Abstract
Extreme high temperatures frequently occur in southwestern China, significantly impacting the local ecological system and economic development. However, accurate prediction of extreme high-temperature days (EHDs) in this region is still an unresolved challenge. Based on the spatiotemporal characteristics of EHDs over China, a domain-averaged EHD index over southwestern China (SWC-EHDs) during April–May is defined. The simultaneous dynamic and thermodynamic fields associated with the increased SWC-EHDs are a local upper-level anticyclonic (high-pressure) anomaly and wavy geopotential height anomaly patterns over Eurasia. In tracing the origins of the lower boundary anomalies, two physically meaningful precursors are detected for SWC-EHDs. They are the tripolar SST change tendency from December–January to February–March in the northern Atlantic and the February–March mean snow depth in central Asia. Using these two selected predictors, a physics-based empirical model prediction was applied to the training period of 1961–2005 to obtain a skillful prediction of the EHDs index, attaining a correlation coefficient of 0.76 in the independent prediction period (2006–19), suggesting that 58% of the total SWC-EHDs variability is predictable. This study provides an estimate for the lower bound of the seasonal predictability of EHDs as well as for the hydrological drought over southwestern China.
摘 要
近年来,中国西南地区极端高温事件频发,对当地生态系统和经济发展产生严重影响。然而,准确预测该地区极端高温日数年际变化仍具挑战。基于中国极端高温日数时空分布特征,本文定义了4-5月中国西南区域平均极端高温日数指数(SWC-EHDs)。从SWC-EHDs相关同期环流场上发现西南地区极端高温日数的增加伴随着局地高空反气旋(高压)异常和欧亚大陆上空呈波列形势的位势高度异常。通过诊断SWC-EHDs相关的前期下垫面异常,挑选出两个具有物理意义的前兆信号。第一个信号是12-1月至2-3月的北大西洋海温三级子变化倾向;第二个信号是中亚地区2-3月平均的积雪深度。利用1961-2005年训练期的前兆信号建立基于物理机制的SWC-EHDs季节预报模型,该模型在独立预测时期(2006-2019年)预报的SWC-EHDs相关系数可达0.76,表明其变率的58%是可预测的。本研究可为西南地区极端高温日数以及气象水文干旱的季节预测提供参考。
Similar content being viewed by others
Data Availability Statement
The monthly mean SST data can be obtained at https://psl.noaa.gov/data/gridded/data.noaa.ersst.v5.html, global monthly precipitation data can be downloaded from https://psl.noaa.gov/data/gridded/data.prec.html, ERA-40 and ERA-Interim data can be obtained from https://apps.ecmwf.int/datasets/.
References
Alexander, L. V., and Coauthors, 2006: Global observed changes in daily climate extremes of temperature and precipitation. J. Geophys. Res.: Atmos., 111, D05109, https://doi.org/10.1029/2005JD006290.
Ambrizzi, T., B. J. Hoskins, and H. H. Hsu, 1995: Rossby wave propagation and teleconnection patterns in the austral winter. J. Atmos. Sci., 52(21), 3661–3672, https://doi.org/10.1175/1520-0469(1995)052<3661:RWPATP>2.0.CO;2.
Barnston, A. G., and R. E. Livezey, 1987: Classification, seasonality and persistence of low-frequency atmospheric circulation patterns. Mon. Wea. Rev., 115(6), 1083–1126, https://doi.org/10.1175/1520-0493(1987)115<1083:CSAPOL>2.0.CO;2.
Chao, Q. C., Z. W. Yan, Y. Sun, Z. H. Jang, H. Liao, G. S. Jia, and R. S. Cai, 2020: A recent scientific understanding of climate change in China. China Population, Resources and Environment, 30(3), 1–9, (in Chinese with English abstract)
Chen, M. Y., P. P. Xie, J. E. Janowiak, and P. A. Arkin, 2002: Global land precipitation: A 50-yr monthly analysis based on gauge observations. Journal of Hydrometeorology, 3(3), 249–266, https://doi.org/10.1175/1525-7541(2002)003<0249:GLPAYM>2.0.CO;2.
Chen, W., and B. W. Dong, 2019: Anthropogenic impacts on recent decadal change in temperature extremes over China: Relative roles of greenhouse gases and anthropogenic aerosols. Climate Dyn., 52, 3643–3660, https://doi.org/10.1007/s00382-018-4342-9.
