April–September minimum temperature reconstruction based on Sabina tibetica ring-width chronology in the central eastern Tibetan Plateau, China

doi:10.1007/s11676-023-01682-7

摘要/Abstract

Abstract:

Minimum temperatures have remarkable impacts on tree growth at high-elevation sites on the Tibetan Plateau, but the shortage of long-term and high-resolution paleoclimate records inhibits understanding of recent minimum temperature anomalies. In this study, a warm season (April–September) reconstruction is presented for the past 467 years (1550–2016) based on Sabina tibetica ring-width chronology on the Lianbaoyeze Mountain of the central eastern Tibetan Plateau. Eight warm periods and eight cold periods were identified. Long-term minimum temperature variations revealed a high degree of coherence with nearby reconstructions. Spatial correlations between our reconstruction and global sea surface temperatures suggest that warm season minimum temperature anomalies in the central eastern Tibetan Plateau were strongly influenced by large-scale ocean atmospheric circulations, such as the El Niño-Southern Oscillation and the Atlantic Multidecadal Oscillation.

Key words: Tree-ring analysis, Sabina tibetica, Minimum temperatures, Central eastern Tibetan Plateau, Climate change

Teng Li, Jianfeng Peng, Tsun Fung Au, Jinbao Li. [J]. 林业研究(英文版), 2024, 35(1): 37-.

Teng Li, Jianfeng Peng, Tsun Fung Au, Jinbao Li. April–September minimum temperature reconstruction based on Sabina tibetica ring-width chronology in the central eastern Tibetan Plateau, China[J]. JOURNAL OF FORESTRY RESEARCH, 2024, 35(1): 37-.

