Regional characteristics and mechanisms of lake water level decline in the Xizang Plateau since 2 000 years ago

WANG Yuhan; AN Fuyuan; LIU Xiangjun

doi:10.16562/j.cnki.0256-1492.2024021801

2024 Vol. 44, No. 2

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Article navigation > Marine Geology & Quaternary Geology > 2024 > 44(2): 55-68

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WANG Yuhan, AN Fuyuan, LIU Xiangjun. Regional characteristics and mechanisms of lake water level decline in the Xizang Plateau since 2 000 years ago[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 55-68. doi: 10.16562/j.cnki.0256-1492.2024021801

Citation:

WANG Yuhan, AN Fuyuan, LIU Xiangjun. Regional characteristics and mechanisms of lake water level decline in the Xizang Plateau since 2 000 years ago[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 55-68. doi: 10.16562/j.cnki.0256-1492.2024021801

Regional characteristics and mechanisms of lake water level decline in the Xizang Plateau since 2 000 years ago

1.
Key Laboratory of Xizang Plateau Surface Processes and Ecological Conservation, Ministry of Education, Qinghai Normal University, Xining 810008, China
2.
College of Geographic Sciences, Qinghai Normal University, Key Laboratory of Physical Geography and Environmental Processes of Qinghai Province, Xining 810008, China
3.
Institute of Plateau Science and Sustainable Development, Beijing Normal University, People's Government of Qinghai Province, Xining 810008, China
4.
College of Geographic Sciences and Tourism, Jiaying University, Meizhou 514015, China
5.
Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China

More Information

Corresponding authors: AN Fuyuan, dongzhu8@sina.com ; LIU Xiangjun, xiangjunliu@126.com

Received Date: 18 February 2024

Revised Date: 18 March 2024

Accepted Date: 18 March 2024

Publish Date: 28 April 2024

Abstract

Abstract

The Xizang Plateau (TP) was divided into three zones based on the influence of the Asian summer monsoon and the westerlies. By comparing multiple proxy indicators in sediments with late Holocene volcanic activity, the Northern Hemisphere temperatures, and the Asian monsoon index, the reasons for the decline in plateau lake levels ～2 kaBP were explored and the spatial differences in lake responses to climate fluctuations in the different zones were analyzed. Results show that the decline in lake water level in the southwestern part of the TP is greater than in the northwestern part, and even greater in the northeastern TP. This may be due to the weakening in the intensity of the Indian Summer Monsoon (ISM), which made lakes in the southwestern TP more dependent on the ISM precipitation replenishment and thus more sensitive to the reduction in water vapor flux brought by the ISM. Moreover, during this period, the phase of the North Atlantic Oscillation (NAO) shifted from negative to positive, leading to the increase in water vapor convergence in the northern part of the TP with more precipitation there, while the southern part of the TP received less rainfall, resulting in a generally greater decline in water levels in the southern lakes compared to those in the north. The main cause of the climate turning to colder and drier in the TP ～2 kaBP is attributed to the intensification of El Niño. In addition, the different phases of the Southern Annular Mode in winter and summer through complex ocean-atmosphere coupling processes crossing the equator, also played a role in cooling and dehumidifying the climate of the TP.
- climate change /
- Xizang Plateau lakes /
- Indian Summer Monsoon /
- ENSO /
- NAO

