Dendroclimatological study of Sabina saltuaria and Abies faxoniana in the mixed forests of the Qionglai Mountains, eastern Tibetan Plateau
Tree-ring chronologies were developed for Sabina saltuaria and Abies faxoniana in mixed forests in the Qionglai Mountains of the eastern Tibetan Plateau. Climate-growth relationship analysis indicated that the two co-existing species reponded similarly to climate factors, although S. saltuaria was more sensitive than A. faxoniana. The strongest correlation was between S. saltuaria chronology and regional mean temperatures from June to November. Based on this relationship, a regional mean temperature from June to November for the period 1605–2016 was constructed. Reconstruction explained 37.3% of the temperature variance during th period 1961–2016. Six major warm periods and five major cold periods were identified. Spectral analysis detected significant interannual and multi-decadal cycles. Reconstruction also revealed the influence of the Atlantic Multi-decadal Oscillation, confirming its importance on climate change on the eastern Tibetan Plateau.
Tree-ring analysis / Mixed forests / Dendroclimatology / Qionglai Mountains
[1] | Biondi F, Waikul K (2004) Dendroclim 2002: A C ++ program for statistical calibration of climate signals in tree-ring chronologies. Comput Geosci 30:303–311 |
[2] | Br?uning A, Mantwill B (2004) Summer temperature and summer monsoon history on the Tibetan Plateau during the last 400 years recorded by tree rings. Geophys Res Lett 31:L24205 |
[3] | Cai QF, Liu Y (2017) Two centuries temperature variations over subtropical southeast China inferred from Pinus taiwanensis Hayata tree-ring width. Clim Dynam 48:1813–1825 |
[4] | Cook ER, Holmes RL (1986) Users manual for ARETAN: laboratory of tree-ring research. University of Arizona, Tucson, pp 50–60 |
[5] | Cook ER, Kairiukstis LA (1990) Methods of dendrochronology, applications in the environmental sciences. Kluwer, Dordrecht |
[6] | Cook ER, Meko DM, Stahle DW, Cleaveland MK (1999) Drought reconstructions for the continental United States. J Clim 12:1145–1162 |
[7] | Cook ER, Krusic PJ, Jones PD (2003) Dendroclimatic signals in long tree-ring chronologies from the Himalayas of Nepal. Int J Climatol 23(7):707–732 |
[8] | Deng Y, Gou XH, Gao LL, Yang T, Yang MX (2014) Early summer temperature variations over the past 563 yr inferred from tree rings in the Shaluli Mountains, southeastern Tibet Plateau. Quat Res 81(3):513–519 |
[9] | Ding YH, Liu YJ, Liang SJ, Ma XQ, Zhang YX, Si D, Liang P, Song YF, Zhang J (2014) Interdecadal variability of the East Asian winter monsoon and its possible links to global climate change. J Meteor Res 28:693–713 |
[10] | Dong BW, Sutton RT, Scaife AA (2006) Multidecadal modulation of El Nino-Southern Oscillation (ENSO) variance by Atlantic Ocean sea surface temperatures. Geophys Res Lett 33:L08705 |
[11] | Duan JP, Zhang QB (2014) A 449 year warm season temperature reconstruction in the southeastern Tibetan Plateau and its relation to solar activity. J Geophys Res: Atmos 119:11578–11592 |
[12] | Duan JP, Wang LL, Li L, Chen KL (2010) Temperature variability since AD 1837 inferred from tree-ring maximum density of Abies fabric in Gongga Mountains China. Chin Sci Bull 55(11):1036–1042 |
[13] | Durbin J, Watson GS (1950) Testing for serial correlation in least squares regression. I Biometrika 37:409–428 |
[14] | Fan ZX, Brauning A, Tian QH, Yang B, Cao KF (2010) Tree ring recorded May–August temperature variations since A.D. 1585 in the Gaoligong Mountains. Southeastern 296:94–102 |
[15] | Fritts HC (1976) Tree rings and climate. Academic Press, New York |
[16] | Gou XH, Chen FH, Jacoby G, Cook E, Yang MX, Peng JF, Zhang Y (2007) Rapid tree growth with respect to the last 400 years in response to climate warming, northeastern Tibetan Plateau. Int J Climatol 27:1497–1503 |
[17] | Gou XH, Deng Y, Chen FH, Yang MX, Fang KY, Gao LL, Yang T, Zhang F (2010) Tree ring based streamflow reconstruction for the Upper Yellow River over the past 1234 years. Chin Sci Bull 55(36):4179–4186 |
[18] | Harris I, JonesD OTJ, Lister DH (2014) Updated high-resolution grids of monthly climatic observations—the CRU TS3. 10 Dataset. Int J Climatol 34:623–642 |
