应用生态学报 ›› 2021, Vol. 32 ›› Issue (10): 3771-3780.doi: 10.13287/j.1001-9332.202110.009
• 综合评述 • 上一篇
聂文政1,2, 李明启1,2*
收稿日期:
2021-04-08
修回日期:
2021-06-30
出版日期:
2021-10-15
发布日期:
2022-04-15
通讯作者:
* E-mail: limq@igsnrr.ac.cn
作者简介:
聂文政, 男, 1998年生, 硕士研究生。主要从事树木年轮气候学研究。E-mail: niewenzheng20@mails.ucas.ac.cn
基金资助:
NIE Wen-zheng1,2, LI Ming-qi1,2*
Received:
2021-04-08
Revised:
2021-06-30
Online:
2021-10-15
Published:
2022-04-15
Contact:
* E-mail: limq@igsnrr.ac.cn
Supported by:
摘要: 强火山喷发是影响全球气候变化的重要因素。过去几十年,不同学者基于青藏高原地区树木年轮重建了多条气候变化序列,并依据这些序列研究了全球强火山喷发对青藏高原地区气候的影响。结果表明: 探讨强火山喷发对青藏高原气候影响的树轮序列主要分布在青藏高原东部。利用序列对比法和时序叠加法分析发现,中低纬度的强火山喷发对青藏高原地区温度和干湿变化影响显著,并在强火山喷发后的1~2年内出现降温或者发生干旱,而高纬度的强火山喷发影响较小。此外,连续的多次强火山喷发能导致该区出现年代际的冷期。影响强火山喷发气候效应的因素主要包括火山喷发位置、喷发强度、大气环流等。最后结合国内外研究现状,对未来需要开展的研究方向进行了展望。
聂文政, 李明启. 树轮数据揭示的强火山喷发对青藏高原地区气候的影响[J]. 应用生态学报, 2021, 32(10): 3771-3780.
NIE Wen-zheng, LI Ming-qi. Influence of large volcanic eruptions on climate as revealed by tree-ring data on the Tibetan Plateau, China[J]. Chinese Journal of Applied Ecology, 2021, 32(10): 3771-3780.
[1] Robock A. Volcanic eruptions and climate. Reviews of Geophysics, 2000, 38: 191-219 [2] Salzer MW, Hughes MK. Bristlecone pine tree rings and volcanic eruptions over the last 5000 yr. Quaternary Research, 2007, 67: 57-68 [3] Santer BD, Bonfils C, Painter JF, et al. Volcanic contribution to decadal changes in tropospheric temperature. Nature Geoscience, 2014, 7: 185-189 [4] Briffa KR, Jones PD, Schweingruer FH, et al. Influence of volcanic eruptions on Northern Hemisphere summer temperature over the past 600 years. Nature, 1998, 393: 450-455 [5] Iles CE, Hegerl GC. The global precipitation response to volcanic eruptions in the CMIP5 models. Environmental Research Letters, 2014, 9: 104012 [6] Chung CE, Ramanathan V. Weakening of North Indian SST gradients and the monsoon rainfall in India and the Sahel. Journal of Climate, 2006, 19: 2036-2045 [7] Duan JP, Li L, Ma Z, et al. Summer cooling driven by large volcanic eruptions over the Tibetan Plateau. Journal of Climate, 2018, 31: 9869-9879 [8] 郝志新, 孙迪, 张学珍, 等. 20世纪以来强火山喷发对中国温度变化区域差异的影响. 地理科学进展, 2016, 35(3): 331-338 [Hao Z-X, Sun D, Zhang X-Z, et al. Regional differences in temperature response in China to the large volcanic eruptions since the 20th century. Progress in Geography, 2016, 35(3): 331-338] [9] 徐群. 皮纳图博火山云对1992年大范围气候的影响. 应用气象学报, 1995, 6(1): 35-42 [Xu Q. Influences of Pinatubo volcanic clouds on large scale climate in 1992. Quarterly Journal of Applied Meteorology, 1995, 6(1): 35-42] [10] Scuderi LA. Tree-ring evidence for climatically effective volcanic eruptions. Quaternary Research, 1990, 34: 67-85 [11] Lough JM, Fritts HC. An assessment of the possible effects of volcanic eruptions on North American climate using tree-ring data, 1602 to 1900 A.D. Climatic Change, 1987, 10: 219-239 [12] LaMarche VC, Hirschboeck KK. Frost rings in trees as records of major volcanic eruptions. Nature, 1984, 307: 121-126 [13] Jones PD, Briffa KR, Schweingruber FH. Tree-ring evidence of the widespread effects of explosive volcanic eruptions. Geophysical Research Letters, 1995, 22: 1333-1336 [14] Szeicz JM. White spruce light rings in northwestern Ca-nada. Arctic and Alpine Research, 1996, 28: 184-189 [15] Piermattei A, Crivellaro A, Krusic PJ, et al. A millennium-long ‘Blue Ring' chronology from the Spanish Pyrenees reveals severe ephemeral summer cooling after volcanic eruptions. Environmental Research Letters, 2020, 15: 124016 [16] D'Arrigo RD, Jacoby GC. Northern North American tree-ring evidence for regional temperature changes after major volcanic events. Climatic Change, 1999, 41: 1-15 [17] D'Arrigo R, Wilson R, Anchukaitis KJ. Volcanic coo-ling signal in tree ring temperature records for the past millennium. Journal of Geophysical Research: Atmospheres, 2013, 118: 9000-9010 [18] 方克艳, 陈秋艳, 刘昶智, 等. 