Abstract
The middle and lower Yangtze River basin (MLYRB) suffered persistent heavy rainfall in summer 2020, with nearly continuous rainfall for about six consecutive weeks. How the likelihood of persistent heavy rainfall resembling that which occurred over the MLYRB in summer 2020 (hereafter 2020PHR-like event) would change under global warming is investigated. An index that reflects maximum accumulated precipitation during a consecutive five-week period in summer (Rx35day) is introduced. This accumulated precipitation index in summer 2020 is 60% stronger than the climatology, and a statistical analysis further shows that the 2020 event is a 1-in-70-year event. The model projection results derived from the 50-member ensemble of CanESM2 and the multimodel ensemble (MME) of the CMIP5 and CMIP6 models show that the occurrence probability of the 2020PHR-like event will dramatically increase under global warming. Based on the Kolmogorov—Smirnoff test, one-third of the CMIP5 and CMIP6 models that have reasonable performance in reproducing the 2020PHR-like event in their historical simulations are selected for the future projection study. The CMIP5 and CMIP6 MME results show that the occurrence probability of the 2020PHR-like event under the present-day climate will be double under lower-emission scenarios (CMIP5 RCP4.5, CMIP6 SSP1-2.6, and SSP2-4.5) and 3–5 times greater under higher-emission scenarios (3.0 times for CMIP5 RCP8.5, 2.9 times for CMIP6 SSP3-7.0, and 4.8 times for CMIP6 SSP5-8.5). The inter-model spread of the probability change is small, lending confidence to the projection results. The results provide a scientific reference for mitigation of and adaptation to future climate change.
摘要
2020年夏季, 长江中下游地区经历了一次持续性极端降水事件, 区域内日降水量连续近六周维持在较高水平. 本文对类2020年夏季长江中下游持续性极端降水事件发生概率在未来全球变暖背景下的变化进行了定量预估. 首先, 本文利用夏季连续五周最大累积降水量(Rx35day)表征持续性极端降水事件的强度, 结果表明2020年夏季长江中下游Rx35day较1951–2020年气候态偏强60%, 这是一次70年一遇的持续性极端降水事件. 进一步利用CanESM2模式50成员集合和CMIP5、 CMIP6多模式集合进行未来预估, 发现在全球变暖背景下, 类2020年持续性极端降水事件的发生概率将会显著增加. 具体来说, 本文先利用Kolmogorov–Smirnoff检验挑选出能合理再现当今气候背景下类2020年持续性极端降水事件的CMIP模式, 再对这些相对可靠的模式的未来情景模拟结果进行分析, 结果表明: 在低排放情景下(CMIP5 RCP4.5, CMIP6 SSP1-2.6和SSP2-4.5), 类2020年持续性极端降水事件发生概率约为当今气候背景下的2倍; 在高排放情景下, 该风险比率增至3–5倍(CMIP5 RCP8.5为3.0倍, CMIP6 SSP3-7.0为2.9倍, CMIP6 SSP5-8.5为4.8倍). 通过Bootstrap检验发现上述预估结果的不确定性较小, 说明在高排放情景下未来类2020年持续性极端降水事件发生概率很可能显著增加. 该研究结果说明了我国当前积极推广“碳中和”这一重要举措的必要性, 减缓和适应未来气候变化刻不容缓.
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References
Alexander, L. V., and Coauthors, 2006: Global observed changes in daily climate extremes of temperature and precipitation. J. Geophys. Res., 111, D05109, https://doi.org/10.1029/2005JD006290.
Arora, V. K., and Coauthors, 2011: Carbon emission limits required to satisfy future representative concentration pathways of greenhouse gases. Geophys. Res. Lett., 38, L05805, https://doi.org/10.1029/2010GL046270.
Berg, P., C. Moseley, and J. O. Haerter, 2013: Strong increase in convective precipitation in response to higher temperatures. Nature Geoscience, 6, 181–185, https://doi.org/10.1038/ngeo1731.
Chen, H. P., J. Q. Sun, and X. L. Chen, 2014: Projection and uncertainty analysis of global precipitation-related extremes using CMIP5 models. International Journal of Climatology, 34, 2730–2748, https://doi.org/10.1002/joc.3871.