Dee, D. P., and Coauthors, 2011: The ERA-Interim reanalysis: Configuration and performance of the data assimilation system. Quart. J. Roy. Meteor. Soc., 137(656), 553–597, https://doi.org/10.1002/qj.828.
Ding, T., and H. Gao, 2020: The record-breaking extreme drought in Yunnan province, Southwest China during spring–early summer of 2019 and possible causes. J. Meteor. Res., 34(5), 997–1012, https://doi.org/10.1007/s13351-020-0032-8.
Dirmeyer, P. A., G. Balsamo, E. M. Blyth, R. Morrison, and H. M. Cooper, 2021: Land-atmosphere interactions exacerbated the drought and heatwave over northern Europe during summer 2018. AGU Advances, 2(2), e2020AV000283, https://doi.org/10.1029/2020AV000283.
Drusch, M., D. Vasiljevic, and P. Viterbo, 2004: ECMWF’s global snow analysis: Assessment and revision based on satellite observations. J. Appl. Meteorol., 43(9), 1282–1294, https://doi.org/10.1175/1520-0450(2004)043<1282:EGSAAA>2.0.CO;2.
Fan, X. W., C. Y. Miao, Q. Y. Duan, C. W. Shen, and Y. Wu, 2020: The performance of CMIP6 versus CMIP5 in simulating temperature extremes over the global land surface. J. Geophys. Res.: Atmos., 125, e2020JD033031, https://doi.org/10.1029/2020JD033031.
Fang, K. Y., and Coauthors, 2021: ENSO modulates wildfire activity in China. Nature Communications, 12, 1764, https://doi.org/10.1038/s41467-021-21988-6.
Feng, L., T. M. Li, and W. D. Yu, 2014: Cause of severe droughts in Southwest China during 1951–2010. Climate Dyn., 43(7–8), 2033–2042, https://doi.org/10.1007/s00382-013-2026-z.
Halder, S., S. K. Saha, P. A. Dirmeyer, T. N. Chase, and B. N. Goswami, 2016: Investigating the impact of land-use land-cover change on Indian summer monsoon daily rainfall and temperature during 1951–2005 using a regional climate model. Hydrology and Earth System Sciences, 20, 1765–1784, https://doi.org/10.5194/hess-20-1765-2016.
Hansen, J., M. Sato, R. Ruedy, K. Lo, D. W. Lea, and M. Medina-Elizade, 2006: Global temperature change. Proceedings of the National Academy of Sciences of the United States of America, 103(39), 14 288–14 293, https://doi.org/10.1073/pnas.0606291103. https://doi.org/10.1073/pnas.0606291103.
Hao, Z. C., A. AghaKouchak, and T. J. Phillips, 2013: Changes in concurrent monthly precipitation and temperature extremes. Environmental Research Letters, 8, 034014, https://doi.org/10.1088/1748-9326/8/3/034014.
Hirschi, M., and Coauthors, 2011: Observational evidence for soil-moisture impact on hot extremes in southeastern Europe. Nature Geoscience, 4, 17–21, https://doi.org/10.1038/ngeo1032.
Huang, B., and Coauthors, 2017: Extended reconstructed sea surface temperature, version 5 (ERSSTv5): Upgrades, validations, and intercomparisons. J. Climate, 30(20), 8179–8205, https://doi.org/10.1175/JCLI-D-16-0836.1.
Huang, R. H., Y. Liu, L. Wang, and L. Wang, 2012: Analyses of the causes of severe drought occurring in Southwest China from the fall of 2009 to the spring of 2010. Chinese Journal of Atmospheric Sciences, 36(3), 443–457, https://doi.org/10.3878/j.issn.1006-9895.2011.11101. (in Chinese with English abstract)
Jiang, L., Y. D. Chen, J. F. Li, and C. C. Liu, 2022: Amplification of soil moisture deficit and high temperature in a drought-heatwave co-occurrence in southwestern China. Natural Hazards, 111(1), 641–660, https://doi.org/10.1007/s11069-021-05071-3.
Ju, J., J. M. Lü, G. Q. Xie, and Z. Y. Huang, 2011: Studies on the influences of persistent anomalies of MJO and AO on drought appeared in Yunnan. Journal of Arid Meteorology, 29(4), 401–406, https://doi.org/10.3969/j.issn.1006-7639.2011.04.001. (in Chinese with English abstract)
Lee, J. Y., S. S. Lee, B. Wang, K. J. Ha, and J. G. Jhun, 2013: Seasonal prediction and predictability of the Asian winter temperature variability. Climate Dyn., 41, 573–587, https://doi.org/10.1007/s00382-012-1588-5.