[19] | He MH, Yang B, Datsenko NM (2014) A six hundred-year annual minimum temperature history for the central Tibetan Plateau derived from tree-ring width series. Clim Dynam 43:641–655 |
[20] | Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull 43:69–75 |
[21] | Huang BY, Banzon V, Freeman E, Lawrimore J, Liu W, Peterson TC, Smith TM, Thorne PW, Woodruff SD, Zhang HM (2015) Extended reconstructed sea surface temperature version 4 (ERSST.v4). Part I: upgrades and Intercomparisons. J Climate 28:911–930 |
[22] | IPCC (2013) Climate change 2013: the physical science basis. Contribution of working group I to the fifth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge and New York, NY |
[23] | Li SL, Bates GT (2007) Influence of the Atlantic multidecadal oscillation on the winter climate of East China. Adv Atmos Sci 24:126–135 |
[24] | Li T, Li JB (2017) A 564-year annual minimum temperature reconstruction for the east central Tibetan Plateau from tree rings. Global Planet Change 157:165–173 |
[25] | Li ZX, He YQ, Jia WX, Pang HX, Yuan LL, Ning BY, Liu Q, He XZ, Song B, Zhang NN (2008) Response of “Glaciers-Runoff” system in a typical temperature-glacier, Hailuogou Glacier in Gongga Mountain of China to global change. Scientia Geographica Sinica 28(2):229–234 (in Chinese) |
[26] | Li ZX, He YQ, Jia WX, Pang HX, He XZ, Wang SJ, Zhang NN, Zhang WJ, Liu Q, Xin HJ (2009) Changes in Hailuogou glacier during the recent 100 years under global warming. J Glaciol Geocryol 31(1):75–81 (in Chinese) |
[27] | Li ZS, Liu GH, Zhang QB, Hu CJ, Luo SZ, Liu XL, He F (2010) Tree ring reconstruction of summer temperature variations over the past 159 years in Wolong National Natural Reserve, western Sichuan. China Chin J Plant Ecol 34(6):628–641 (in Chinese) |
[28] | Li JJ, Shao XM, Li YY, Qin NS (2014) Annual temperature recorded in tree-ring from Songpan region. Chin Sci Bull 59(15):1446–1458 |
[29] | Li X, Liang E, Gri?ar J, Rossi S, ?ufar K, Ellison AM (2017) Critical minimum temperature limits xylogenesis and maintains treelines on the southeastern Tibetan Plateau. Sci Bull 62(11):804–812 |
[30] | Li MY, Duan JP, Wang LL, Zhu HF (2018) Late summer temperature reconstruction based on tree-ring density for Sygera Mountain, southeastern Tibetan Plateau. Global Planet Change 163:10–17 |
[31] | Li JX, Li JB, Li T, Au TF (2020) Tree growth divergence from winter temperature in the Gongga Mountains, southeastern Tibetan Plateau. Asian Geogr 37(1):1–15 |
[32] | Li JX, Li JB, Li T, Au TF (2021) 351-year tree ring reconstruction of the Gongga Mountains winter minimum temperature and its relationship with the Atlantic Multidecadal Oscillation. Clim Chang 165:1–19 |
[33] | Liang HX, Lyu LX, Wahab M (2016) A 382-year reconstruction of August mean minimum temperature from tree-ring maximum latewood density on the southeastern Tibetan Plateau, China. Dendrochronologia 37:1–8 |
[34] | Lin PJ, Li CY, Lu CT, Wang G, Yang L, Liu QC (2019) Analysis of red color-leafed forest landscape stability in Bipeng Valley Scenic Spots. J Sichuan Forest Sci Technol 40(4):7–11 (in Chinese) |
[35] | Liu XD, Chen BD (2000) Climatic warming in the Tibetan Plateau during recent decades. Int J Climatol 20:1729–1742 |
[36] | Liu XD, Zhang MF (1998) Contemporary climatic change over the Qinghai- Xizang Plateau and its response to the Green-House effect. Chin Geogr Sci 8(4):289–298 |
[37] | Liu SY, Ding YJ, Li J, Shangguan DH, Zhang Y (2006a) Glaciers in response to recent climate warming in Western China. Quaternary Sci 26(5):762–771 (in Chinese) |
[38] | Liu Y, An ZS, Ma HZ, Cai QF, Liu ZY, Kutzbach JK, Shi JF, Song HM, Sun JY, Yi L, Li Q, Yang YK, Wang L (2006) Precipitation variations recorded by tree rings in Dulan area of Qinghai Province since 850 A.D. and their relationship with temperature in the Northern Hemisphere. Sci China Series D Earth Sci 36(5):461–471 |
[39] | Liu Y, An ZS, Linderholm HW, Chen DL, Song HM, Cai QF, Sun JY, Tian H (2009) Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings. Sci China Series D Earth Sci 52(3):348–359 |
[40] | Liu Y, Xiang N, Song HM (2012) Tree-ring temperature records in Arxan, Inner Mongolia for the past 187 years. J Earth Environ 3(3):862–867 (in Chinese) |
[41] | Lu RY, Dong BW, Ding H (2006) Impact of the Atlantic multidecadal oscillation on the Asian summer monsoon. Geophys Res Lett 33:L24701 |
