ENSO对极端水文事件的影响机制研究综述及展望
A Review and Prospect on the Impact Mechanisms of ENSO on Extreme Hydrological Events
DOI: 10.12677/jwrr.2026.152013, PDF,    科研立项经费支持
作者: 何 难, 尹家波*, 李佳瑞, 沈玎睿, 胡千棋, 金妍岑, 付 湘*:武汉大学水资源与水电工程科学国家重点实验室,湖北 武汉
关键词: ENSO极端水文事件遥相关物理机制气候模型ENSO Hydrological Extremes Teleconnection Physical Mechanisms Climate Models
摘要: 厄尔尼诺–南方涛动(ENSO)是全球年际尺度最强的海气耦合信号,通过调制大气环流和水汽输运,深刻影响干旱和洪水等极端水文事件的时空分布、强度及传播规律。本文综述了ENSO对干旱、洪水、洪旱转换等极端水文事件影响的研究进展,重点分析了区域响应差异、物理驱动机制、模型模拟能力及外部强迫干扰四个核心方面。研究发现,ENSO对极端水文事件的影响呈现显著的空间异质性,主要通过“海温异常–环流调整–水汽输运–对流变化”的链式耦合过程影响旱涝灾害;另一方面,ENSO类型、外部强迫和下垫面条件等多重因素也对旱涝灾害产生显著影响。尽管现有气候模型能捕捉到ENSO与极端水文事件的主导关联,但在区域精细响应和外部强迫干扰模拟等方面仍有不足,未来需重点关注ENSO指数标准化、多因子耦合机制、物理引导模型改进及长时序重建等工作,为极端水文事件精准预测和灾害风险管理提供科学技术支撑。
Abstract: El Niño-Southern Oscillation (ENSO) is the strongest interannual air-sea coupled signal on the global scale, which profoundly affects the spatiotemporal distribution, intensity, and propagation of extreme hydrological events such as droughts and floods by modulating atmospheric circulation and moisture transport. This paper reviews the research progress of ENSO impacts on extreme hydrological events including droughts, floods, and flood-drought alternation, focusing on four core aspects: regional response differences, physical driving mechanisms, model simulation capabilities, and disturbances from external forcing. It is found that the impacts of ENSO on extreme hydrological events exhibit significant spatial heterogeneity, mainly through the chained coupling process of “sea surface temperature anomaly-circulation adjustment-moisture transport-convective variation” to influence droughts and floods; meanwhile, multiple factors such as ENSO types, external forcing, and underlying surface conditions also exert significant impacts on droughts and floods. Although existing climate models can capture the dominant correlation between ENSO and extreme hydrological events, there are still deficiencies in simulating fine-grained regional responses and disturbances from external forcing. Future work should focus on the standardization of ENSO indices, multi-factor coupling mechanisms, physically informed model improvements, and long-term reconstruction, to provide scientific and technological support for accurate prediction of extreme hydrological events and disaster risk management.
文章引用:何难, 尹家波, 李佳瑞, 沈玎睿, 胡千棋, 金妍岑, 付湘. ENSO对极端水文事件的影响机制研究综述及展望[J]. 水资源研究, 2026, 15(2): 97-106. https://doi.org/10.12677/jwrr.2026.152013

参考文献

[1] ZHANG, X., LI, J. B., XIE, S. P., et al. Volcanic eruptions disrupt ENSO teleconnections with land summer temperature. Nature Communications, 2025, 16(1): 9882. [Google Scholar] [CrossRef
[2] 夏军, 陈进, 佘敦先. 2022年长江流域极端干旱事件及其影响与对策[J]. 水利学报, 2022, 53(10): 1143-1153.
[3] 顾磊, 陈杰, 尹家波, 等. 气候变化下中国主要流域气象水文干旱潜在风险传播[J]. 水科学进展, 2021, 32(3): 321-333.
[4] XIONG, J., YANG, Y. Climate change and hydrological extremes. Current Climate Change Reports, 2025, 11(1): 1. [Google Scholar] [CrossRef
[5] LENGFELD, K., KIRSTETTER, P. E., FOWLER, H. J., et al. Use of radar data for characterizing extreme precipitation at fine scales and short durations. Environmental Research Letters, 2020, 15(8): 085003. [Google Scholar] [CrossRef
[6] MCPHADEN, M. J., ZEBIAK, S. E. and GLANTZ, M. H. ENSO as an integrating concept in earth science. Science, 2006, 314(5806): 1740-1745. [Google Scholar] [CrossRef] [PubMed]
[7] 张人禾, 闵庆烨, 苏京志. 厄尔尼诺对东亚大气环流和中国降水年际变异的影响: 西北太平洋异常反气旋的作用[J]. 中国科学: 地球科学, 2017, 47(5): 544-553.