参考文献 71

1	Asad F, Zhu HF, Zhang H, Liang EY, Muhammad S, Farhan SB, Hussain I, Wazir MA, Ahmed M, Esper J. Are Karakoram temperatures out of phase compared to hemispheric trends?. Clim Dyn, 2016, 48(9–10): 3381-3390
2	Bao G, Liu Y, Liu N. A tree-ring-based reconstruction of the Yimin river annual runoff in the Hulun Buir region, Inner Mongolia, for the past 135 years. Chin Sci Bull, 2012, 57(36): 4765-4775, DOI
3	Chen F, Yu SL, Yuan YJ, Wang HQ, Gagen M. A tree-ring width based drought reconstruction for southeastern China, links to Pacific Ocean climate variability. Boreas, 2016, 45(2): 335-346, DOI
4	Chen F, Shang HM, Panyushkina I, Meko D, Li JB, Yuan YJ, Yu SL, Chen FH, He DM, Luo X. 500-year tree-ring reconstruction of Salween river streamflow related to the history of water supply in Southeast Asia. Clim Dyn, 2019, 53: 6595-6607, DOI
5	Classen AT, Sundqvist MK, Henning JA, Newman GS, Moore JAM, Cregger MA, Moorhead LC, Patterson CM. Direct and indirect effects of climate change on soil microbial and soil microbial-plant interactions: what lies ahead?. Ecosphere, 2015, 6: 1-21, DOI
6	Cook ER, Holmes RL. User’s manual for ARSTAN, 1986 Tucson Laboratory of Tree-ring Research, University of Arizona
7	Cook ER, Kairiukstis LA. Methods of dendrochronology, 1990 Dordrecht Kluwer Academic Publishers, DOI
8	Cook ER, Peters K. Calculating unbiased tree-ring indices for the study of climatic and environmental change. The Holocene, 1997, 7(3): 361-370, DOI
9	Cook ER, Anchukaitis KJ, Buckley BM, D'Arrigo RD, Jacoby GC, Wright WE. Asian monsoon failure and Megadrought during the last millennium. Science, 2010, 328(5977): 486-489, DOI
10	Davi NK, D’Arrigo R, Jacoby GC, Cook ER, Anchukaitis KJ, Nachin B, Rao MP, Leland C. A long-term context (931–2005 C.E.) for rapid warming over Central Asia. Quat Sci Rev, 2015, 121: 89-97, DOI
11	Deng Y, Gou XH, Gao LL, Zhang F, Xu X, Yang MX. Tree-ring recorded drought variability in the northern Min Mountains of northwestern China. Int J Clim, 2016, 36(10): 3550-3560, DOI
12	Deng Y, Gou XH, Gao LL, Yang MX, Zhang F. Spatiotemporal drought variability of the eastern Tibetan Plateau during the last millennium. Clim Dyn, 2017, 49(5–6): 2077-2091, DOI
13	Deslauriers A, Morin H, Begin Y. Cellular phenology of annual ring formation of Abies balsamea in the Quebec boreal forest (Canada). Can J for Res, 2003, 33: 190-200, DOI
14	Duan JP, Wang LL, Li L, Chen K. Temperature variability since AD 1837 inferred from tree-ring maximum density of Abies fabri on Gongga Mountain, China. Chin Sci Bull, 2010, 55: 3015-3022, DOI
15	Esper J, Cook ER, Schweingruber FH. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science, 2002, 295(5563): 2250-2253, DOI
16	Fan ZX, Brauning A, Fu PL, Yang RQ, Qi JH, Griebinger J, Gebrekirstos A. Intra-annual radial growth of Pinus kesiya var. langbianensis is mainly controlled by moisture availability in the Ailao Mountains Southwestern China. Forests, 2019, 10: 899, DOI
17	Fang KY, Chen DL, Li JB, Seppä H. Covarying hydroclimate patterns between monsoonal Asia and North America over the past 600 years. J Clim, 2014, 27: 8017-8033, DOI
18	Fang KY, Guo ZT, Chen DL, Linderholm HW, Li JB, Zhou FF, Guo GY, Dong ZP, Li YJ. Drought variation of western Chinese Loess Plateau since 1568 and its linkages with droughts in western North America. Clim Dyn, 2017, 49: 3839-3850, DOI
19	Fritts HC. Tree rings and climate, 1976 New York Academic Press
20	Gou XH, Chen FH, Jacoby G, Cook E, Yang MX, Peng JF, Zhang Y. Rapid tree growth with respect to the last 400 years in response to climate warming, northeastern Tibetan Plateau. Int J Climatol, 2007, 27: 1497-1503, DOI
21	Gou XH, Yang T, Gao LL, Deng Y, Yang MX, Chen FH. A 457-year reconstruction of precipitation in the southeastern Qinghai-Tibet Plateau, China using tree-ring records. Chin Sci Bull, 2013, 58(10): 1107-1114, in Chinese DOI
22	Harris I, Osborn TJ, Jones P, Lister D. Version 4 of the CRU TS monthly high-resolution gridded multivariate climate dataset. Sci Data, 2020, 7: 109, DOI
23	He MH, Yang B, Datsenko NM. A six hundred-year annual minimum temperature history for the central Tibetan Plateau derived from tree-ring width series. Clim Dyn, 2014, 43: 641-655, DOI
24	Holmes RL. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Res, 1983, 43: 69-78
25	Hu JH, Zeng H. A preliminary analysis of stereoscopic exploitation and utilization of climate resources in central eastern Tibetan Plateau. Chin J Agrometeorol, 2003, 24(1): 54-57 in Chinese