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References

[1]	Qiu J. China: the third pole[J]. Nature, 2008, 454(7203):393-396. doi: 10.1038/454393a CrossRef Google Scholar
[2]	Chen F H, Yu Z C, Yang M L, et al. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history[J]. Quaternary Science Reviews, 2008, 27(3-4):351-364. doi: 10.1016/j.quascirev.2007.10.017 CrossRef Google Scholar
[3]	Liu X J, Madsen D B, Liu R Y, et al. Holocene lake level variations of Longmu Co, western Qinghai-Xizang Plateau[J]. Environmental Earth Sciences, 2016, 75(4):301. doi: 10.1007/s12665-015-5188-7 CrossRef Google Scholar
[4]	Liu X J, Lai Z P, Madsen D, et al. Last deglacial and Holocene lake level variations of Qinghai lake, north-eastern Qinghai–Xizang Plateau[J]. Journal of Quaternary Science, 2015, 30(3):245-257. doi: 10.1002/jqs.2777 CrossRef Google Scholar
[5]	Shi X H, Kirby E, Furlong K P, et al. Rapid and punctuated late Holocene recession of Siling Co, central Xizang[J]. Quaternary Science Reviews, 2017, 172:15-31. doi: 10.1016/j.quascirev.2017.07.017 CrossRef Google Scholar
[6]	Huang C, Yu L P, Lai Z P. Holocene millennial lake-level fluctuations of Lake Nam Co in Xizang using OSL dating of shorelines[J]. Journal of Hydrology, 2023, 618:128643. doi: 10.1016/j.jhydrol.2022.128643 CrossRef Google Scholar
[7]	Huang L, Chen Y W, Wu Y, et al. Lake level changes of Nam Co since 25 ka as revealed by OSL dating of paleo-shorelines[J]. Quaternary Geochronology, 2022, 70:101274. doi: 10.1016/j.quageo.2022.101274 CrossRef Google Scholar
[8]	Ahlborn M, Haberzettl T, Wang J B, et al. Holocene lake level history of the Tangra Yumco lake system, southern-central Xizang Plateau[J]. The Holocene, 2016, 26(2):176-187. doi: 10.1177/0959683615596840 CrossRef Google Scholar
[9]	Cong L, Wang Y X, Zhang X Y, et al. Radiocarbon and luminescence dating of lacustrine sediments in Zhari Namco, southern Xizang Plateau[J]. Frontiers in Earth Science, 2021, 9:640172. doi: 10.3389/feart.2021.640172 CrossRef Google Scholar
[10]	Chen Y W, Zong Y Q, Li B, et al. Shrinking lakes in Xizang linked to the weakening Asian monsoon in the past 8.2 ka[J]. Quaternary Research, 2013, 80(2):189-198. doi: 10.1016/j.yqres.2013.06.008 CrossRef Google Scholar
[11]	Liu X J, Madsen D, Zhang X J. The driving forces underlying spatiotemporal lake extent changes in the inner Xizang Plateau during the Holocene[J]. Frontiers in Earth Science, 2021, 9:685928. doi: 10.3389/feart.2021.685928 CrossRef Google Scholar
[12]	丛禄, 王懿萱, 孙爱军, 等. 青藏高原中部当穹错末次冰消期以来湖面变化研究[J]. 第四纪研究, 2021, 41(6):1619-1631 doi: 10.11928/j.issn.1001-7410.2021.06.10 CrossRef Google Scholar CONG Lu, WANG Yixuan, SUN Aijun, et al. Lake level variations of Tanqung Co since last deglaciation, central Xizang Plateau[J]. Quaternary Sciences, 2021, 41(6):1619-1631.] doi: 10.11928/j.issn.1001-7410.2021.06.10 CrossRef Google Scholar
[13]	丛禄. 青藏高原全新世湖泊演化与其湖岸风成沉积物相关性研究[D]. 中国科学院大学(中国科学院青海盐湖研究所)博士学位论文, 2021 Google Scholar CONG Lu. The research of correlation relationship between evolution of typical lakes and lakeside's aeolian sediments within Xizang Plateau[D]. Doctor Dissertation of Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, 2021.] Google Scholar
[14]	Herzschuh U. Palaeo-moisture evolution in monsoonal Central Asia during the last 50, 000 years[J]. Quaternary Science Reviews, 2006, 25(1-2):163-178. doi: 10.1016/j.quascirev.2005.02.006 CrossRef Google Scholar
[15]	Herzschuh U, Mischke S, Meyer H, et al. Using variations in the stable carbon isotope composition of macrophyte remains to quantify nutrient dynamics in lakes[J]. Journal of Paleolimnology, 2010, 43(4):739-750. doi: 10.1007/s10933-009-9365-0 CrossRef Google Scholar