[42] | Mann ME, Lees JM (1996) Robust estimation of background noise and signal detection in climatic time series. Clim Chang 33:409–445 |
[43] | Peng JF, Liu YZ, Wang T (2014) A tree-ring record of 1920’s—1940’s droughts and mechanism analyses in Henan Province. Acta Ecol Sin 34(13):3509–3518 (in Chinese) |
[44] | Qin NS, Shi XH, Shao XM, Wang QC (2008) Average maximum temperature change recorded by tree rings in West Sichuan Plateau. Plateau and Mountain Meteorology Research 28(4):18–24 (in Chinese) |
[45] | Schweingruber FH (1996) Tree rings and environment dendroecology. Paul Haupt Verlag, Bern |
[46] | Shao XM (1997) Advancements in dendrochronology. Quaternary Sci 17(3):265–271 (in Chinese) |
[47] | Shao XM, Fan JM (1999) Past climate on west Sichuan Plateau as reconstructed from ring-widths of dragon spruce. Quater Sci 1:81–89 (in Chinese) |
[48] | Shao XM, Huang L, Liu HB, Liang EY, Fang XQ, Wang LL (2005) Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai. Sci China Ser D Earth Sci 48(7):939–949 |
[49] | Sheppard PR, Tarasov PE, Graumlich LJ, Heussner KU, Wagner M, Osterle H, Thompson LG (2004) Annual precipitation since 515 BC reconstructed from living and fossil juniper growth of northeastern Qinghai Province, China. Clim Dynam 23:869–881 |
[50] | Song HM, Liu Y, Ni WM, Cai QF, Sun JY, Ge WB, Xiao WY (2007) Winter mean lowest temperature derived from tree ring width in Jiuzhaigou region, China since 1750 AD. Quaternary Sci 27(4):486–491 |
[51] | Torrence C, Compo GP (1998) A practical guide to wavelet analysis. Bull Am Meteorol Soc 79:61–78 |
[52] | Wang YM, Li SL, Luo DH (2009) Seasonal response of Asian monsoonal climate to the Atlantic Multidecadal Oscillation. J Geophys Res Atmos 114:D02112 |
[53] | Wang JL, Yang B, Qin C, Kang SY, He MH, Wang ZY (2014) Tree-ring inferred annual mean temperature variations on the southeastern Tibetan Plateau during the last millennium and their relationships with the Atlantic Multidecadal Oscillation. Clim Dynam 43:627–640 |
[54] | Wigley TML, Briffa KR, Jones PD (1984) On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. J Appl Meteorol Climatol 23:201–213 |
[55] | Wu P, Wang LL, Shao XM (2005) Reconstruction of summer temperature from maximum latewood density of Pinus densata in West Sichuan. Acta Geogr Sin 60(6):998–1006 (in Chinese) |
[56] | Wu FZ, Yang WQ, Zhang J, Deng R (2010) Fine root decomposition in two subalpine forests during the freeze-thaw season. Can J Forest Res 40:298–307 |
[57] | Xiao DM, Qin NS, Li JJ, Li YY (2013a) Variations of June air temperature derived from tree-ring records in 1713–2010 in Jinchuan, west Sichuan Plateau, China. Progressus Inquisitiones De Mutatione Climatis 9(4):252–257 (in Chinese) |
[58] | Xiao DM, Qin NS, Li JJ, Li YY (2013b) Change of mean maximum temperature in July during 1506–2008 in Seda of west Sichuan Plateau according to reconstructed tree-ring series. J Desert Res 33(5):1536–1543 (in Chinese) |
[59] | Xiao DM, Qin NS, Huang XM (2015a) A 325-year reconstruction of July–August mean temperature in the north of west Sichuan derived from tree-ring. Quaternary Sciences 35(5):1134–1144 (in Chinese) |
[60] | Xiao DM, Qin NS, Li JJ, Li YY, Mu L (2015b) Change of mean temperature from July to September in Northeast of Western Sichuan Plateau based tree-ring. Plateau Meteorology 34(3):762–770 (in Chinese) |
[61] | Yang B (2012) Spatial and temporal patterns of climate variations over the Tibetan Plateau during the period 1300–2010. Quaternary Sci 32(1):81–94 (in Chinese) |
[62] | Yang B, Qin C, Wang JL, He MH, Melvin TM, Osborn TJ, Briffa KR (2014) A 3,500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. Proc Natl Acad Sci USA 111:2903–2908 |
[63] | Yu SL, Yuan YJ, Wei WS, Shang HM, Zhang TW, Chen F, Zhang RB (2012a) Reconstruction of minimum temperature field in June–July during 1787–2005 in the West Sichuan Plateau. J Desert Res 32(4):1010–1016 (in Chinese) |
[64] | Yu SL, Yuan YJ, Wei WS, Zhang TW, Shang HM, Chen F (2012b) Reconstructed mean temperature in Mearkang, West Sichuan in July and its detection of climatic period signal. Plateau Meteorol 31(1):193–200 (in Chinese) |
[65] | Zhu LJ, Zhang YD, Li ZS, Guo BD, Wang XC (2016) A 368-year maximum temperature reconstruction based on tree-ring data in the northwestern Sichuan Plateau (NWSP), China. Clim past 12:1485–1498 |
/
〈 | 〉 |