Chen, M. Y., W. Shi, P. P. Xie, V. B. S. Silva, V. E. Kousky, R. Wayne Higgins, and J. E. Janowiak, 2008: Assessing objective techniques for gauge-based analyses of global daily precipitation. J. Geophys. Res., 113, D04110, https://doi.org/10.1029/2007JD009132.
Chen, X. D., A. G. Dai, Z. P. Wen, and Y. Y. Song, 2021: Contributions of Arctic Sea-Ice loss and East Siberian atmospheric blocking to 2020 record-breaking Meiyu-Baiu rainfall. Geophys. Res. Lett., 48, e2021GL092748, https://doi.org/10.1029/2021GL092748.
Chen, X. L., and T. J. Zhou, 2018: Relative contributions of external SST forcing and internal atmospheric variability to July—August heat waves over the Yangtze River valley. Climate Dyn., 51, 4403–4419, https://doi.org/10.1007/s00382-017-3871-y.
Chen, Y., and P. M. Zhai, 2013: Persistent extreme precipitation events in China during 1951–2010. Climate Research, 57, 143–155, https://doi.org/10.3354/cr01171.
Chen, Y., and P. M. Zhai, 2017: Revisiting summertime hot extremes in China during 1961–2015: Overlooked compound extremes and significant changes. Geophys. Res. Lett., 44, 5096–5103, https://doi.org/10.1002/2016GL072281.
Cressman, G. P., 1959: An operational objective analysis system. Mon. Wea. Rev., 87, 367–374, https://doi.org/10.1175/1520-0493(1959)087<0367:AOOAS>2.0.CO;2.
Dai, A. G., and T. B. Zhao, 2017: Uncertainties in historical changes and future projections of drought. Part I: Estimates of historical drought changes. Climatic Change, 144, 519–533, https://doi.org/10.1007/s10584-016-1705-2.
Deser, C., A. Phillips, V. Bourdette, and H. Y. Teng, 2012: Uncertainty in climate change projections: The role of internal variability. Climate Dyn., 38, 527–546, https://doi.org/10.1007/s00382-010-0977-x.
Ding, L. D., T. Li, and Y. Sun, 2021a: Subseasonal and synoptic variabilities of precipitation over the Yangtze River Basin in the summer of 2020. Adv. Atmos. Sci., 38, 2108–2124, https://doi.org/10.1007/s00376-021-1133-8.
Ding, Y. H., Z. Y. Wang, and Y. Sun, 2008: Inter — decadal variation of the summer precipitation in East China and its association with decreasing Asian summer monsoon. Part I: Observed evidences. International Journal of Climatology, 28, 1139–1161, https://doi.org/10.1002/joc.1615.
Ding, Y. H., Y. Sun, Z. Y. Wang, Y. X. Zhu, and Y. F. Song, 2009: Inter-decadal variation of the summer precipitation in China and its association with decreasing Asian summer monsoon Part II: Possible causes. International Journal of Climatology, 29, 1926–1944, https://doi.org/10.1002/joc.1759.
Ding, Y. H., Y. Y. Liu, and Z. Z. Hu, 2021b: The record-breaking mei-yu in 2020 and associated atmospheric circulation and tropical SST anomalies. Adv. Atmos. Sci., 38, 1980–1993, https://doi.org/10.1007/s00376-021-0361-2.
Du, H. B., and Coauthors, 2019: Precipitation from persistent extremes is increasing in most regions and globally. Geophys. Res. Lett., 46, 6041–6049, https://doi.org/10.1029/2019GL081898.
Easterling, D. R., G. A. Meehl, C. Parmesan, S. A. Changnon, T. R. Karl, and L. O. Mearns, 2000: Climate extremes: Observations, modeling, and impacts. Science, 289, 2068–2074, https://doi.org/10.1126/science.289.5487.2068.
Fang, C. X., Y. Liu, Q. F. Cai, and H. M. Song, 2021: Why does extreme rainfall occur in central China during the summer of 2020 after a weak El Niño. Adv. Atmos. Sci., 38, 2067–2081, https://doi.org/10.1007/s00376-021-1009-y.