[16]	Cane M A. The evolution of El Niño, past and future[J]. Earth and Planetary Science Letters, 2005, 230(3-4):227-240. doi: 10.1016/j.jpgl.2004.12.003 CrossRef Google Scholar
[17]	Clement A C, Seager R, Cane M A. Suppression of El Niño during the mid-Holocene by changes in the Earth's orbit[J]. Paleoceanography, 2000, 15(6):731-737. doi: 10.1029/1999PA000466 CrossRef Google Scholar
[18]	Li C G, Wang M D, Liu W G, et al. Quantitative estimates of Holocene glacier meltwater variations on the Western Xizang Plateau[J]. Earth and Planetary Science Letters, 2021, 559:116766. doi: 10.1016/j.jpgl.2021.116766 CrossRef Google Scholar
[19]	Gasse F, Fontes J C, Van Campo E, et al. Holocene environmental changes in Bangong Co basin (Western Xizang). Part 4: discussion and conclusions[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1996, 120(1-2):79-92. doi: 10.1016/0031-0182(95)00035-6 CrossRef Google Scholar
[20]	Zhang Y Z, Zhang J W, McGowan S, et al. Climatic and environmental change in the western Xizang Plateau during the Holocene, recorded by lake sediments from Aweng Co[J]. Quaternary Science Reviews, 2021, 259:106889. doi: 10.1016/j.quascirev.2021.106889 CrossRef Google Scholar
[21]	Mishra P K, Prasad S, Anoop A, et al. Carbonate isotopes from high altitude Tso Moriri Lake (NW Himalayas) provide clues to late glacial and Holocene moisture source and atmospheric circulation changes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 425:76-83. doi: 10.1016/j.palaeo.2015.02.031 CrossRef Google Scholar
[22]	Yan D D, Wünnemann B. Late Quaternary water depth changes in Hala Lake, northeastern Xizang Plateau, derived from ostracod assemblages and sediment properties in multiple sediment records[J]. Quaternary Science Reviews, 2014, 95:95-114. doi: 10.1016/j.quascirev.2014.04.030 CrossRef Google Scholar
[23]	Zhang W Y, Mischke S, Hosner D, et al. Late glacial and Holocene climate in the Kunlun Pass region (northern Xizang Plateau) inferred from a multi-proxy lake record[J]. Quaternary International, 2023, 643:46-60. doi: 10.1016/j.quaint.2022.10.013 CrossRef Google Scholar
[24]	Wünnemann B, Yan D D, Andersen N, et al. A 14 ka high-resolution δ¹⁸O lake record reveals a paradigm shift for the process-based reconstruction of hydroclimate on the northern Xizang Plateau[J]. Quaternary Science Reviews, 2018, 200:65-84. doi: 10.1016/j.quascirev.2018.09.040 CrossRef Google Scholar
[25]	李友谟, 吴铎, 袁子杰, 等. 青藏高原腹地班德湖记录的全新世夏季风变化与流域环境响应[J]. 第四纪研究, 2022, 42(5):1328-1348 Google Scholar LI Youmo, WU Duo, YUAN Zijie, et al. Holocene summer monsoon variation and environmental response in the drainage basin of Lake Bande in the inner Xizang Plateau[J]. Quaternary Sciences, 2022, 42(5):1328-1348.] Google Scholar
[26]	Bird B W, Lei Y B, Perello M, et al. Late-Holocene Indian summer monsoon variability revealed from a 3300-year-long lake sediment record from Nir’pa Co, southeastern Xizang[J]. The Holocene, 2017, 27(4):541-552. doi: 10.1177/0959683616670220 CrossRef Google Scholar
[27]	Feng X P, Zhao C, D'Andrea W J, et al. Evidence for a relatively warm mid-to late holocene on the southeastern Xizang Plateau[J]. Geophysical Research Letters, 2022, 49(15):e2022GL098740. doi: 10.1029/2022GL098740 CrossRef Google Scholar
[28]	赵光通, 都永生, 魏海成, 等. 班戈错盐湖古湖岸堤石英光释光年代学及其古环境指示意义研究[J]. 盐湖研究, 2018, 26(3):26-34 Google Scholar ZHAO Guangtong, DU Yongsheng, WEI Haicheng, et al. Optically stimulated luminescence dating of paleo-shorelines of bange Co, Qinghai-Xizang Plateau and its implications for palaeo-environment[J]. Journal of Salt Lake Research, 2018, 26(3):26-34.] Google Scholar
[29]	Herzschuh U, Winter K, Wünnemann B, et al. A general cooling trend on the central Xizang Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra[J]. Quaternary International, 2006, 154-155:113-121. doi: 10.1016/j.quaint.2006.02.005 CrossRef Google Scholar