[8] 陈文, 丁硕毅, 冯娟, 等. 不同类型ENSO对东亚季风的影响和机理研究进展[J]. 大气科学, 2018, 42(3): 640-655.
[9] CHEN, Y., MORTON, D. C., ANDELA, N., et al. A pan-tropical cascade of fire driven by El Niño/Southern Oscillation. Nature Climate Change, 2017, 7(12): 906-911. [Google Scholar] [CrossRef
[10] VAN OLDENBORGH, G. J., et al. Defining El Niño indices in a warming climate. Environmental Research Letters, 2021, 16: 044003.[CrossRef
[11] WU, X., TAN, X., CHEN, X., et al. Synoptic circulation forcing of large-scale extreme precipitation events over southeastern China. Journal of Geophysical Research: Atmospheres, 2024, 129(17): e2024JD041396. [Google Scholar] [CrossRef
[12] ZHANG, Q., LI, J., SINGH, V. P., et al. Influence of ENSO on precipitation in the East River basin, south China. Journal of Geophysical Research: Atmospheres, 2013, 118(5): 2207-2219. [Google Scholar] [CrossRef
[13] 杨晓霞, 吴娟, 刘佳, 等. 鄱阳湖流域极端降水时空变化特征及ENSO事件影响分析[J]. 水资源研究, 2021, 10(1): 33.
[14] GOSWAMI, B. N., VENUGOPAL, V., SENGUPTA, D., et al. Increasing trend of extreme rain events over India in a warming environment. Science, 2006, 314: 1442-1445.[CrossRef] [PubMed]
[15] HILL, S. A., MEYERS, D. Z., SOBEL, A. H., et al. More extreme Indian monsoon rainfall in El Niño summers. Science, 2025, 389(6753): 1220-1224. [Google Scholar] [CrossRef
[16] CAI, W., et al. Increasing frequency of extreme El Niño events due to greenhouse warming. Nature Climate Change, 2014, 4: 111-116.[CrossRef
[17] SUN, Q., MIAO, C., AGHAKOUCHAK, A., et al. Possible increased frequency of ENSO-related dry and wet conditions over some major watersheds in a warming climate. Bulletin of the American Meteorological Society, 2020, 101(4): E409-E426. [Google Scholar] [CrossRef
[18] LIU, W., WU, J., TANG, R., et al. Daily precipitation threshold for rainstorm and flood disaster in the mainland of China: An economic loss perspective. Sustainability, 2020, 12(1): 407. [Google Scholar] [CrossRef
[19] 冯扬, 秦鹏程, 胡一阳, 等. 长江流域复合极端气候事件指标及识别方法综述[J]. 人民长江, 2025, 56(3): 95-105.
[20] YU, J. Y., KAO, H. Y., LEE, T., et al. Subsurface ocean temperature indices for central-Pacific and eastern-Pacific types of El Niño and La Niña events. Theoretical and Applied Climatology, 2011, 103(3-4): 337-344. [Google Scholar] [CrossRef
[21] 袁媛, 杨辉, 李崇银. 不同分布型厄尔尼诺事件及对中国次年夏季降水的可能影响[J]. 气象学报, 2012, 70(3): 467-478.
[22] WALKER, G. T. On the meteorological evidence for supposed changes of climate in India. Technical Report, India Meteorological Department, 1910.
[23] KENYON, J., HEGERL, G. C. Influence of modes of climate variability on global precipitation extremes. Journal of Climate, 2010, 23(18): 6248-6262. [Google Scholar] [CrossRef
[24] POWER, S. B., CHUNG, C., KOCIUBA, G. and KEAY, K. Robust twenty-first-century projections of El Niño and related precipitation variability. Nature, 2013, 502: 541-545.[CrossRef] [PubMed]
[25] POWER, S. B., DELAGE, F. P. D. El Niño-Southern Oscillation and associated climatic conditions around the world during the latter half of the twenty-first century. Journal of Climate, 2018, 31(15): 6189-6207. [Google Scholar] [CrossRef
[26] D’ARRIGO, R., WILSON, R., PALMER, J., et al. Monsoon drought over Java, Indonesia, during the past two centuries. Geophysical Research Letters, 2006, 33(4): L04709. [Google Scholar] [CrossRef
[27] 龚道溢, 王绍武. ENSO对中国四季降水的影响[J]. 自然灾害学报, 1998, 7(4): 44-52.