Feng, S., S. Nadarajah, and Q. Hu, 2007: Modeling annual extreme precipitation in China using the generalized extreme value distribution. J. Meteor. Soc. Japan, 85, 599–613, https://doi.org/10.2151/jmsj.85.599.
Field, C. B., V. Barros, T. F. Stocker, and D. H. Qin, 2012: Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation. Cambridge University Press, 582 pp, https://doi.org/10.1017/CBO9781139177245.
Freychet, N., S. F. B. Tett, A. A. Abatan, A. Schurer, and Z. Feng, 2021: Widespread persistent extreme cold events over South — East China: Mechanisms, trends, and attribution. J. Geophys. Res., 126, https://doi.org/10.1029/2020JD033447.
Fyfe, J. C., and Coauthors, 2017: Large near-term projected snow-pack loss over the western United States. Nature Communications, 8, 14996, https://doi.org/10.1038/ncomms14996.
Guan, Y. H., X. C. Zhang, F. L. Zheng, and B. Wang, 2015: Trends and variability of daily temperature extremes during 1960–2012 in the Yangtze River Basin, China. Global and Planetary Change, 124, 79–94, https://doi.org/10.1016/j.gloplacha.2014.11.008.
Guan, Y. H., F. L. Zheng, X. C. Zhang, and B. Wang, 2017: Trends and variability of daily precipitation and extremes during 1960–2012 in the Yangtze River Basin, China. International Journal of Climatology, 37, 1282–1298, https://doi.org/10.1002/joc.4776.
Guo, Y. Y., R. J. Zhang, Z. P. Wen, J. C. Li, C. Zhang, and Z. J. Zhou, 2021: Understanding the role of SST anomaly in extreme rainfall of 2020 Meiyu season from an interdecadal perspective. Science China Earth Sciences, 64, 1619–1632, https://doi.org/10.1007/s11430-020-9762-0.
Habeeb, D., J. Vargo, and B. StoneJr., 2015: Rising heat wave trends in large US cities. Natural Hazards, 76, 1651–1665, https://doi.org/10.1007/s11069-014-1563-z.
He, B.-R., and P.-M. Zhai, 2018: Changes in persistent and non-persistent extreme precipitation in China from 1961 to 2016. Advances in Climate Change Research, 9, 177–184, https://doi.org/10.1016/j.accre.2018.08.002.
He, S. C., J. Yang, Q. Bao, L. Wang, and B. Wang, 2019: Fidelity of the observational/reanalysis datasets and global climate models in representation of extreme precipitation in East China. J. Climate, 32, 195–212, https://doi.org/10.1175/JCLI-D-18-0104.1.
Jones, P. D., S. C. B. Raper, R. S. Bradley, H. F. Diaz, P. M. Kellyo, and T. M. L. Wigley, 1986: Northern hemisphere surface air temperature variations: 1851–1984. J. Climate Appl. Meteorol., 28, 161–179, https://doi.org/10.1175/1520-0450(1986)025<0161:NHSATV>2.0.CO;2.
Karl, T. R., and R. W. Knight, 1998: Secular trends of precipitation amount, frequency, and intensity in the United States. Bull. Amer. Meteor. Soc., 79, 231–242, https://doi.org/10.1175/1520-0477(1998)079<0231:STOPAF>2.0.CO;2.
Kharin, V. V., F. W. Zwiers, X. Zhang, and M. Wehner, 2013: Changes in temperature and precipitation extremes in the CMIP5 ensemble. Climatic Change, 119, 345–357, https://doi.org/10.1007/s10584-013-0705-8.
Lehmann, J., D. Coumou, and K. Frieler, 2015: Increased record-breaking precipitation events under global warming. Climatic Change, 132, 501–515, https://doi.org/10.1007/s10584-015-1434-y.
Lenderink, G., and E. van Meijgaard, 2008: Increase in hourly precipitation extremes beyond expectations from temperature changes. Nature Geoscience, 1, 511–514, https://doi.org/10.1038/ngeo262.
