DOI QR코드

DOI QR Code

Growth performance of planted population of Pinus roxburghii in central Nepal

  • Tiwari, Achyut (Central Department of Botany, Tribhuvan University) ;
  • Thapa, Nita (Central Department of Botany, Tribhuvan University) ;
  • Aryal, Sugam (Institute of Geography, University of Erlangen Nurnberg) ;
  • Rana, Prabina (Nepal Academy of Science and Technology) ;
  • Adhikari, Shankar (Ministry of Forests and Environment, Government of Nepal)
  • Received : 2020.07.09
  • Accepted : 2020.11.09
  • Published : 2020.12.31

Abstract

Background: Climate change has altered the various ecosystem processes including forest ecosystem in Himalayan region. Although the high mountain natural forests including treelines in the Himalayan region are mainly reported to be temperature sensitive, the temperature-related water stress in an important growth-limiting factor for middle elevation mountains. And there are very few evidences on growth performance of planted forest in changing climate in the Himalayan region. A dendrochronological study was carried out to verify and record the impact of warming temperature tree growth by using the tree cores of Pinus roxburghii from Batase village of Dhulikhel in Central Nepal with sub-tropical climatic zone. For this total, 29 tree cores from 25 trees of P. roxburghii were measured and analyzed. Result: A 44-year long tree ring width chronology was constructed from the cores. The result showed that the radial growth of P. roxburghii was positively correlated with pre-monsoon (April) rainfall, although the correlation was not significant and negatively correlated with summer rainfall. The strongest negative correlation was found between radial growth and rainfall of June followed by the rainfall of January. Also, the radial growth showed significant positive correlation with that previous year August mean temperature and maximum temperature, and significant negative correlation between radial growth and maximum temperature (Tmax) of May and of spring season (March-May), indicating moisture as the key factor for radial growth. Despite the overall positive trend in the basal area increment (BAI), we have found the abrupt decline between 1995 and 2005 AD. Conclusion: The results indicated that chir pine planted population was moisture sensitive, and the negative impact of higher temperature during early growth season (March-May) was clearly seen on the radial growth. We emphasize that the forest would experience further moisture stress if the trend of warming temperatures continues. The unusual decreasing BAI trend might be associated with forest management processes including resin collection and other disturbances. Our results showed that the planted pine forest stand is sub-healthy due to major human intervention at times. Further exploration of growth climate response from different climatic zones and management regimes is important to improve our understanding on the growth performance of mid-hill pine forests in Nepal.

Keywords

Acknowledgement

We would like to acknowledge the Ministry of Forests and Environment, Government of Nepal for providing financial support, and members of the Batase Community Forest Users Group of Dhulikhel Central Nepal for sample collection permission for this research work. We are grateful to Nepal Academy of Science and Technology (NAST) Nepal for providing lab work permission in the Dendrolab. Further, Saroj Basnet of NAST and Mr. Basu Dev Paudel are acknowledged for their kind cooperation on sample measurement and preparation of study area map.