[30]	黄凌昕, 陈婕, 阳坤, 等. 现代青藏高原亚洲夏季风气候北界及其西风区和季风区划分[J]. 中国科学: 地球科学, 2023, 53(4): 866-678 Google Scholar HUANG Lingxin, CHEN Jie, YANG Kun, et al. The northern boundary of the Asian summer monsoon and division of westerlies and monsoon regimes over the Xizang Plateau in present-day[J]. Science China Earth Sciences, 2023, 66(4): 882-893.] Google Scholar
[31]	张镱锂, 李炳元, 刘林山, 等. 再论青藏高原范围[J]. 地理研究, 2021, 40(6):1543-1553 Google Scholar ZHANG Yili, LI Bingyuan, LIU Linshan, et al. Redetermine the region and boundaries of Xizang Plateau[J]. Geographical Research, 2021, 40(6):1543-1553.] Google Scholar
[32]	Gomez B, Carter L, Orpin A R, et al. ENSO/SAM interactions during the middle and late Holocene[J]. The Holocene, 2012, 22(1):23-30. doi: 10.1177/0959683611405241 CrossRef Google Scholar
[33]	Qiao B J, Zhu L P, Yang R M. Temporal-spatial differences in lake water storage changes and their links to climate change throughout the Xizang Plateau[J]. Remote Sensing of Environment, 2019, 222:232-243. doi: 10.1016/j.rse.2018.12.037 CrossRef Google Scholar
[34]	Yu W S, Ma Y M, Sun W Z, et al. Climatic significance of δ¹⁸O records from precipitation on the western Xizang Plateau[J]. Chinese Science Bulletin, 2009, 54(16):2732-2741. doi: 10.1007/s11434-009-0495-6 CrossRef Google Scholar
[35]	Gasse F, Arnold M, Fontes J C, et al. A 13, 000-year climate record from western Xizang[J]. Nature, 1991, 353(6346):742-745. doi: 10.1038/353742a0 CrossRef Google Scholar
[36]	Thompson L G, Severinghaus J P, Yao T D, et al. Use of δ¹⁸O_atm in dating a Xizang ice core record of Holocene/Late Glacial climate[J]. Proceedings of the National Academy of Sciences of the United States of America, 2022, 119(45):e2205545119. Google Scholar
[37]	Wu D, Ma X Y, Yuan Z J, et al. Holocene hydroclimatic variations on the Xizang Plateau: an isotopic perspective[J]. Earth-Science Reviews, 2022, 233:104169. doi: 10.1016/j.earscirev.2022.104169 CrossRef Google Scholar
[38]	Quade J, Broecker W S. Dryland hydrology in a warmer world: lessons from the Last Glacial period[J]. The European Physical Journal Special Topics, 2009, 176(1):21-36. doi: 10.1140/epjst/e2009-01146-y CrossRef Google Scholar
[39]	Rades E F, Tsukamoto S, Frechen M, et al. A lake-level chronology based on feldspar luminescence dating of beach ridges at Tangra Yum Co (southern Xizang)[J]. Quaternary Research, 2015, 83(3):469-478. doi: 10.1016/j.yqres.2015.03.002 CrossRef Google Scholar
[40]	Rades E F, Hetzel R, Xu Q, et al. Constraining Holocene lake-level highstands on the Xizang Plateau by ¹⁰Be exposure dating: a case study at Tangra Yumco, southern Xizang[J]. Quaternary Science Reviews, 2013, 82:68-77. doi: 10.1016/j.quascirev.2013.09.016 CrossRef Google Scholar
[41]	郑度, 李炳元. 青藏高原自然地理研究的进展[J]. 地理学报, 1990, 45(2):235-244 Google Scholar ZHENG Du, LI Bingyuan. Recent progress of geographical studies on the Qinghai-Xizang Plateau[J]. Acta Geographica Sinica, 1990, 45(2):235-244.] Google Scholar
[42]	Hou S G, Zhang W B, Pang H X, et al. Apparent discrepancy of Xizang ice core δ¹⁸O records may be attributed to misinterpretation of chronology[J]. The Cryosphere, 2019, 13(6):1743-1752. doi: 10.5194/tc-13-1743-2019 CrossRef Google Scholar
[43]	俞鸣同, 林振山, 杜建丽, 等. 格陵兰冰芯氧同位素显示近千年气候变化的多尺度分析[J]. 冰川冻土, 2009, 31(6):1037-1042 Google Scholar YU Mingtong, LIN Zhenshan, DU Jianli, et al. Multi-scale analysis of the last millennium climate variations in Greenland derived from ice core oxygen isotope[J]. Journal of Glaciology and Geocryology, 2009, 31(6):1037-1042.] Google Scholar
[44]	威廉斯, Dunkerley D L, De Deckker P, 等. 第四纪环境[M]. 刘东生, 译. 北京: 科学出版社, 1997 Google Scholar Williams M A J, Dunkerley D L, De Deckker P, et al. Quaternary Environments[M]. LIU Dongsheng, trans. Beijing: Science Press, 1997.] Google Scholar
