pp. 103-112. Creative Commons Attribution BY-ND 3.0 PL license Licencja Creative Commons Uznanie autorstwa-Bez utworów zależnych 3.0 Polska CC-BY CC-BY-ND CBGiOS. IGiPZ PAN, call nos.: Cz.2085, Cz.2173, Cz.2406 http://195.187.71.2/ipac20/ipac.jsp?profile=geogpan&index=BOCLC&term=ee95400564 CBGiOS. IGiPZ PAN, sygn.: Cz.2085, Cz.2173, Cz.2406 Babia Góra Mountain Carpathians climate dendrochronology Norway spruce tree-rings Babia Góra Karpaty klimat dendrochronologia świerk norweski przyrosty drzew Text Tekst 2015 ftrcin https://doi.org/10.1016/j.foreco.2009.01.050 https://doi.org/10.1038/35596 https://doi.org/10.1191/0959683602hl588rp https://doi.org/10.1191/0959683602hl587rp https://doi.org/10.1093/treephys/27.5.689 https://doi.org/10.1111/j.1365-2486.2008.016 2022-11-28T01:29:57Z 24 cm The growth/climate response of Norway spruce in the timberline ecotone of Babia Góra Mountain was examined. Based on a pool of 708 trees from 10 sites, the influence of age, exposure, and method of computingchronology, was assessed. Gridded data and 12 instrumental series were used to study the spatiotemporal relationship of the tree growth and climate. Temperature mainly controls the growth of the Norway spruce in thetimberline ecotone at Babia Góra Mountain. The most important factors were the June and July temperatures (r = 0.57) and of the entire growing season April-September (r = 0.52). The precipitation of late winter (Marchand correspondingly the January-March season) had a positive influence on the tree growth. The previously reported negative correlation with the summer precipitation was found but it was less important. The maturetrees growing on the northern slope showed a response to the summer temperature in a stronger manner than all the other groups. The low-frequency SPL chronologies (detrended using the cubic smoothing splinesmethod) performed better than the RCS (regional curve standardisation) of the high-frequency SPL. A strong correlation was found with Obidowa, the nearest located instrumental data (a distance of 35 km), and theHala Gąsienicowa, the station located at a similar elevation a.s.l. (1508 m a.s.l.), but also with the Krakow located farther away and at a lower elevation (237 m a.s.l.). The TRW/temperature correlation was temporallymost stable in the case of Zakopane. 24 cm The growth/climate response of Norway spruce in the timberline ecotone of Babia Góra Mountain was examined. Based on a pool of 708 trees from 10 sites, the influence of age, exposure, and method of computingchronology, was assessed. Gridded data and 12 instrumental series were used to study the spatiotemporal relationship of the tree growth and climate. Temperature mainly controls the growth of the Norway spruce in thetimberline ecotone at Babia Góra Mountain. The most important factors were the ... Text Arctic Digital Repository of Scientific Institutes (RCIN) Norway Forest Ecology and Management 257 9 1883 1892

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