References

  1. Aryal S, Bhuju DR, Kharal DK, Gaire NP, Dyola N. Climatic upshot using growth patternof Pinus roxburghii from western Nepal. Pak J Bot. 2018;50(2):579-88.
  2. Bhattacharyya A, La Marche VC, Hughes MK. Tree-ring chronologies from Nepal. Tree Ring Bulletin. 1992;52:59-66.
  3. Bhuju DR, Gaire NP. Plantation history and growth of old Pine stands in Kathmandu valley: a dendrochronological approach. FUUAST J. Biol. 2012;2(2):13-7.
  4. Borgaonkar HP, Pant GB, Kumar KR. Tree-ring chronologies from Western Himalaya and their dendroclimatic potential. IAWA Journal. 1999;20(3):295-309. https://doi.org/10.1163/22941932-90000692
  5. Borgaonkar HP, Sikder AB, Ram S. High altitude forest sensitivity to the recent warming: a tree-ring analysis of conifers from Western Himalaya, India. Quat Int. 2011;236:158-66. https://doi.org/10.1016/j.quaint.2010.01.016.
  6. Brown PM, Bhattacharyya A, Shah SK. Potential for developing fire histories in Chir Pine (Pinus roxburghii) forests in the Himalayan Foothills. Tree-ring Res. 2011;67(1):57-62. https://doi.org/10.3959/2009-15.1
  7. Cai Q, Liu Y, Qian H, Liu R. Inverse effects of recent warming on trees growing at the low and high altitudes of the Dabie Mountains, subtropical China. Dendrochronologia. 2020;59:125649. https://doi.org/10.1016/j.dendro.2019.125649
  8. Chhetri PK, Thapa S. Tree ring and climate change in Langtang National Park, central Nepal. Our Nature. 2010;8(1):139-43. https://doi.org/10.3126/on.v8i1.4321
  9. Cook ER. A time-series analysis approach to tree-ring standardization. Ph.D. Dissertation. The University of Arizona Press, Tucson; 1985.
  10. Cook ER, Kairiiukstis LA. Methods of dendrochronology: Applications in the Environmental Sciences. Dordrecht, The Netherlands: Kluwer Academic Publisher and International Institute for Applied System Analysis; 1990.
  11. Cook ER, Krusic PJ, Jones PD. Dendroclimatic signals in long tree - ring chronologies from the Himalayas of Nepal. Int J Climatol. 2003;23(7):707-32. https://doi.org/10.1002/joc.911
  12. Cook ER, Peters K. The smoothing spline: a new approach to standardizing forest interior tree-ring width series for dendroclimatic studies. Tree-Ring Bulletin. 1981;41:45-53.
  13. Core Team R. R: a language and environment for statistical computing. Vienna: R Foundation for Statistical Computing; 2019.
  14. Dawadi B, Liang E, Tian L, Devkota LP, Yao T. Premoonsoon precipitation signal in tree ring of timberline Betula utilis in Central Himalayas. Quat Int. 2013;283:72-7. https://doi.org/10.1016/j.quaint.2012.05.039
  15. DFRS. State of Nepal's Forests. Department of Forest Resource and Survey.: Kathmandu; 2015.
  16. DHM. Observed Climate Trend Analysis in the Districts and Physiographic Regions of Nepal (1971-2014). Department of Hydrology and Meteorology, Kathmandu; 2017.
  17. Duchesne L, Ouimet R, Morneau C. Assessment of sugar maple health based on basal area growth pattern. Can J For Res. 2003,33:2074-2080. https://doi.org/10.1139/x03-141
  18. Esper J, Cook E, Schweingruber F. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science. 2002;295:2250-3. https://doi.org/10.1126/science.1066208
  19. Fritts HC. Tree rings and climate. London: Academic Press; 1976.
  20. Gaire NP, Koirala M, Bhuju DR, Borgaonkar HP. Treeline dynamics with climate change at the central Nepal Himalaya. Clim Past. 2014;10(4):1277-90. https://doi.org/10.5194/cp-10-1277-2014
  21. Gaire, NP, Koirala, M, Bhuju, DR. Site- and species-specific treeline responses to climatic variability in eastern Nepal Himalaya. Dendrochronologia. 2017;41:44-56. https://doi.org/10.1016/j.dendro.2016.03.001
  22. Grissino-Mayer HD. Evaluating crossdating accuracy: a manual and tutorial for the computer program COFECHA. Tree-Ring Res. 2001;57(2):17.
  23. Harsch MA, Hulme PE, McGlone MS, Duncan RP. Are treelines advancing? A global meta-analysis of treeline response to climate warming. Ecol Lett. 2009;12:1040-9. https://doi.org/10.1111/j.1461-0248.2009.01355.x.
  24. Holmes RL. Computer-assisted quality control in tree-ring dating and measurement. Tree -Ring Bulletin. 1983;43:69-78.
  25. Holtmeier FK, Broll G. Treeline advance - driving processes and adverse factors. Landscape Online. 2007;1:1-33. https://doi.org/10.3097/LO.200701.