[45]	Yang B, Qin C, Bräuning A, et al. Long-term decrease in Asian monsoon rainfall and abrupt climate change events over the past 6, 700 years[J]. Proceedings of the National Academy of Sciences of the United States of America, 2021, 118(30):e2102007118. Google Scholar
[46]	Shen J, Liu X Q, Wang S M, et al. Palaeoclimatic changes in the Qinghai Lake area during the last 18, 000 years[J]. Quaternary International, 2005, 136(1):131-140. doi: 10.1016/j.quaint.2004.11.014 CrossRef Google Scholar
[47]	Hou J Z, Huang Y S, Zhao J T, et al. Large Holocene summer temperature oscillations and impact on the peopling of the northeastern Xizang Plateau[J]. Geophysical Research Letters, 2016, 43(3):1323-1330. doi: 10.1002/2015GL067317 CrossRef Google Scholar
[48]	Kasper T, Wang J B, Schwalb A, et al. Precipitation dynamics on the Xizang Plateau during the Late Quaternary – Hydroclimatic sedimentary proxies versus lake level variability[J]. Global and Planetary Change, 2021, 205:103594. doi: 10.1016/j.gloplacha.2021.103594 CrossRef Google Scholar
[49]	Doberschütz S, Frenzel P, Haberzettl T, et al. Monsoonal forcing of Holocene paleoenvironmental change on the central Xizang Plateau inferred using a sediment record from Lake Nam Co (Xizang, China)[J]. Journal of Paleolimnology, 2014, 51(2):253-266. doi: 10.1007/s10933-013-9702-1 CrossRef Google Scholar
[50]	Kylander M E, Ampel L, Wohlfarth B, et al. High-resolution X-ray fluorescence core scanning analysis of Les Echets (France) sedimentary sequence: new insights from chemical proxies[J]. Journal of Quaternary Science, 2011, 26(1):109-117. doi: 10.1002/jqs.1438 CrossRef Google Scholar
[51]	Gyawali A R, Wang J B, Ma Q F, et al. Paleo-environmental change since the Late Glacial inferred from lacustrine sediment in Selin Co, central Xizang[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2019, 516:101-112. doi: 10.1016/j.palaeo.2018.11.033 CrossRef Google Scholar
[52]	Gu Z Y, Liu J Q, Yuan B Y, et al. Monsoon variations of the Qinghai-Xizang plateau during the last 12, 000 years: geochemical evidence from the sediments in the Siling Lake[J]. Chinese Science Bulletin, 1993, 38(7):577-581. doi: 10.1360/csb1993-38-7-577 CrossRef Google Scholar
[53]	Yao T D, Masson-Delmotte V, Gao J, et al. A review of climatic controls on δ¹⁸O in precipitation over the Xizang Plateau: observations and simulations[J]. Reviews of Geophysics, 2013, 51(4):525-548. doi: 10.1002/rog.20023 CrossRef Google Scholar
[54]	Chen F H, Zhang J F, Liu J B, et al. Climate change, vegetation history, and landscape responses on the Xizang Plateau during the Holocene: a comprehensive review[J]. Quaternary Science Reviews, 2020, 243:106444. doi: 10.1016/j.quascirev.2020.106444 CrossRef Google Scholar
[55]	Pang H X, Hou S G, Zhang W B, et al. Temperature trends in the northwestern Xizang Plateau constrained by ice core water isotopes over the past 7, 000 years[J]. Journal of Geophysical Research:Atmospheres, 2020, 125(19):e2020JD032560. doi: 10.1029/2020JD032560 CrossRef Google Scholar
[56]	Lang T J, Barros A P. Winter storms in the central Himalayas[J]. Journal of the Meteorological Society of Japan. Ser. II, 2004, 82(3):829-844. doi: 10.2151/jmsj.2004.829 CrossRef Google Scholar
[57]	Pang H, Hou S, Kaspari S, et al. Influence of regional precipitation patterns on stable isotopes in ice cores from the central Himalayas[J]. The Cryosphere, 2014, 8(1):289-301. doi: 10.5194/tc-8-289-2014 CrossRef Google Scholar
[58]	Feng L, Zhou T J. Water vapor transport for summer precipitation over the Xizang Plateau: multidata set analysis[J]. Journal of Geophysical Research:Atmospheres, 2012, 117(D20):D20114. Google Scholar