Li, C. F., W. Chen, X. W. Hong, and R. Y. Lu, 2017: Why was the strengthening of rainfall in summer over the Yangtze River valley in 2016 less pronounced than that in 1998 under similar preceding El Niño events?—Role of midlatitude circulation in August Adv. Atmos. Sci., 34, 1290–1300, https://doi.org/10.1007/s00376-017-7003-8.
Li, C., F. Zwiers, X. Zhang, G. Li, Y. Sun, and M. Wehner, 2021a: Changes in Annual Extremes of Daily Temperature and Precipitation in CMIP6 Models. Journal of Climate, 34, 3441–3460.
Li, C. F., R. Y. Lu, N. Dunstone, A. A. Scaife, P. E. Bett, and F. Zheng, 2021b: The seasonal prediction of the exceptional Yangtze River rainfall in summer 2020. Adv. Atmos. Sci., 38, 2055–2066, https://doi.org/10.1007/s00376-021-1092-0.
Liu, B. Q., Y. H. Yan, C. W. Zhu, S. M. Ma, and J. Y. Li, 2020: Record-breaking Meiyu rainfall around the Yangtze River in 2020 regulated by the subseasonal phase transition of the North Atlantic oscillation. Geophys. Res. Lett., 47, e2020GL090342, https://doi.org/10.1029/2020GL090342.
Liu, Y. Y. and Y. H. Ding, 2020: Characteristics and possible causes for the extreme Meiyu in 2020. Meteorological Monthly, 46, 1393–1404, https://doi.org/10.7519/j.issn.1000-0526.2020.11.001. (in Chinese with English abstract)
Lu, R., 2000: Anomalies in the Tropics Associated with the Heavy Rainfall in East Asia during the Summer of 1998. Advances in Atmospheric Sciences, 17, 205–220.
Luo, Y. L., W. M. Qian, R. H. Zhang, and D.-L. Zhang, 2013: Gridded hourly precipitation analysis from high-density rain gauge network over the Yangtze—Huai Rivers Basin during the 2007 mei-yu season and comparison with CMORPH. Journal of Hydrometeorology, 14, 1243–1258, https://doi.org/10.1175/JHM-D-12-0133.1.
Luo, Z. Q., J. Yang, M. N. Gao, and D. L. Chen, 2020: Extreme hot days over three global mega-regions: Historical fidelity and future projection. Atmospheric Science Letters, 21, e1003, https://doi.org/10.1002/asl.1003.
Meinshausen, M., and Coauthors, 2019: The SSP greenhouse gas concentrations and their extensions to 2500. Geoscientific Model Development, https://doi.org/10.5194/gmd-2019-222.
Nanding, N., and Coauthors, 2020: Anthropogenic Influences on 2019 July Precipitation Extremes Over the Mid—Lower Reaches of the Yangtze River. Frontiers in Environmental Science, 8.
O’Neill, B. C., and Coauthors, 2016: The scenario model intercomparison project (ScenarioMIP) for CMIP6. Geoscientific Model Development, 9, 3461–3482, https://doi.org/10.5194/gmd-9-3461-2016.
Pan, X., T. Li, Y. Sun, and Z. W. Zhu, 2021: Cause of extreme heavy and persistent rainfall over Yangtze River in summer 2020. Adv. Atmos. Sci., 38, 1994–2009, https://doi.org/10.1007/s00376-021-0433-3.
Papalexiou, S. M., and A. Montanari, 2019: Global and regional increase of precipitation extremes under global warming. Water Resour. Res., 55, 4901–4914, https://doi.org/10.1029/2018WR024067.
Perkins-Kirkpatrick, S. E., and P. B. Gibson, 2017: Changes in regional heatwave characteristics as a function of increasing global temperature. Scientific Reports, 7, 12256, https://doi.org/10.1038/s41598-017-12520-2.
Pfleiderer, P., C.-F. Schleussner, K. Kornhuber, and D. Coumou, 2019: Summer weather becomes more persistent in a 2°C world. Nature Climate Change, 9, 666–671, https://doi.org/10.1038/s41558-019-0555-0.
Qiao, S. B., and Coauthors, 2021: The longest 2020 meiyu season over the past 60 years: Subseasonal perspective and its predictions. Geophys. Res. Lett., 48, e2021GL093596, https://doi.org/10.1029/2021GL093596.