树木年代学的研究进展. 应用生态学报, 2014, 25(7): 1879-1888 [Fang K-Y, Chen Q-Y, Liu C-Z, et al. Research advances in dendrochronology. Chinese Journal of Applied Ecology, 2014, 25(7): 1879-1888] [19] Esper J, Schneider L, Krusic PJ, et al. European summer temperature response to annually dated volcanic eruptions over the past nine centuries. Bulletin of Volca-nology, 2013, 75: 1-14 [20] Anchukaitis KJ, Wilson R, Briffa KR, et al. Last millennium Northern Hemisphere summer temperatures from tree rings. Ⅱ. Spatially resolved reconstructions. Quaternary Science Reviews, 2017, 163: 1-22 [21] Huang R, Zhu H, Liang E, et al. A tree ring-based winter temperature reconstruction for the southeastern Tibetan Plateau since 1340 CE. Climate Dynamics, 2019, 53: 3221-3233 [22] Liu X, Qin D, Shao X, et al. Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millennium. Science in China, Series D: Earth Sciences, 2005, 48: 521-529 [23] 邵雪梅, 范金梅. 树轮宽资料所指示的川西过去气候变化. 第四纪研究, 1999, 19(1): 81-89 [Shao X-M, Fan J-M. Past climate on west Sichuan Plateau as reconstructed from ring-widths of dragon spurce. Quaternary Sciences, 1999, 19(1): 81-89] [24] Cook ER, Krusic PJ, Anchukaitis KJ, et al. Tree-ring reconstructed summer temperature anomalies for tempe-rate East Asia since 800 CE. Climate Dynamics, 2013, 41: 2957-2972 [25] Liang E, Dawadi B, Pederson N, et al. Strong link between large tropical volcanic eruptions and severe droughts prior to monsoon in the central Himalayas revealed by tree-ring records. Science Bulletin, 2019, 64: 1018-1023 [26] Wang Y, Shao X, Zhang Y, et al. The response of annual minimum temperature on the eastern central Tibetan Plateau to large volcanic eruptions over the period 1380-2014 CE. Climate of the Past, 2021, 17: 241-252 [27] Immerzeel WW, Van Beek LP, Bierkens MF. Climate change will affect the Asian water towers. Science, 2010, 328: 1382-1385 [28] 赵东升, 吴绍洪, 尹云鹤. 气候变化情景下中国自然植被净初级生产力分布. 应用生态学报, 2011, 22(4): 897-904 [Zhao D-S, Wu S-H, Yin Y-H. Variation trends of natural vegetation net primary productivity in China under climate change scenario. Chinese Journal of Applied Ecology, 2011, 22(4): 897-904] [29] Li M, Huang L, Yin ZY, et al. Temperature reconstruction and volcanic eruption signal from tree-ring width and maximum latewood density over the past 304 years in the southeastern Tibetan Plateau. International Journal of Biometeorology, 2017, 61: 2021-2032 [30] Zhao F, Fan Z, Su T, et al. Tree-ring δ18O inferred spring drought variability over the past 200 years in the Hengduan Mountains, Southwest China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2019, 518: 22-33 [31] Shi C, Daux V, Zhang QB, et al. Reconstruction of southeast Tibetan Plateau summer climate using tree ring δ18O: Moisture variability over the past two centuries. Climate of the Past, 2012, 8: 205-213 [32] 李明启, 邵雪梅. 基于树轮资料初探过去千年强火山喷发与青藏高原东部温度变化关系. 地球科学进展, 2016, 31(6): 634-642 [Li M-Q, Shao X-M. Study on the relationship between large volcanic eruptions and temperature variation based on tree-ring data in the eas-tern Tibetan Plateau during the past millennium. Advances in Earth Science, 2016, 31(6): 634-642] [33] Sigl M, Winstrup M, McConnell JR, et al. Timing and climate forcing of volcanic eruptions for the past 2500 years. Nature, 2015, 523: 543-549 [34] Chen F, Wang H, Yuan Y. Two centuries of temperature variation and volcanic forcing reconstructed for the northern Tibetan Plateau. Physical Geography, 2017, 38: 248-262 [35] Rao MP, Cook ER, Cook BI, et al. A double bootstrap approach to Superposed Epoch Analysis to evaluate response uncertainty. Dendrochronologia, 2019, 55: 119-124 [36] Zhang Y, Shao XM, Yin ZY, et al. Millennial minimum temperature variations in the Qilian Mountains, China: Evidence from tree rings. Climate of the Past, 2014, 10: 1763-1778 [37] Fan ZX, Bräuning A, Yang B, et al. Tree ring density-based summer temperature reconstruction for the central Hengduan Mountains in southern China. Global and Planetary Change, 2009, 65: 1-11 [38] Liang E, Shao X, Qin N. Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau. Global and Planetary Change, 2008, 61: 313-320 [39] Liang H, Lyu L, 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 [40] Zhu HF, Shao XM, Yin ZY, et al. August temperature variability in the southeastern Tibetan Plateau since AD 1385 inferred from tree rings. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 305: 84-92 [41] Wang B, Chen T, Xu G, et al. Reconstructed annual mean temperatures for the northeastern margin of the Tibetan Plateau: Associations with the East Asian monsoons and volcanic events. International Journal of Climatology, 2017, 37: 3044-3056 [42] Li MY, Wang L, Fan ZX, et al. Tree-ring density inferred late summer temperature variability over the past three centuries in the Gaoligong Mountains, southeastern Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 422: 57-64 [43] Fan ZX, Bräuning A, Tian QH, et al. Tree ring recorded May-August temperature variations since A.D. 1585 in the Gaoligong Mountains, southeastern Tibetan Pla-teau. Palaeogeography, Palaeoclimatology, Palaeoeco-logy, 2010, 296: 94-102 [44] Filion L, Payette S, Gauthier L, et al. Light rings in subarctic conifers as a dendrochronological tool. Quaternary Research, 1986, 26: 272-279 [45] Lamb HH. Climate, History and the Modern World. Oxfordshire, England, UK: Routledge, 1995: 436 [46] Oppenheimer C. Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815. Progress in Physical Geography, 2003, 27: 230-259 [47] Shi C, Wang K, Sun C, et al. Significantly lower summer minimum temperature warming trend on the sou-thern Tibetan Plateau than over the Eurasian continent since the industrial revolution. Environmental Research Letters, 2019, 14: 124033 [48] Wang L, Duan J, Chen J, et al. Temperature reconstruction from tree-ring maximum density of Belfour spruce in eastern Tibet, China. International Journal of Climatology, 2010, 30: 972-979 [49] Gou X, Yang T, Gao L, et al. A 457-year reconstruction of precipitation in the southeastern Qinghai-Tibet Plateau, China using tree-ring records. Chinese Science Bulletin, 2013, 58: 1107-1114 [50] Xing P, Zhang QB, Lv LX. Absence of late-summer warming trend over the past two and half centuries on the eastern Tibetan Plateau. Global and Planetary Change, 2014, 123: 27-35 [51] Zhu H, Zheng Y, Shao X, et al. Millennial temperature reconstruction based on tree-ring widths of Qilian juniper from Wulan, Qinghai Province, China. Chinese Science Bulletin, 2008, 53: 3914-3920 [52] Gou X, Peng J, Chen F, et al. A dendrochronological analysis of maximum summer half-year temperature variations over the past 700 years on the northeastern Tibetan Plateau. Theoretical and Applied Climatology, 2008, 93: 195-206 [53] Shindell DT, Schmidt GA, Miller RL, et al. Volcanic and solar forcing of climate change during the preindustrial era. Journal of Climate, 2003, 16: 4094-4107 [54] Briffa KR, Osborn TJ, Schweingruber FH. Large-scale temperature inferences from tree rings: A review. Global and Planetary Change, 2004, 40: 11-26 [55] Bräuning A. Dendrochronology for the last 1400 years in eastern Tibet. GeoJournal, 1994, 34: 75-95 [56] Bräuning A. Summer temperature and summer monsoon history