Address: 17 Naberezhnaya Severnoy Dviny, Arkhangelsk 163002 Russian Federation. Northern (Arctic) Federal University named after M.V.Lomonosov. Office 1425
Phone / Fax: (818-2) 21-61-18 Archive |
These works are licensed under a Creative Commons Attribution 4.0 International License. A.S. Alekseev, S.K. Sharma Complete text of the article:Download article (pdf, 1.5MB )UDС630*561.24:582.47DOI:10.37482/0536-1036-2020-3-42-54AbstractThe Lisino training and experimental forest of the Saint-Petersburg State Forest Technical University was chosen as a study area. The forest is located in the central part of the Leningrad region and has a high level of protection as a forest of scientific and historical value. According to the official data, mean annual temperature in the region increased by 0.6 °C within 10 years as well as precipitation. The impact determination of changing climate conditions on Norway spruce trees growth was the aim of this study. Three most representative compartments dominated by Norway spruce (Picea abies (L.) Karst.) were selected for data collection. Core samples were taken by the Pressler increment borer from 107 dominant trees while climatic data were obtained from the nearest weather stations. Tree rings were measured and analyzed using WinDendro software while climate data were processed by Microsoft Excel. Tree ring data cover the time interval from 1848 to 2011, each ring was characterized by width, calendar year, age and diameter of the tree. Radial growth was analyzed within age and diameter classes. Annual rings widths were varied from 0.1 to 6 mm. There was a positive trend in age classes of 0-20, 21-40 and 41-60 years old. The growth was very slow in the age classes of 61-80, 81-100 and >100. Diameters are larger in the age classes of 20-40 and 41-60 as compare to the local diameter growth table which was developed in the 19th century. Diameters for age classes older than 41-60 years were less than prescribed by the diameter growth table. Annual rings width for all age classes also demonstrate cyclic dynamics, moreover, the decline in growth sometimes occurred in recent decades. Multiple regression was used for developing the response function of growth to changes in climatic conditions. There was revealed a high correlation (90 %) and low influence of vegetation period climate data on growth during 1848–2011 (0.08102 mm/°C and 0.00085 mm/mm). Likewise, analysis shows that growth is higher in young and middle-aged than mature and over mature stands. Overall, climate change impact has a positive effect on the radial growth of Norway spruce for the studied area, however, not for all age and diameter classes.AuthorsA.S. Alekseev1, Doctor of Geography, Prof., Head of the Department of Forest Inventory, Management and GIS; ResearcherID: F-6891-2010,ORCID: https://orcid.org/0000-0001-8795-2888 S.K. Sharma2, MS in Forestry, Program Coordinator; ResearcherID: AAD-8788-2019, ORCID: https://orcid.org/0000-0003-4952-748X Affiliation1Saint-Petersburg State Forest Technical University, Institutskiy per., 5, Saint Petersburg, 194021, Russian Federation; e-mail: a_s_alekseev@mail.ru2The Resource Nepal, Santinagar, Post Box No. 24609, Kathmandu, Federal Democratic Republic of Nepal; e-mail: sk_victory@hotmail.com KeywordsNorway spruce, annual ring width, climate change, age classes, growth trend, temperature, precipitationsFor citationAlekseev A.S., Sharma S.K. Long-Term Growth Trends Analysis of Norway Spruce Stands in Relation to Possible Climate Change: Case Study of Leningrad Region. Lesnoy Zhurnal [Russian Forestry Journal], 2020, no. 3, pp. 42–54. DOI: 10.37482/0536-1036-2020-3-42-54References1. Alekseev A.S., Soroka A.R. Analysis of the Long-Term Trends of Pinus sylvestris (Pinaceae) Growth of the North-Western Kola Peninsula. Botanicheskii Zhurnal, 2003, vol. 88, no. 6, pp. 59–85.2. Vaganov E.A., Skomarkova M.V., Schulze E.-D., Linke P. The Influence of Climatic Factors on Wood Increment and Density of Tree Rings in Spruce and Pine in Mountains of Northern Italy. Lesovedenie [Russian Journal of Forest Science], 2007, no. 2, pp. 37–44. 3. Vaganov E.A., Shashkin A.V. Coniferous Species Tree Rings Growth and Structure. Novosibirsk, Nauka Publ., 2000. 232 p. 4. Second Assessment Report of Federal Service of Hydrometeorology and Environmental Monitoring about Climate Changes and Their Consequences on Territory of Russian Federation. Technical Resume. Moscow, Rosgidromet Publ., 2014. 94 p. 5. Abrams M.D., van de Gevel S., Dodson R.C., Copenheaver C.A. The Dendroecology and Climatic Impacts for Old-Growth White Pine and Hemlock on the Extreme Slopes of the Berkshire Hills, Massachusetts, USA. Canadian Journal of Botany, 2000, vol. 78, no. 7, pp. 851–861. DOI: 10.1139/b00-057 6. Alekseev A.S., Sharma Kumar S. Norway Spruce Trees Long-Term Growth with Account for Possible Climate Change in the Leningrad Region of Russian Federation. IUFRO 125th Anniversary Congress, 18–22 September 2017, Freiburg, Germany. Freiburg, IUFRO, 2017, art. IUFRO17-457. 