Ren, L. W., and Coauthors, 2020: Anthropogenic influences on the persistent night-time heat wave in Summer 2018 over Northeast China. Bull. Amer. Meteor. Soc., 101, S83–S88, https://doi.org/10.1175/BAMS-D-19-0152.1.
Ren, Z. H., Y. Yu, F. L. Zou, and Y. Xu, 2012: Quality detection of surface historical basic meteorological data. Journal of Applied Meteorological Science, 23, 739–747, https://doi.org/10.3969/j.issn.1001-7313.2012.06.011. (in Chinese with English abstract)
Sillmann, J., V. V. Kharin, X. Zhang, F. W. Zwiers, and D. Bronaugh, 2013a: Climate extremes indices in the CMIP5 multimodel ensemble: Part 1. Model evaluation in the present climate. J. Geophys. Res., 118, 1716–1733, https://doi.org/10.1002/jgrd.50203.
Sillmann, J., V. V. Kharin, F. W. Zwiers, X. Zhang, and D. Bronaugh, 2013b: Climate extremes indices in the CMIP5 multimodel ensemble: Part 2. Future climate projections. J. Geophys. Res., 118, 2473–2493, https://doi.org/10.1002/jgrd.50188.
Stocker, T. F., and Coauthors, 2013: Climate Change 2013: The Physical Science Basis. Cambridge University Press, 1535 pp.
Su, B. D., T. Jiang, and W. B. Jin, 2006: Recent trends in observed temperature and precipitation extremes in the Yangtze River basin, China. Theor. Appl. Climatol., 83, 139–151, https://doi.org/10.1007/s00704-005-0139-y.
Sun, J. Q., and J. Ao, 2013: Changes in precipitation and extreme precipitation in a warming environment in China. Chinese Science Bulletin, 58, 1395–1401, https://doi.org/10.1007/s11434-012-5542-z.
Sun, J. Q., H. J. Wang, W. Yuan, and H. P. Chen, 2010: Spatial-temporal features of intense snowfall events in China and their possible change. J. Geophys. Res., 115, D16110, https://doi.org/10.1029/2009JD013541.
Sun, Y., X. B. Zhang, F. W. Zwiers, L. C. Song, H. Wan, T. Hu, H. Yin, and G. Y. Ren, 2014: Rapid increase in the risk of extreme summer heat in Eastern China. Nature Climate Change, 4, 1082–1085, https://doi.org/10.1038/nclimate2410.
Takaya, Y., I. Ishikawa, C. Kobayashi, H. Endo, and T. Ose, 2020: Enhanced Meiyu-baiu rainfall in early summer 2020: Aftermath of the 2019 super IOD event. Geophys. Res. Lett., 47, e2020GL090671, https://doi.org/10.1029/2020GL090671.
Tang, S. L., J.-J. Luo, J. Y. He, J. Y. Wu, Y. Zhou, and W. S. Ying, 2021: Toward understanding the extreme floods over Yangtze River Valley in June–July 2020: Role of Tropical Oceans. Adv. Atmos. Sci., 38, 2023–2039, https://doi.org/10.1007/s00376-021-1036-8.
Trenberth, K. E., 2011: Changes in precipitation with climate change. Climate Research, 47, 123–138, https://doi.org/10.3354/cr00953.
Trenberth, K. E., A. G. Dai, G. van der Schrier, P. D. Jones, J. Barichivich, K. R. Briffa, and J. Sheffield, 2014: Global warming and changes in drought. Nature Climate Change, 4, 17–22, https://doi.org/10.1038/nclimate2067.
von Salzen, K., and Coauthors, 2013: The Canadian fourth generation atmospheric global climate model (CanAM4). Part I: Representation of physical processes. Atmosphere-Ocean, 51, 104–125, https://doi.org/10.1080/07055900.2012.755610.
Wang, B., R. G. Wu, and X. H. Fu, 2000a: Pacific—East Asian teleconnection: How Does ENSO affect East Asian climate. J. Climate, 13, 1517–1536, https://doi.org/10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2.