  26. Houghton J. Global warming: the complete briefing. Cambridge: Cambridge University Press; 2004.
  27. IPCC. Climate change 2013: the physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. New York: Cambridge University Press; 2013. p. 1535. https://doi.org/10.1029/2000JD000115.
  28. IPCC. Summary for policymakers. In Climate Change 2014: Impacts, Adaptation, and Vulnerability. Part A: Global and Sectoral Aspects.Contribution of Working Group II to Fifth Assessment Report of the Intergovernmental Panel on Climate Change (eds) FieldCB, BarrosVR, Dokken DJ, Mach KJ, Mastrandrea MD, Bilir TE, Chatterjee M, Ebi KL, Estrada YO, Genova RC, Girma B, Kissal ES, Levy AN, MacCracken S, Mastrandrea PR, White LL. Cambridge University Press, Cambridge, and New York. 2014: 1-32.
  29. Jackson JK. Manual of afforestation in Kathmandu, Nepal: Forest Research and Survey; 1994. p. 2.
  30. 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;8:294. https://doi.org/10.3390/f8090294.
  31. Jump AS, Hunt JM, Penuelas J. Rapid climate change-related growth decline at the southern range edge of Fagus sylvatica. Glob Chang Biol. 2006, 12:2163-2174. doi: https://doi.org/10.1111/j.1365-2486.2006.01250.x.
  32. Karki R, Hasson S, Gerlitz L, Talchabhadel R, Schickhoff U, Scholten T, Bohner J. Rising mean and extreme near-surface air temperature across Nepal. Int J Climatol. 2019:1-19. https://doi.org/10.1002/joc.6344.
  33. Kloeppel BD, Abrams MD, Kubiske ML. Seasonal ecophysiology and leaf morphology of four successional Pennsylvania barrens species in open versus understory environments. Can J For Res. 1993;23:181-9. https://doi.org/10.1139/x93-025
  34. Korner C. Biosphere response to CO2 enrichment. Ecol Appl. 2000;10:1590-619. https://doi.org/10.1890/1051-0761(2000)010[1590:BRTCE]2.0.CO;2
  35. Korner C. Alpine plant life: functional plant ecology of high mountainecosystems. Berlin: Springer; 2003.
  36. LeBlanc DC, Nicholas NS, Zedaker SM. Prevalence of individual-tree growth decline in red spruce populations of the southern Appalachian Mountains. Can J For Res. 1992;22:905-14. https://doi.org/10.1139/x92-120
  37. Liang E, Dawadi B, Pederson N, Eckstein D. Is the growth of birch at the upper timberline in the Himalayas limited by moisture or by temperature? Ecology. 2014;95:140307191613003. https://doi.org/10.1890/13-1904.1.
  38. Lv LX, Zhang QB. Asynchronous recruitment history of Abies spectabilis along an altitudinal gradient in the Mt. Everest region. Journal of Plant Ecology 2012,5:147-156. https://doi.org/10.1093/jpe/rtr016.
  39. Nepal S, Pradhananga S, Shrestha NK, Kralisch S, Shrestha J, Fink M. Spacetime variability of soil moisture droughts in the Himalayan region. Hydrol Earth Syst Sci Discuss. 2020. https://doi.org/10.5194/hess-2020-337, in review.
  40. Panthi S, Brauning A, Zhou ZK, Fan ZX. Tree rings reveal recent intensified spring drought in the Central Himalaya, Nepal. Glob Planet Chang. 2017;157:26-34. https://doi.org/10.1016/j.gloplacha.2017.08.012
  41. Penuelas J, Canadell JG, Ogaya R. Increased water-use efficiency during the 20th century did not translate into enhanced tree growth. Glob Ecol Biogeogr. 2011;20:597-608. https://doi.org/10.1111/j.1466-8238.2010.00608.x.
  42. Pichler P, Oberhuber W. Radial growth response of coniferous forest trees in an inner Alpine environment to heat-wave in 2003. For Ecol Manag. 2007;242:688-99. https://doi.org/10.1016/j.foreco.2007.02.007
  43. Pokharel B, Wang S-Y S, Meyer J, Marahatta S, Nepal B, Chikamoto Y, Gillies R. The east-west division of changing precipitation in Nepal. Int J Clim. 2019. https://doi.org/10.1002/joc.6401.
  44. Pompa-Garcia M, Hadad MA. Sensitivity of pines in Mexico to temperature varies with age. Atmosfera. 2016;29:209-19. https://doi.org/10.20937/ATM.2016.29.03.03
  45. Qi Z, Liu H, Wu X, Hao Q. Climate-driven speedup of alpine treeline forest growth in the Tianshan Mountains, Northwestern China. Glob Chang Biol. 2015;21:816-26. https://doi.org/10.1111/gcb.12703.
  46. Rakthai S, Fu P-L, Fan ZX, Gaire NP, Pumijumnong N, Eiadthong W, Tangmitcharoen S. Increased drought sensitivity results in a declining tree growth of Pinus latteri in Northeastern Thailand. Forests. 2020;11:361. https://doi.org/10.3390/f11030361