7. Alekseev A.S., Soroka A.R. Scots Pine Growth Trends in Northwestern Kola Peninsula as an Indicator of Positive Changes in the Carbon Cycle. Climatic Change, 2002, vol. 55, iss. 1-2, pp. 183–196. DOI: 10.1023/A:1020271629819 8. Badeau V., Becker M., Bert D., Dupouey J.L., Lebourgeois F., Picard J.-F. LongTerm Growth Trends of Trees: Ten Years of Dendrochronological Studies in France. Growth Trends in European Forests. Ed. by H. Spiecker, K. Mielikäinen, M. Köhl, J.P. Skovsgaard. Berlin, Springer, 1996, pp. 167–181. DOI: 10.1007/978-3-642-61178-0_14 9. Begon M., Townsend C.R., Harper J.L. Ecology: From Individuals to Ecosystems. Oxford, UK, Wiley-Blackwell, 2005. 750 p. 10. Chen P-Y., Welsh C., Hamann A. Geographic Variation in Growth Response of Douglas-Fir to Interannual Climate Variability and Projected Climate Change. Global Change Biology, 2010, vol. 16, iss. 12, pp. 3374–3385. DOI: 10.1111/j.1365-2486.2010.02166.x 11. Chhin S. Influence of Climate on the Growth of Hybrid Poplar in Michigan. Forests, 2010, vol. 1, iss. 4, pp. 209–229. DOI: 10.3390/f1040209 12. Chhin S., Chumack K., Dahl T., David E.T., Kurzeja P., Magruder M., Telewski F.W. Growth-Climate Relationships of Pinus strobus in the Floodway versus Terrace Forest along the Banks of the Red Cedar River, Michigan. Tree-Ring Research, 2013, vol. 69, iss. 2, pp. 37–47. DOI: 10.3959/1536-1098-69.2.37 13. Chhin S., Zalesny Jr. R.S., Parker W.C., Brissette J. Dendroclimatic Analysis of White Pine (Pinus strobus L.) Using Long-Term Provenance Test Sites across Eastern North America. Forest Ecosystems, 2018, vol. 5, art. 18. DOI: 10.1186/s40663-018-0136-0 14. Fritts H.C. Tree Rings and Climate. London, Academic Press, 1976. 567 p. 15. Jiao L., Jiang Y., Wang M., Zhang W., Zhang Y. Age-Effect Radial Growth Responses of Picea schrenkiana to Climate Change in the Eastern Tianshan Mountains, Northwest China. Forests, 2017, vol. 8, iss. 9, art. 294. DOI: 10.3390/f8090294 16. Juknys R., Stravinskiene V., Vencloviene J. Tree-Ring Analysis for the Assessment of Anthropogenic Changes and Trends. Environmental Monitoring and Assessment, 2002, vol. 77, pp. 81–97. DOI: 10.1023/a:1015718519559 17. Juknys R., Vencloviene J., Stravinskiene V., Augustaitis A., Bartkevicius E. Scots Pine (Pinus sylvestris L.) Growth and Condition in a Polluted Environment: From Decline to Recovery. Environmental Pollution, 2003, vol. 125, iss. 2, pp. 205–212. DOI: 10.1016/S0269-7491(03)00070-8 18. Körner C. Significance of Temperature in Plant Life. Plant Growth and Climate Change. Ed. by J.I.L. Morison, M.D. Morecroft. UK, Blackwell Publishing, 2006, pp. 48–70. DOI: 10.1002/9780470988695.ch3 19. Myneni R.B., Keeling C.D., Tucker C.J., Asrar G., Nemani R.R. Increased Plant Growth in the Northern High Latitudes from 1981 to 1991. Nature, 1997, vol. 386, pp. 698–702. DOI: 10.1038/386698a0 20. Rodríguez-Catón M., Villalba R., Srur A.M., Luckman B. Long-Term Trends in Radial Growth Associated with Nothofagus pumilio Forest Decline in Patagonia: Integrating Local- into Regional-Scale Patterns. Forest Ecology and Management, 2015, vol. 339, pp. 44–56. DOI: 10.1016/j.foreco.2014.12.004 21. Schadauel K. Growth Trends in Austria. Growth Trends in European Forests. Ed. by H. Spiecker, K. Mielikäinen, M. Köhl, J.P. Skovsgaard. Berlin, Springer, 1996, pp. 275–289. DOI: 10.1007/978-3-642-61178-0_20 22. Schneider O., Hartmann F. Growth Trends of Trees. Regional Study on Norway Spruce (Picea abies (L.) Karst.) in the Swiss Jura. Growth Trends in European Forests. Ed. by H. Spiecker, K. Mielikäinen, M. Köhl, J.P. Skovsgaard. Berlin, Springer, 1996, pp. 183–198. DOI: 10.1007/978-3-642-61178-0_15 23. Stravinskienė V. Dendrochronological Indication of Climatic Factors and Anthropogenic Environmental Trends in Lithuania. Dr. Habilitation Dissertation. Kaunas, Lithuania, Vytautas Magnus University, 2002. 175 p. 24. Stravinskienè V., Bartkevičius E., Plaušinytè E. Impact of Industrial Pollution on Scots Pine (Pinus sylvestris L.) Radial Growth in the Areas of Mineral Fertilizer Factory “Achema”. Russian Journal of Ecology, 2014, vol. 45, iss. 6, pp. 525–531. DOI: 10.1134/S1067413614060137 25. Wang H., Shao X.-M., Jiang Y., Fang X.-Q., Wu S.-H. The Impacts of Climate Change on the Radial Growth of Pinus koraiensis along Elevations of Changbai Mountain in Northeastern China. Forest Ecology and Management, 2013, vol. 289, pp. 333–340. DOI: 10.1016/j.foreco.2012.10.023 Long-Term Growth Trends Analysis of Norway Spruce Stands in Relation to Possible Climate Change: Case Study of Leningrad Region |
Make a Submission
Lesnoy Zhurnal (Russian Forestry Journal) was awarded the "Seal of Recognition for Active Data Provider of the Year 2024" INDEXED IN:
|
|
|
|
|
|
|
|
|
|
|
|
|