Wang, C., K. Wu, L. G. Wu, H. K. Zhao, and J. Cao, 2021a: What caused the unprecedented absence of Western North Pacific tropical cyclones in July 2020. Geophys. Res. Lett., 48, e2020GL092282, https://doi.org/10.1029/2020GL092282.
Wang, J., Y. Chen, S. F. B. Tett, Z. W. Yan, P. M. Zhai, J. M. Feng, and J. J. Xia, 2020b: Anthropogenically-driven increases in the risks of summertime compound hot extremes. Nature Communications, 11, 528, https://doi.org/10.1038/s41467-019-14233-8.
Wang, S. S., J. P. Huang, and X. Yuan, 2021b: Attribution of 2019 extreme spring—early summer hot drought over Yunnan in Southwestern China. Bull. Amer. Meteor. Soc., 102, S91–S96, https://doi.org/10.1175/BAMS-D-20-0121.1.
Wartenburger, R., M. Hirschi, M. G. Donat, P. Greve, A. J. Pitman, and S. I. Seneviratne, 2017: Changes in regional climate extremes as a function of global mean temperature: An interactive plotting framework. Geoscientific Model Development, 10, 3609–3634, https://doi.org/10.5194/gmd-10-3609-2017.
Wu, J., B.-T. Zhou, and Y. Xu, 2015: Response of precipitation and its extremes over China to warming: CMIP5 simulation and projection. Chinese Journal of Geophysics, 58, 461–473, https://doi.org/10.1002/cjg2.20187.
Xie, S.-P., and Coauthors, 2015: Towards predictive understanding of regional climate change. Nature Climate Change, 5, 921–930, https://doi.org/10.1038/nclimate2689.
Ye, D. X., J. F. Yin, Z. H. Chen, Y. F. Zheng, and R. J. Wu, 2014: Spatial and temporal variations of heat waves in China from 1961 to 2010. Advances in Climate Change Research, 5, 66–73, https://doi.org/10.3724/SPJ.1248.2014.066.
Ye, Y. B., and C. Qian, 2021: Conditional attribution of climate change and atmospheric circulation contributing to the record-breaking precipitation and temperature event of summer 2020 in southern China. Environmental Research Letters, 16, 044058, https://doi.org/10.1088/1748-9326/abeeaf.
Zhai, P. M., X. B. Zhang, H. Wan, and X. H. Pan, 2005: Trends in total precipitation and frequency of daily precipitation extremes over China. J. Climate, 18, 1096–1108, https://doi.org/10.1175/JCLI-3318.1.
Zhang, Q., C.-Y. Xu, Z. X. Zhang, Y. D. Chen, C.-L. Liu, and H. Lin, 2008: Spatial and temporal variability of precipitation maxima during 1960–2005 in the Yangtze River basin and possible association with large-scale circulation. J. Hydrol., 353, 215–227, https://doi.org/10.1016/j.jhydrol.2007.11.023
Zhang, W. J., Z. C. Huang, F. Jiang, M. F. Stuecker, G. S. Chen, and F.-F. Jin, 2021: Exceptionally persistent madden — julian oscillation activity contributes to the extreme 2020 East Asian summer monsoon rainfall. Geophys. Res. Lett., 48, e2020GL091588, https://doi.org/10.1029/2020GL091588.
Zhang, W. X., and T. J. Zhou, 2020: Increasing impacts from extreme precipitation on population over China with global warming. Science Bulletin, 65, 243–252, https://doi.org/10.1016/j.scib.2019.12.002.
Zhang, W. X., and Coauthors, 2020: Anthropogenic influence on 2018 summer persistent heavy rainfall in central Western China. Bull. Amer. Meteor. Soc., 101, S65–S70, https://doi.org/10.1175/BAMS-D-19-0147.1.
Zhang, X.-L., S.-Y. Tao, and J. Wei, 2006: An analysis on the Basin-wide catastrophic floods in the Yangtze River during the 20th Century. Climatic and Environmental Research, 11, 669–682, https://doi.org/10.3969/j.issn.1006-9585.2006.06.001. (in Chinese with English abstract)
Zhao, P., S. Yang, and R. C. Yu, 2010: Long-term changes in rainfall over eastern China and large-scale atmospheric circulation associated with recent global warming. J. Climate, 23, 1544–1562, https://doi.org/10.1175/2009JCLI2660.1.