26	Huang R, Zhu HF, Liang EY, Liu B, Shi JF, Zhang RB, Yuan YJ, Griessinger J. A tree ring-based winter temperature reconstruction for the southeastern Tibetan Plateau since 1340 CE. Clim Dyn, 2019, 53(5–6): 3221-3233, DOI
27	IPCC (2021) In: Climate change 2021: the physical science basis. Contribution of working group I to the sixth assessment report of the intergovernmental panel on climate CM-D, V. Zhai P, Pirani A, Connors SL, Péan C, Berger S, Caud N, Chen Y, Goldfarb L, Gomis MI et al. (eds) Cambridge University Press, Cambridge, UK; New York, USA
28	Jiao L, Wang SJ, Chen K, Liu XP. Dynamic response to climate change in the radial growth of Picea schrenkiana in western Tien Shan, China. J for Res, 2022, 33: 147-157, DOI
29	Körner C. Alpine plant life: functional plant ecology of high mountain ecosystems, 1999 Berlin Springer, DOI
30	Li T, Li JB. A 564-year annual minimum temperature reconstruction for the east central Tibetan Plateau from tree rings. Glob Planet Change, 2017, 157: 165-173, DOI
31	Li JB, Xie SP, Cook ER. El Niño phases embedded in Asian and North American drought reconstructions. Quat Sci Rev, 2014, 85: 20-34, DOI
32	Li JJ, Shao XM, Li YY, Qin NS. Annual temperature recorded in tree-ring from Songpan region. Chin Sci Bull, 2014, 59: 1446-1458
33	Li ZS, Liu GH, Wu X, Gong L, Wang M, Wang XC (2015a) Tree ring-based temperature reconstruction over the past 186 years for the Miyaluo Natural Reserve, western Sichuan Province of China. Theor Appl Climatol 120(3–4):495–506
34	Li ZS, Liu GH, Wu X, Wang XC. Tree-ring-based temperature reconstruction for the Wolong Natural Reserve, central eastern Tibetan Plateau of China. Int J Climatol, 2015, 35(11): 3296-3307, DOI
35	Li JB, Shi JF, Zhang DD, Yang B, Fang KY, Yue PH. Moisture increase in response to high-altitude warming evidenced by tree-rings on the southeastern Tibetan Plateau. Clim Dyn, 2017, 48(1–2): 649-660, DOI
36	Li JX, Li JB, Li T, Au TF. 351-year tree ring reconstruction of the Gongga Mountains winter minimum temperature and its relationship with the Atlantic multidecadal oscillation. Clim Change, 2021, 165: 49, DOI
37	Liang EY, Shao X, Xu Y. Tree-ring evidence of recent abnormal warming on the southeast Tibetan plateau. Theor Appl Climatol, 2009, 98(1–2): 9-18, DOI
38	Liang HX, Lyu LX, Wahab M. A 382-year reconstruction of August mean minimum temperature from tree-ring maximum latewood density on the southeastern Tibetan Plateau, China. Dendrochronologia, 2016, 37: 1-8, DOI
39	Liu Y, An ZS, Linderholm HW, Chen DL, Song HM, Cai QF, Sun JY, Tian H. Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings. Sci China Ser D, 2009, 52(3): 348-359, DOI
40	Liu Y, Cobb KM, Song HM, Li Q, Li CY, Nakatsuka T, An ZS, Zhou WJ, Cai QF, Li JB, Leavitt SW, Sun CF, Mei RC, Shen CC, Chan MH, Sun JY, Yan LB, Lei Y, Ma YY, Li XX, Chen DL, Linderholm HW. Recent enhancement of central Pacific El Nino variability relative to last eight centuries. Nat Commun, 2017, 8: 15386, DOI
41	Liu Y, Liu H, Song HM, Li Q, Burr GS, Wang L, Hu SL. A monsoon-related 174-year relative humidity record from tree-ring δ¹⁸O in the Yaoshan region, eastern central China. Sci Total Environ, 2017, 593–594: 523-534, DOI
42	Mann ME, Lees JM. Robust estimation of background noise and signal detection in climatic time series. Clim Change, 1996, 33: 409-445, DOI
43	Mann ME, Zhang ZH, Hughes MK, Bradley RS, Miller SK, Rutherford S, Ni FB. Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia. P Natl Acad Sci USA, 2008, 105(36): 13252-13257, DOI
44	Michaelsen J. Cross-validation in statistical climate forecast models. J Clim Appl Meteor, 1987, 26: 1589-1600, DOI
45	Peng JF, Liu YZ. Reconstructed droughts for the northeastern Tibetan Plateau since AD 1411 year and its linkages to the Pacific, Indian and Atlantic Oceans. Quat Int, 2013, 283: 98-116, DOI
46	Rayner NA, Parker DE, Horton EB, Folland CK, Alexander LV, Rowell DP, Kent EC, Kaplan A. Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J Geophys Res, 2003, 108: D144407, DOI
47	Shao XM, Fan JM. Past climate on west Sichuan Plateau as reconstructed from ring-widths of dragon spruce. Quat Sci, 1999, 19: 81-89 in Chinese
48	Shao XM, Huang L, Liu HB, Liang EY, Fang XQ, Wang LL. Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai. Sci Chin Ser D, 2005, 48(7): 939-949, DOI
49	Shao X, Xu Y, Yin ZY, Liang E, Zhu H, Wang S. Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau. Quat Sci Rev, 2010, 29: 2111-2122, DOI