on the Tibetan Plateau during the last 400 years recorded by tree rings. Geophysical Research Letters, 2004, 31: L24205 [57] Li J, Cook ER, D'Arrigo RO, et al. Common tree growth anomalies over the northeastern Tibetan Plateau during the last six centuries: Implications for regional moisture change. Global Change Biology, 2008, 14: 2096-2107 [58] Bräuning A. Tree-ring evidence of ‘Little Ice Age' gla-cier advances in southern Tibet. The Holocene, 2006, 16: 369-380 [59] Li ZS, Zhang QB, Ma K. Tree-ring reconstruction of summer temperature for A.D. 1475-2003 in the central Hengduan Mountains, northwestern Yunnan, China. Climatic Change, 2012, 110: 455-467 [60] Iles CE, Hegerl GC, Schurer AP, et al. The effect of volcanic eruptions on global precipitation. Journal of Geophysical Research: Atmospheres, 2013, 118: 8770-8786 [61] Breitenmoser P, Beer J, Brnnimann S, et al. Solar and volcanic fingerprints in tree-ring chronologies over the past 2000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 313: 127-139 [62] Fischer EM, Luterbacher J, Zorita E, et al. European climate response to tropical volcanic eruptions over the last half millennium. Geophysical Research Letters, 2007, 34, doi: 10.1029/2006GL027992 [63] Sheppard PR, Tarasov PE, Graumlich LJ, et al. Annual precipitation since 515 BC reconstructed from living and fossil juniper growth of northeastern Qinghai Province, China. Climate Dynamics, 2004, 23: 869-881 [64] Wernicke J, Hochreuther P, Grieinger J, et al. Multi-century humidity reconstructions from the southeastern Tibetan Plateau inferred from tree-ring δ18O. Global and Planetary Change, 2017, 149: 26-35 [65] Gao C, Gao Y, Zhang Q, et al. Climatic aftermath of the 1815 Tambora eruption in China. Journal of Meteo-rological Research, 2017, 31: 28-38 [66] Zuo M, Zhou T, Man W. Hydroclimate responses over global monsoon regions following volcanic eruptions at different latitudes. Journal of Climate, 2019, 32: 4367-4385 [67] Li J, Shi J, Zhang DD, et al. Moisture increase in response to high-altitude warming evidenced by tree-rings on the southeastern Tibetan Plateau. Climate Dynamics, 2017, 48: 649-660 [68] Liang E, Shao X, Liu X. Annual precipitation variation inferred from tree rings since AD 1770 for the western Qilian Mts., northern Tibetan Plateau. Tree-Ring Research, 2009, 65: 95-103 [69] Liu Y, An Z, Ma H, et al. Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the northern hemisphere temperature. Science in China Series D: Earth Sciences, 2006, 49: 408-420 [70] Shao X. Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai. Science in China Series D: Earth Sciences, 2005, 48: 939 [71] Huang JG, Zhang QB. Tree rings and climate for the last 680 years in Wulan Area of northeastern Qinghai-Tibe-tan Plateau. Climatic Change, 2007, 80: 369-377 [72] Zhang QB, Cheng G, Yao T, et al. A 2326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophysical Research Letters, 2003, 30: 10.1029/2003GL017425 [73] Stothers RB. The great Tambora eruption in 1815 and its aftermath. Science, 1984, 224: 1191-1198 [74] Cook ER, Anchukaitis KJ, Buckley BM, et al. Asian monsoon failure and megadrought during the last millennium. Science, 2010, 328: 486-489 [75] Trenberth KE, Dai A. Effects of Mount Pinatubo volca-nic eruption on the hydrological cycle as an analog of geoengineering. Geophysical Research Letters, 2007, 34: L15702 [76] Gennaretti F, Arseneault D, Nicault A, et al. Volcano-induced regime shifts in millennial tree-ring chronologies from northeastern North America. Proceedings of the National Academy of Sciences of the United States of America, 2014, 111: 10077-10082 |
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