  47. Rinn F. TSAP-Win: Time Series Analysis and Presentation for Dendrochronology and Related Applications. Version 0.55 User reference. Heidelberg, Germany. 2003. http://www.rimatech.com.
  48. Rubino DL, McMarthy BC. Dendroclimatological analysis of white oak (Quercus alba L., Fagaceae) from an old-growth forest of southeastern Ohio, USA. J Torrey Bot Soc. 2000;127:240-50. https://doi.org/10.2307/3088761
  49. Ruiz-Benito P, Madrigal-Gonzalez J, Young S, Mercatoris P, Cavin L, Huang T-J. Climatic stress during stand development alters the sign and magnitude of age-related growth responses in a subtropical mountain pine. 2015;10(5):e0126581. https://doi.org/10.1371/journal.pone.0126581.
  50. Salzer MW, Hughes MK, Bunnb AG, Kipfmueller KF. Recent unprecedented treering growth in bristlecone pine at the highest elevations and possible causes. PNAS. 2009;106:20348-53. https://doi.org/10.1073/pnas.0903029106
  51. Sano M, Furuta F, Kobayashi O, Sweda T. Temperature variations since the mid-18th century for western Nepal, as reconstructed from tree-ring width and density of Abies spectabilis. Dendrochronologia. 2005;23:83-92. https://doi.org/10.1016/j.dendro.2005.08.003
  52. Shrestha AB, Aryal R. Climate change in Nepal and its impact on Himalayan glaciers. Environ Change. 2011;11(1):65-77. https://doi.org/10.1007/s10113-010-0174-9
  53. Shrestha AB, Bajracharya SR, Sharma AR, Duo C, Kulkarni A. Observed trends and changes in daily temperature and precipitation extremes over the Koshi river basin 1975-2010. Int J Clim. 2017;37:1066-83. https://doi.org/10.1002/joc.4761
  54. Shrestha AB, Wake CP, Dibb JE, Mayewski PA. Precipitation fluctuations in the Nepal Himalaya and its vicinity and relationship with some large scale climatological parameters. Int J Clim. 2000;20:317-27. https://doi.org/10.1002/(SICI)1097-0088(20000315)20:3<317::AID-JOC476>3.0.CO;2-G
  55. Shrestha AB, Wake CP, Mayewsk PA, Dibb JE. Maximum temperature trends in the Himalaya and its vicinity: an analysis based on temperature records from Nepal for the period 1971-94. J Clim. 1999;12(9):12.
  56. Shrestha KB, Hofgaard A, Vandvik V. Recent treeline dynamics are similar between dry and mesic areas of Nepal, central Himalaya. Journal of Plant Ecology 2014,8: 347-358. https://doi.org/10.1093/jpe/rtu035
  57. Sigdel SR, Dawadi B, Camarero JJ, Liang E, Leavitt SW. Moisture-limited tree growth for a subtropical Himalayan conifer forest in Western Nepal. Forests. 2018;9(6):340. https://doi.org/10.3390/f9060340.
  58. Speer JH. Fundamentals of tree-ring research. Tucson: The University of Arizona Press; 2010.
  59. Speer JH, et al. Pinus roxburghii stand dynamics at a heavily impacted site in Nepal: research through an educational fieldweek. Dendrochronologia. 2017;2017(1):2-9. https://doi.org/10.1016/j.dendro.2016.01.005.
  60. Thapa UK, Shah SK, Gaire NP, Bhuju DR. Spring temperatures in the far-western Nepal Himalaya since AD 1640 reconstructed from Picea smithiana treering widths. Clim Dyn. 2014. https://doi.org/10.1007/s00382-0142457-1.
  61. Tiwari A, Fan ZX, Jump AS, Zhou ZK. Warming induced growth decline of Himalayan birch at its lower range edge in a semi-arid region of Trans-Himalaya, Central Nepal. Plant Ecol. 2017;218(5):621-33. https://doi.org/10.1007/s11258-017-0716-z.
  62. Tiwari A, Jha PK. An overview of treeline response to environmental changes in Nepal Himalaya. Tropical Ecology 2018,59(2): 273-285.
  63. Vose JM, Swank WT. Effects of long-term drought on the hydrology and growth of a white pine plantation in the southern Appalachians, For. Ecol. Manag. 1994,64:(1)25-39. https://doi.org/10.1016/0378-1127(94)90124-4.
  64. Weiner J, Thomas SC. The nature of tree growth and the age-related decline in forest productivity. Oikos. 2001;94:374-6. https://doi.org/10.1034/j.1600-0706.2001.940219.x
  65. Yu D, Liu J, Lewis BJ, Li Z, Wangming Z, Xiangmin F, Yawei W, Shengwei J, Limin D. Spatial variation and temporal instability in the climate-growth relationship of Korean pine in the Changbai Mountain region of Northeast China. For Ecol Manag. 2013;300:96-105. https://doi.org/10.1016/j.foreco.2012.06.032
  66. Zang C, Biondi F. Dendroclimatic calibration in R: the bootRes package for response and correlation function analysis. Dendrochronologia. 2013;31:68-74. https://doi.org/10.1016/j.dendro.2012.08.001