[59]	Zhang X J, Jin L Y, Jia W N. Centennial-scale teleconnection between North Atlantic sea surface temperatures and the Indian summer monsoon during the Holocene[J]. Climate Dynamics, 2016, 46(9):3323-3336. Google Scholar
[60]	Grossmann I, Klotzbach P J. A review of North Atlantic modes of natural variability and their driving mechanisms[J]. Journal of Geophysical Research:Atmospheres, 2009, 114(D24):D24107. Google Scholar
[61]	Knight J R, Folland C K, Scaife A A. Climate impacts of the Atlantic multidecadal oscillation[J]. Geophysical Research Letters, 2006, 33(17):L17706. Google Scholar
[62]	Li S L, Bates G T. Influence of the Atlantic multidecadal oscillation on the winter climate of East China[J]. Advances in Atmospheric Sciences, 2007, 24(1):126-135. doi: 10.1007/s00376-007-0126-6 CrossRef Google Scholar
[63]	刘焕才, 段克勤. 北大西洋涛动对青藏高原夏季降水的影响[J]. 冰川冻土, 2012, 34(2):311-318 Google Scholar LIU Huancai, DUAN Keqin. Effects of North Atlantic Oscillation on summer precipitation over the Xizang Plateau[J]. Journal of Glaciology and Geocryology, 2012, 34(2):311-318.] Google Scholar
[64]	Overpeck J, Anderson D, Trumbore S, et al. The southwest Indian Monsoon over the last 18 000 years[J]. Climate Dynamics, 1996, 12(3):213-225. doi: 10.1007/BF00211619 CrossRef Google Scholar
[65]	Wang C Z, Deser C, Yu J Y, et al. El Niño and southern oscillation (ENSO): a review[M]//Glynn P W, Manzello D P, Enochs I C. Coral Reefs of the Eastern Tropical Pacific: Persistence and Loss in a Dynamic Environment. Dordrecht: Springer, 2017: 85-106. Google Scholar
[66]	Srivastava G, Chakraborty A, Nanjundiah R S. Multidecadal variations in ENSO-Indian summer monsoon relationship at sub-seasonal timescales[J]. Theoretical and Applied Climatology, 2020, 140(3):1299-1314. Google Scholar
[67]	Lin S H, Yang S, He S, et al. Atmospheric–oceanic processes over the Pacific involved in the effects of the Indian summer monsoon on ENSO[J]. Journal of Climate, 2023, 36(17):6021-6043. doi: 10.1175/JCLI-D-22-0822.1 CrossRef Google Scholar
[68]	Brown J R, Hope P, Gergis J, et al. ENSO teleconnections with Australian rainfall in coupled model simulations of the last millennium[J]. Climate Dynamics, 2016, 47(1):79-93. Google Scholar
[69]	Conroy J L, Overpeck J T, Cole J E, et al. Holocene changes in eastern tropical Pacific climate inferred from a Galápagos lake sediment record[J]. Quaternary Science Reviews, 2008, 27(11-12):1166-1180. doi: 10.1016/j.quascirev.2008.02.015 CrossRef Google Scholar
[70]	Moy C M, Seltzer G O, Rodbell D T, et al. Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch[J]. Nature, 2002, 420(6912):162-165. doi: 10.1038/nature01194 CrossRef Google Scholar
[71]	Saji N H, Goswami B N, Vinayachandran P N, et al. A dipole mode in the tropical Indian Ocean[J]. Nature, 1999, 401(6751):360-363. Google Scholar
[72]	Zinke J, Pfeiffer M, Park W, et al. Seychelles coral record of changes in sea surface temperature bimodality in the western Indian Ocean from the Mid-Holocene to the present[J]. Climate Dynamics, 2014, 43(3-4):689-708. doi: 10.1007/s00382-014-2082-z CrossRef Google Scholar
[73]	Zinke J, Rountrey A, Feng M, et al. Corals record long-term Leeuwin current variability including Ningaloo Niño/Niña since 1795[J]. Nature Communications, 2014, 5(1):3607. doi: 10.1038/ncomms4607 CrossRef Google Scholar
[74]	Stuecker M F, Timmermann A, Jin F F, et al. Revisiting ENSO/Indian Ocean dipole phase relationships[J]. Geophysical Research Letters, 2017, 44(5):2481-2492. doi: 10.1002/2016GL072308 CrossRef Google Scholar
[75]	Hong C C, Li T, LinHo, et al. Asymmetry of the Indian Ocean Dipole. Part I: observational analysis[J]. Journal of Climate, 2008, 21(18):4834-4848. doi: 10.1175/2008JCLI2222.1 CrossRef Google Scholar