Li, J., and B. Wang, 2018: Predictability of summer extreme precipitation days over eastern China. Climate Dyn., 51, 4543–4554, https://doi.org/10.1007/s00382-017-3848-x.
Li, J., Z. W. Zhu, and W. J. Dong, 2017a: Assessing the uncertainty of CESM-LE in simulating the trends of mean and extreme temperature and precipitation over China. International Journal of Climatology, 37, 2101–2110, https://doi.org/10.1002/joc.4837.
Li, S. F., A. C. Hughes, T. Su, J. L. Anberrée, A. A. Oskolski, M. Sun, D. K. Ferguson, and Z. K. Zhou, 2017b: Fire dynamics under monsoonal climate in Yunnan, SW China: Past, present and future. Palaeogeography, Palaeoclimatology, Palaeoecology, 465, 168–176, https://doi.org/10.1016/j.palaeo.2016.10.028.
Lindzen, R. S., and S. Nigam, 1987: On the role of sea surface temperature gradients in forcing low-level winds and convergence in the tropics. J. Atmos. Sci., 44(17), 2418–2436, https://doi.org/10.1175/1520-0469(1987)044<2418:OTROSS>2.0.CO;2.
Liu, Y., E. X. Zhao, G. F. Peng, and S. Q. Yang, 2008: Severe drought in the early summer of 2005 in Yunnan and middle-high latitudes circulation. Journal of Arid Meteorology, 25(1), 32–37. (in Chinese with English abstract)
Lu, E., Y. L. Luo, R. H. Zhang, Q. X. Wu, and L. P. Liu, 2011: Regional atmospheric anomalies responsible for the 2009–2010 severe drought in China. J. Geophys. Res.: Atmos., 116, D21114, https://doi.org/10.1029/2011JD015706.
Lu, R. Y., J. H. Oh, and B. J. Kim, 2002: A teleconnection pattern in upper-level meridional wind over the North African and Eurasian continent in summer. Tellus A, 54, 44–55, https://doi.org/10.3402/tellusa.v54i1.12122.
Lü, J. M., J. H. Ju, J. Z. Ren, and W. W. Gan, 2012: The influence of the Madden-Julian Oscillation activity anomalies on Yunnan’s extreme drought of 2009–2010. Science China Earth Sciences, 55, 98–112, https://doi.org/10.1007/s11430-011-4348-1.
Luo, N., Y. Guo, Z. B. Gao, K. X. Chen, and J. M. Chou, 2020: Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China. Atmospheric and Oceanic Science Letters, 13(6), 589–597, https://doi.org/10.1080/16742834.2020.1808430.
Ma, S. M., C. W. Zhu, and B. Q. Liu, 2021: Possible causes of persistently extreme-hot-days-related circulation anomalies in Yunnan from April to June 2019. Chinese Journal of Atmospheric Sciences, 45(1), 165–180, https://doi.org/10.3878/j.issn.1006-9895.2004.19226. (in Chinese with English abstract)
Marcott, S. A., J. D. Shakun, P. U. Clark, and A. C. Mix, 2013: A reconstruction of regional and global temperature for the past 11, 300 years. Science, 339(6124), 1198–1201, https://doi.org/10.1126/science.1228026.
Moberg, A., and Coauthors, 2006: Indices for daily temperature and precipitation extremes in Europe analyzed for the period 1901–2000. J. Geophys. Res.: Atmos., 111, D22106, https://doi.org/10.1029/2006JD007103.
Murphy, A. H., 1988: Skill scores based on the mean square error and their relationships to the correlation coefficient. Mon. Wea. Rev., 116(12), 2417–2424, https://doi.org/10.1175/1520-0493(1988)116<2417:SSBOTM>2.0.CO;2.
North, G. R., T. L. Bell, R. F. Cahalan, and F. J. Moeng, 1982: Sampling Errors in the Estimation of Empirical Orthogonal Functions. Mon. Mon. Wea. Rev., 110(7), 699–706, https://doi.org/10.1175/1520-0493(1982)110<0699:SEITEO>2.0.CO;2.