[28] 马思源, 金燕, 张思, 等. 厄尔尼诺/南方涛动事件对云南秋季气象干旱的不同影响分析[J]. 干旱气象, 2023, 41(6): 860-872.
[29] 周建琴, 晏红明. 东部和中部型El Niño事件对云南冬季降水影响的差异分析[J]. 高原气象, 2021, 40(1): 98-108.
[30] 徐静, 张鑫. 青海省东部地区气候变化与ENSO事件关系[J]. 水文, 2012, 32(4): 88-95.
[31] 顾子也, 顾磊, 尹家波, 等. 中国陆域干旱的大气环流机制及旱情传播规律[J]. 中国科学: 地球科学, 2024, 54(8): 2674-2689.
[32] 尹家波, 郭生练, 杨妍, 等. 基于陆地水储量异常预估中国干旱及其社会经济暴露度[J]. 中国科学: 地球科学, 2022, 52(10): 2061-2076.
[33] STENCHIKOV, G., et al. Arctic Oscillation response to the 1991 Mount Pinatubo eruption: Effects of volcanic aerosols and ozone depletion. Journal of Geophysical Research: Atmospheres, 2002, 107: 4803.[CrossRef
[34] DOGAR, M. M., KUCHARSKI, F. and AZHARUDDIN, S. Study of the global and regional climatic impacts of ENSO magnitude using SPEEDY AGCM. Journal of Earth System Science, 2017, 126(2): 30. [Google Scholar] [CrossRef
[35] ATHIRA, K. S., ROXY, M. K., DASGUPTA, P., et al. Regional and temporal variability of Indian summer monsoon rainfall in relation to El Niño southern oscillation. Scientific Reports, 2023, 13(1): 12643. [Google Scholar] [CrossRef] [PubMed]
[36] WANG, B., LUO, X. and LIU, J. How robust is the Asian precipitation-ENSO relationship during the industrial warming period (1901-2017)? Journal of Climate, 2020, 33(7): 2779-2792. [Google Scholar] [CrossRef
[37] D’ARRIGO, R., SMERDON, J. E. Tropical climate influences on drought variability over Java, Indonesia. Geophysical Research Letters, 2008, 35(5): 2007GL032589. [Google Scholar] [CrossRef
[38] PRATIWI, E. P. A., MURTI, C. K. W. and WIDIASTUTI, E. I. Assessment of the 2015 and 2019 droughts in the rice agriculture sector in Java. In International Conference on Sustainable Environment, Agriculture and Tourism (ICOSEAT 2022). Dordrecht: Atlantis Press, 2022: 352-359.[CrossRef
[39] AGROTEKNOLOGI, P. S., PERTANIAN, F., JEMBER, U., et al. Pola Spasial Kekeringan di Jawa Barat Pada Kondisi El Nino Berbasis Metode Palmer Drought Severity Index (PDSI). Pengairan, 2021, 12(1): 16-29.[CrossRef
[40] NGUYEN, P., MIN, S. and KIM, Y. Combined impacts of the El Niño-Southern Oscillation and Pacific Decadal Oscillation on global droughts assessed using the standardized precipitation evapotranspiration index. International Journal of Climatology, 2021, 41(S1): E1645-E1662. [Google Scholar] [CrossRef
[41] YIN, H., WU, Z., FOWLER, H. J., et al. Combined impacts of ENSO and IOD on global seasonal droughts. Atmosphere, 2022, 13(10): 1673. [Google Scholar] [CrossRef
[42] LUO, J. J., LIU, G., HENDON, H., et al. Inter-basin sources for two-year predictability of the multi-year La Niña event in 2010-2012. Scientific Reports, 2017, 7(1): 2276. [Google Scholar] [CrossRef] [PubMed]
[43] DE LUCA, P., MESSORI, G., WILBY, R. L., et al. Concurrent wet and dry hydrological extremes at the global scale. Earth System Dynamics, 2020, 11(1): 251-266. [Google Scholar] [CrossRef
[44] 张忠禹, 贾文韬, 高振力, 等. ENSO对冬季中国近海海洋热浪事件的影响分析[J]. 气候变化研究快报, 2024, 13(6): 1554-1563.
[45] 盛宇裕, 毕硕本, 路明月, 等. 1951-2011年ENSO事件对秦岭-淮河地区旱涝灾害的影响分析[J]. 河南大学学报(自然科学版), 2019, 49(4): 418-428.
[46] 李芬, 张祎玮, 乔云红. 近56年山西季节旱涝对ENSO事件的响应[J]. 灾害学, 2015, 30(4): 85-90.
[47] 黄荣辉. 引起我国夏季旱涝的东亚大气环流异常遥相关及其物理机制的研究[J]. 大气科学, 1990, 14(1): 108-117.