Zheng, J. Y., and C. Z. Wang, 2021: Influences of three oceans on record-breaking rainfall over the Yangtze River Valley in June 2020. Science China Earth Sciences, 64, 1607–1618, https://doi.org/10.1007/s11430-020-9758-9.
Zhou, B. T., Q. H. Wen, Y. Xu, L. C. Song, and X. B. Zhang, 2014: Projected changes in temperature and precipitation extremes in China by the CMIP5 multimodel ensembles. J. Climate, 27, 6591–6611, https://doi.org/10.1175/JCLI-D-13-00761.1.
Zhou, C. L., K. C. Wang, D. Qi, and J. G. Tan, 2019: Attribution of a record-breaking heatwave event in summer 2017 over the Yangtze River delta. Bull. Amer. Meteor. Soc., 100, S97–S103, https://doi.org/10.1175/BAMS-D-18-0134.1.
Zhou, T. J., L. W. Ren, and W. X. Zhang, 2021a: Anthropogenic influence on extreme Meiyu rainfall in 2020 and its future risk. Science China Earth Sciences, 64, 1633–1644, https://doi.org/10.1007/s11430-020-9771-8.
Zhou, Z.-Q., S.-P. Xie, and R. H. Zhang, 2021b: Historic Yangtze flooding of 2020 tied to extreme Indian Ocean conditions. Proceedings of the National Academy of Sciences of the United States of America, 118, e2022255118, https://doi.org/10.1073/pnas.2022255118.
Zhu, C. W., B. Wang, W. H. Qian, and B. Zhang, 2012: Recent weakening of northern East Asian summer monsoon: A possible response to global warming. Geophys. Res. Lett., 39, L09701, https://doi.org/10.1029/2012GL051155.
Zhu, H. H., Z. H. Jiang, J. Li, W. Li, C. X. Sun, and L. Li, 2020: Does CMIP6 inspire more confidence in simulating climate extremes over China? Adv. Atmos. Sci., 37, 1119–1132, https://doi.org/10.1007/s00376-020-9289-1.
Acknowledgements
We would like to thank Dr. Wenxia ZHANG for helpful discussion and anonymous reviewers for insightful suggestions and comments. This work was jointly supported by the National Natural Science Foundation of China (Grant No. 42088101), the National Key Research and Development Program of China (2020YFA0608901 and 2019YFC1510004), the Natural Science Foundation of Jiangsu (BK20190781), the National Natural Science Foundation of China (Grant No. 42005020), and the General Program of Natural Science Foundation of Jiangsu Higher Education Institutions (19KJB170019).
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Article Highlights
• The middle and lower Yangtze River basin suffered extremely persistent and heavy rainfall in summer 2020, with the maximum accumulated rainfall over five consecutive weeks being 60% above the 1951–2020 climatology.
• The occurrence probability of the 2020PHR-like event under the present-day climate will be double under lower-emission scenarios (CMIP5 RCP4.5, CMIP6 SSP1-2.6, and SSP2-4.5) and 3–5 times greater under higher-emission scenarios (3.0 times for CMIP5 RCP8.5, 2.9 times for CMIP6 SSP3-7.0, and 4.8 times for CMIP6 SSP5-8.5).
• The increase of the occurrence probability becomes sharper in the high-GHG-emission scenarios than in the low-GHG-emission scenarios, indicating the importance of carbon emission reduction.
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How Frequently Will the Persistent Heavy Rainfall over the Middle and Lower Yangtze River Basin in Summer 2020 Happen under Global Warming?
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Ge, ZA., Chen, L., Li, T. et al. How Frequently Will the Persistent Heavy Rainfall over the Middle and Lower Yangtze River Basin in Summer 2020 Happen under Global Warming?. Adv. Atmos. Sci. 39, 1673–1692 (2022). https://doi.org/10.1007/s00376-022-1351-8
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DOI: https://doi.org/10.1007/s00376-022-1351-8
Key words
- persistent heavy rainfall
- middle and lower Yangtze River basin
- future projection
- CMIP5 and CMIP6 models
- generalized extreme value (GEV) distribution