[76]	Cai W J, Zheng X T, Weller E, et al. Projected response of the Indian Ocean Dipole to greenhouse warming[J]. Nature Geoscience, 2013, 6(12):999-1007. doi: 10.1038/ngeo2009 CrossRef Google Scholar
[77]	黄怡陶, 张文君, 薛奥运. ENSO对印度洋偶极子非对称性的影响及机制研究[J]. 气象科学, 2023, 43(1):1-14 Google Scholar HUANG Yitao, ZHANG Wenjun, XUE Aoyun. Influence of ENSO on Indian Ocean Dipole skewness and its physical mechanism[J]. Journal of the Meteorological Sciences, 2023, 43(1):1-14.] Google Scholar
[78]	Haug G H, Hughen K A, Sigman D M, et al. Southward migration of the intertropical convergence zone through the Holocene[J]. Science, 2001, 293(5533):1304-1308. doi: 10.1126/science.1059725 CrossRef Google Scholar
[79]	Schneider T, Bischoff T, Haug G H. Migrations and dynamics of the intertropical convergence zone[J]. Nature, 2014, 513(7516):45-53. doi: 10.1038/nature13636 CrossRef Google Scholar
[80]	Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J]. Earth and Planetary Science Letters, 2005, 233(1-2):71-86. doi: 10.1016/j.jpgl.2005.01.036 CrossRef Google Scholar
[81]	Wang Y J, Cheng H, Edwards R L, et al. The Holocene Asian monsoon: links to solar changes and North Atlantic climate[J]. Science, 2005, 308(5723):854-857. doi: 10.1126/science.1106296 CrossRef Google Scholar
[82]	Mamalakis A, Randerson J T, Yu J Y, et al. Zonally contrasting shifts of the tropical rain belt in response to climate change[J]. Nature Climate Change, 2021, 11(2):143-151. doi: 10.1038/s41558-020-00963-x CrossRef Google Scholar
[83]	Marcott S A, Shakun J D, Clark P U, et al. A reconstruction of regional and global temperature for the past 11, 300 years[J]. Science, 2013, 339(6124):1198-1201. doi: 10.1126/science.1228026 CrossRef Google Scholar
[84]	Moreno P I, Vilanova I, Villa-Martínez R, et al. Onset and evolution of southern annular mode-like changes at centennial timescale[J]. Scientific Reports, 2018, 8(1):3458. doi: 10.1038/s41598-018-21836-6 CrossRef Google Scholar
[85]	Kobashi T, Menviel L, Jeltsch-Thömmes A, et al. Volcanic influence on centennial to millennial Holocene Greenland temperature change[J]. Scientific Reports, 2017, 7(1):1441. doi: 10.1038/s41598-017-01451-7 CrossRef Google Scholar
[86]	Thompson D W J, Wallace J M. Annular modes in the extratropical circulation. Part I: month-to-month variability[J]. Journal of Climate, 2000, 13(5):1000-1016. doi: 10.1175/1520-0442(2000)013<1000:AMITEC>2.0.CO;2 CrossRef Google Scholar
[87]	郑菲, 李建平, 刘婷. 南半球环状模气候影响的若干研究进展[J]. 气象学报, 2014, 72(5):926-939 Google Scholar ZHENG Fei, LI Jianping, LIU Ting. Some advances in studies of the climatic impacts of the Southern Hemisphere annular mode[J]. Acta Meteorologica Sinica, 2014, 72(5):926-939.] Google Scholar
[88]	豆娟. 南半球环状模对青藏高原及周边气候的可能影响[D]. 南京信息工程大学博士学位论文, 2019 Google Scholar DOU Juan. Possible influence of the Southern Hemiphere annular mode on the climate over the Xizang Plateau and its surrounding areas[D]. Doctor Dissertation of Nanjing University of Information Science & Technology, 2019.] Google Scholar
[89]	Zheng F, Li J P, Ding R Q. Influence of the preceding austral summer Southern Hemisphere annular mode on the amplitude of ENSO decay[J]. Advances in Atmospheric Sciences, 2017, 34(11):1358-1379. doi: 10.1007/s00376-017-6339-4 CrossRef Google Scholar
[90]	Silvestri G, Berman A L, Braconnot P, et al. Long-term trends in the Southern Annular Mode from transient Mid- to Late Holocene simulation with the IPSL-CM5A2 climate model[J]. Climate Dynamics, 2022, 59(3-4):903-914. doi: 10.1007/s00382-022-06160-0 CrossRef Google Scholar
[91]	Barnett T P, Dümenil L, Schlese U, et al. The effect of Eurasian snow cover on global climate[J]. Science, 1988, 239(4839):504-507. doi: 10.1126/science.239.4839.504 CrossRef Google Scholar