[48] ZONG, H., LIU, Y., XIU, P., et al. Interannual variability of latent and sensible heat fluxes in the South China Sea. Chinese Journal of Oceanology and Limnology, 2010, 28(1): 153-159. [Google Scholar] [CrossRef
[49] LIU, K., XU, K., ZHU, C., et al. Diversity of marine heatwaves in the South China Sea regulated by ENSO phase. Journal of Climate, 2022, 35(2): 877-893. [Google Scholar] [CrossRef
[50] LI, X., ZHOU, W., CHEN, D., et al. Water vapor transport and moisture budget over Eastern China: Remote forcing from the two types of El Niño. Journal of Climate, 2014, 27(23): 8778-8792. [Google Scholar] [CrossRef
[51] WANG, Q., CAI, W., ZHONG, W., et al. Response of Southern China winter rainfall to El Niño diversity and its relevance to projected Southern China rainfall change. Journal of Climate, 2019, 32(11): 3343-3356. [Google Scholar] [CrossRef
[52] BETTS, R. A., JONES, C., KNIGHT, J. R., KEELING, R. and KENNEDY, J. J. El Niño and a record CO2 rise. Nature Climate Change, 2016, 6: 806-810.[CrossRef
[53] HE, N., YIN, J., LIU, P., et al. Global increases in dry-wet abrupt alternation events under climate change. Geophysical Research Letters, 2025, 52: e2025GL117322.[CrossRef
[54] FENG, J., CHEN, W. and LI, Y. J. Asymmetry of the winter extra-tropical teleconnections in the Northern Hemisphere associated with two types of ENSO. Climate Dynamics, 2017d, 48(7-8): 2135-2151. [Google Scholar] [CrossRef
[55] 闪丽洁, 张利平, 张艳军, 等. 长江中下游流域旱涝急转事件特征分析及其与ENSO的关系[J]. 地理学报, 2018, 73(1): 25-40.
[56] ALLAN, R. P., SODEN, B. J. Atmospheric warming and the amplification of precipitation extremes. Science, 2008, 321: 1481-1484.[CrossRef] [PubMed]
[57] MEEHL, G. A., HU, A. Megadroughts in the Indian monsoon region and southwest North America and a mechanism for associated multidecadal Pacific sea surface temperature anomalies. Journal of Climate, 2006, 19: 1605-1623.[CrossRef
[58] BELLENGER, H., GUILYARDI, E., LELOUP, J., LENGAIGNE, M. and VIALARD, J. ENSO representation in climate models: From CMIP3 to CMIP5. Climate Dynamics, 2014, 42: 1999-2018.[CrossRef
[59] KENT, C., SCAIFE, A. A., DUNSTONE, N. J., et al. Skilful global seasonal predictions from a machine learning weather model trained on reanalysis data. NPJ Climate and Atmospheric Science, 2025, 8(1): 314. [Google Scholar] [CrossRef
[60] HE, N., YIN, J., SLATER, L. J., et al. Global terrestrial drought and its projected socioeconomic implications under different warming targets. Science of the Total Environment, 2024, 946: 174292.[CrossRef] [PubMed]
[61] ROBOCK, A., MARQUARDT, A., KRAVITZ, B., et al. Benefits, risks, and costs of stratospheric geoengineering. Geophysical Research Letters, 2009, 36(19): 2009GL039209. [Google Scholar] [CrossRef
[62] SIGL, M., WINSTRUP, M., MCCONNELL, J.R., et al. Timing and climate forcing of volcanic eruptions for the past 2,500 years. Nature, 2015, 523(7562): 543-549. [Google Scholar] [CrossRef] [PubMed]
[63] 王远泽. 厄尔尼诺与南方涛动指数的研究综述[J]. 科技与创新, 2018(23): 82-83.
[64] WANG, S., HUANG, J., HE, Y., et al. Combined effects of the Pacific Decadal Oscillation and El Niño-Southern Oscillation on global land dry-wet changes. Scientific Reports, 2014, 4(1): 6651. [Google Scholar] [CrossRef] [PubMed]
[65] CHEN, S., CHEN, W., YING, J., et al. Interdecadal modulation of the Pacific Decadal Oscillation on the relationship between spring Arctic Oscillation and the following winter ENSO. Frontiers in Earth Science, 2022, 9: 810285.[CrossRef
[66] TIPPETT, M. K., L’HEUREUX, M. L., BECKER, E. J., et al. Excessive momentum and false alarms in late-spring ENSO forecasts. Geophysical Research Letters, 2020, 47(8): e2020GL087008. [Google Scholar] [CrossRef