50	Shi JF, Li JB, Zhang DD, Zheng JY, Shi SY, Ge QS, Lee HF, Zhao YS, Zhang J, Lu HY. Two centuries of April–July temperature change in eastern China and its influence on grain productivity. Sci Bull, 2017, 62: 40-45, DOI
80	Shi CM, Masson-Delmotte V, Daux V, Li ZS, Carré M, Moore JC (2015) Unprecedented recent warming rate and temperature variability over the east Tibetan Plateau inferred from Alpine treeline dendrochronology. Clim Dyn 45(5–6):1367–1380
51	Song HM, Liu Y, Ni W, Cai QF, Sun JY, Ge W, Xiao W. Winter mean lowest temperature derived from tree-ring width in Jiuzhaigou region, China since 1750 AD. Quat Sci, 2007, 27(4): 486-491
52	Stokes MA, Smiley TL. Introduction to tree-ring dating, 1968 Chicago University of Chicago Press
53	Sun CF, Liu Y, Song HM, Cai QF, Li Q, Wang L, Mei RC, Fang CX. Sunshine duration reconstruction in the southeastern Tibetan plateau based on tree-ring width and its relationship to volcanic eruptions. Sci Total Environ, 2018, 628–629: 707-714, DOI
54	Torrence C, Compo GP. A practical guide to wavelet analysis. B Am Meteorol Soc, 1998, 79: 61-78, DOI
55	Wang HL, Shao XM, Li MQ. A 2917-year tree-ring-based reconstruction of precipitation for the Buerhanbuda Mts., Southeastern Qaidam Basin, China. Dendrochronologia, 2019, 55: 80-92, DOI
56	Wigley T, Briffa KR, Jones PD. On the average value of correlated time-series, with applications in dendroclimatoloy and hydrometeorology. J Clim Appl Meteorol, 1984, 23: 201-213, DOI
57	Wilson R, Anchukaiti K, Briffa KR, Büntgen U, Cook E, D’Arrigo R, Davi N, Esper J, Frank D, Gunnarson B, Hegerl G, Helama S, Klesse S, Krusic PJ, Linderholm HW, Myglan V, Osborn TJ, Rydval M, Schneider L, Schurer A, Zorita E. Last millennium northern hemisphere summer temperatures from tree rings, part I, the long term context. Quat Sci Rev, 2016, 134: 1-18, DOI
58	Wu P, Wang LL, Shao XM. Reconstruction of summer temperature from maximum latewood density of Pinus densata in west Sichuan. Acta Geogr Sin, 2005, 60(6): 998-1006 in Chinese
59	Xiao DM, Qin NS, Huang X. A 325-year reconstruction of July–August mean temperature in the north of west Sichuan derived from tree-ring. Quat Sci, 2015, 35: 1134-1144 in Chinese
60	Yang B, Qin C, Wang JL, He MH, Melvin TM, Osborn TJ, Briffa KR. A 3500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. Proc Natl Acad Sci USA, 2014, 111: 2903-2908, DOI
61	Yang B, Sonechkin D, Datsenko N, Liu JJ, Qin C. Establishment of a 4650-year-long eigenvalue chronology based on tree-ring cores from Qilian junipers (Juniperus przewalskii Kom) in Western China. Dendrochronologia, 2017, 46: 56-66, DOI
62	Yin H, Liu HB, Linderholm HW, Sun Y. Tree ring density-based warm-season temperature reconstruction since A.D. 1610 in the eastern Tibetan Plateau. Palaeogeogr Palaeoclimatol Palaeoecol, 2015, 426: 112-120, DOI
63	Yu J, Liu Q. Larix olgensis growth-climate response between lower and upper elevation limits: an intensive study along the eastern slope of the Changbai Mountains, northeastern China. J for Res, 2020, 31: 231-244, DOI
64	Yu SL, Yuan YJ, Wei WS, Zhang TW, Shang HM, Chen F. Reconstructed mean temperature in Mearkang, West Sichuan in July and its detection of climatic period signal. Plateau Meteorol, 2012, 31: 193-200 in Chinese
65	Zhang ZH (2015) Tree-rings, a key ecological indicator of environment and climate change. Ecol Indic 51:107–116
66	Zhang TW, Yuan YJ, Wei WS, Yu SL, Zhang RB, Chen F, Shang HM, Qin L. A tree-ring based precipitation reconstruction for the Mohe region in the northernGreater Higgnan Mountains, China, since AD 1724. Quat Res, 2014, 82(1): 14-21, DOI
67	Zhang Y, Shao XM, Yin ZY, Wang Y. Millennial minimum temperature variations in the Qilian Mountains, China: evidence from tree rings. Clim past, 2014, 10: 1763-1778, DOI
68	Zhang QB, Evans MN, Lyu LX (2015) Moisture dipole over the Tibetan Plateau during the past five and a half centuries. Nat Commun 6:8062
69	Zhang RB, Wei WS, Shang HM, Yu SL, Gou XH, Qin L, Bolatov K, Mambetov BT. A tree ring-based record of annual mass balance changes for the TS. Tuyuksuyskiy Glacier and its linkages to climate change in the Tianshan Mountains. Quat Sci Rev, 2019, 205: 10-21, DOI
70	Zhang XL, Li JX, Liu XB, Chen ZJ. Improved EEMD-based standardization method for developing long tree-ring chronologies. J for Res, 2020, 31: 2217-2224, DOI
71	Zhu LJ, Zhang YD, Li ZS, Guo BD, Wang XC. A 368-year maximum temperature reconstruction based on tree-ring data in the northcentral eastern Tibetan Plateau Plateau (NWSP), China. Clim past, 2016, 12: 1485-1498, DOI