[92]	Yasunari T, Kitoh A, Tokioka T. Local and remote responses to excessive snow mass over Eurasia appearing in the northern spring and summer climate[J]. Journal of the Meteorological Society of Japan. Ser. II, 1991, 69(4):473-487. doi: 10.2151/jmsj1965.69.4_473 CrossRef Google Scholar
[93]	Hall A, Visbeck M. Synchronous variability in the Southern Hemisphere atmosphere, sea ice, and ocean resulting from the annular mode[J]. Journal of Climate, 2002, 15(21):3043-3057. doi: 10.1175/1520-0442(2002)015<3043:SVITSH>2.0.CO;2 CrossRef Google Scholar
[94]	Lefebvre W, Goosse H, Timmermann R, et al. Influence of the Southern Annular Mode on the sea ice–ocean system[J]. Journal of Geophysical Research:Oceans, 2004, 109(C9):C09005. Google Scholar
[95]	Zhang Y Z, Li J P, Zhao S, et al. Indian Ocean tripole mode and its associated atmospheric and oceanic processes[J]. Climate Dynamics, 2020, 55(5-6):1367-1383. doi: 10.1007/s00382-020-05331-1 CrossRef Google Scholar
[96]	Gill A E. Some simple solutions for heat-induced tropical circulation[J]. Quarterly Journal of the Royal Meteorological Society, 1980, 106(449):447-462. Google Scholar
[97]	Hoskins B J, Simmons A J, Andrews D G. Energy dispersion in a barotropic atmosphere[J]. Quarterly Journal of the Royal Meteorological Society, 1977, 103(438):553-567. doi: 10.1002/qj.49710343802 CrossRef Google Scholar
[98]	Hoskins B J, Karoly D J. The steady linear response of a spherical atmosphere to thermal and orographic forcing[J]. Journal of the Atmospheric Sciences, 1981, 38(6):1179-1196. doi: 10.1175/1520-0469(1981)038<1179:TSLROA>2.0.CO;2 CrossRef Google Scholar
[99]	Karoly D J. Southern hemisphere circulation features associated with El Niño-Southern Oscillation events[J]. Journal of Climate, 1989, 2(11):1239-1252. doi: 10.1175/1520-0442(1989)002<1239:SHCFAW>2.0.CO;2 CrossRef Google Scholar
[100]	Li L, Nathan T R. Effects of low-frequency tropical forcing on intraseasonal tropical–extratropical interactions[J]. Journal of the Atmospheric Sciences, 1997, 54(2):332-346. doi: 10.1175/1520-0469(1997)054<0332:EOLFTF>2.0.CO;2 CrossRef Google Scholar
[101]	Dou J, Wu Z W. Southern Hemisphere origins for interannual variations of snow cover over the western Xizang Plateau in boreal summer[J]. Journal of Climate, 2018, 31(19):7701-7718. doi: 10.1175/JCLI-D-17-0327.1 CrossRef Google Scholar
[102]	Xiao M Z, Zhang Q, Singh V P. Influences of ENSO, NAO, IOD and PDO on seasonal precipitation regimes in the Yangtze River basin, China[J]. International Journal of Climatology, 2015, 35(12):3556-3567. doi: 10.1002/joc.4228 CrossRef Google Scholar
[103]	Wang L, Chen W, Huang R H. Interdecadal modulation of PDO on the impact of ENSO on the East Asian winter monsoon[J]. Geophysical Research Letters, 2008, 35(20):L20702. Google Scholar
[104]	Sung M K, Kwon W T, Baek H J, et al. A possible impact of the North Atlantic Oscillation on the east Asian summer monsoon precipitation[J]. Geophysical Research Letters, 2006, 33(21):L21713. Google Scholar
[105]	Olsen J, Anderson N J, Knudsen M F. Variability of the North Atlantic Oscillation over the past 5, 200 years[J]. Nature Geoscience, 2012, 5(11):808-812. doi: 10.1038/ngeo1589 CrossRef Google Scholar
[106]	Chen C Z, Zhao W W, Zhang X J. Pacific Decadal Oscillation-like variability at a millennial timescale during the Holocene[J]. Global and Planetary Change, 2021, 199:103448. doi: 10.1016/j.gloplacha.2021.103448 CrossRef Google Scholar
[107]	Wang J L, Yang B, Qin C, et al. Spatial patterns of moisture variations across the Xizang Plateau during the past 700 years and their relationship with Atmospheric Oscillation modes[J]. International Journal of Climatology, 2014, 34(3):728-741. doi: 10.1002/joc.3715 CrossRef Google Scholar