Orsolini, Y., and Coauthors, 2019: Evaluation of snow depth and snow cover over the Tibetan Plateau in global reanalyses using in situ and satellite remote sensing observations. The Cryosphere, 13(8), 2221–2239, https://doi.org/10.5194/tc-13-2221-2019.
Screen, J. A., C. Deser, and L. T. Sun, 2015: Projected changes in regional climate extremes arising from Arctic sea ice loss. Environmental Research Letters, 10(8), 084006, https://doi.org/10.1088/1748-9326/10/8/084006.
Sedlmeier, K., H. Feldmann, and G. Schädler, 2018: Compound summer temperature and precipitation extremes over central Europe. Theor. Appl. Climatol., 131, 1493–1501, https://doi.org/10.1007/s00704-017-2061-5.
Shi, H. Y., and J. Chen, 2018: Characteristics of climate change and its relationship with land use/cover change in Yunnan Province, China. International Journal of Climatology, 38(5), 2520–2537, https://doi.org/10.1002/joc.5404.
Shukla, S., M. Safeeq, A. AghaKouchak, K. Y. Guan, and C. Funk, 2015: Temperature impacts on the water year 2014 drought in California. Geophys. Res. Lett., 42(11), 4384–4393, https://doi.org/10.1002/2015GL063666.
Uppala, S. M., and Coauthors, 2005: The ERA-40 re-analysis. Quart. J. Roy. Meteor. Soc., 131, 2961–3012, https://doi.org/10.1256/qj.04.176.
Wang, B., B. Q. Xiang, J. Li, P. J. Webster, M. N. Rajeevan, J. Liu, and K. J. Ha, 2015: Rethinking Indian monsoon rainfall prediction in the context of recent global warming. Nature Communications, 6, 7154, https://doi.org/10.1038/ncomms8154.
Weisheimer, A., and Coauthors, 2009: ENSEMBLES: A new multi-model ensemble for seasonal-to-annual predictions: Skill and progress beyond DEMETER in forecasting tropical Pacific SSTs. Geophys. Res. Lett., 36(21), L21711, https://doi.org/10.1029/2009GL040896.
Wu, J., and X. J. Gao, 2013: A gridded daily observation dataset over China region and comparison with the other datasets. Chinese Journal of Geophysics, 56(4), 1102–1111, https://doi.org/10.6038/cjg20130406. (in Chinese with English abstract)
Wu, L. Y., and J. Y. Zhang, 2015: The relationship between spring soil moisture and summer hot extremes over North China. Adv. Atmos. Sci., 32, 1660–1668, https://doi.org/10.1007/s00376-015-5003-0.
Wu, Z. W., P. Zhang, H. Chen, and Y. Li, 2016: Can the Tibetan Plateau snow cover influence the interannual variations of Eurasian heat wave frequency? Climate Dyn., 46, 3405–3417, https://doi.org/10.1007/s00382-015-2775-y.
Xing, W., B. Wang, S.-Y. Yim, and K.-J. Ha, 2017: Predictable patterns of the May–June rainfall anomaly over East Asia. J. Geophys. Res.: Atmos., 122, 2203–2217, https://doi.org/10.1002/2016JD025856.
Xu, X., Y. G. Du, J. P. Tang, and Y. Wang, 2011: Variations of temperature and precipitation extremes in recent two decades over China. Atmospheric Research, 101(1–2), 143–154, https://doi.org/10.1016/j.atmosres.2011.02.003.
Xu, Z. X., X. J. Yang, D. P. Zuo, Q. Chu, and W. F. Liu, 2015: Spatiotemporal characteristics of extreme precipitation and temperature: A case study in Yunnan Province, China. Proceedings of IAHS, 369, 121–127, https://doi.org/10.5194/piahs-369-121-2015.
Yan, H. M., X. Duan, and J. G. Cheng, 2007: Study on a severe drought event over Yunnan in spring 2005. Journal of Tropical Meteorology, 23(3), 300–306, https://doi.org/10.3969/j.issn.1004-4965.2007.03.013. (in Chinese with English abstract)
Yan, Z. W., Y. H. Ding, P. M. Zhai, L. C. Song, L. J. Cao, and Z. Li, 2020: Re-assessing climatic warming in China since 1900. J. Meteor. Res., 34(2), 243–251, https://doi.org/10.1007/s13351-020-9839-6.
Yang, H., J. Song, H. M. Yan, and C. Y. Li, 2012a: Cause of the severe drought in Yunnan Province during winter of 2009 to 2010. Climatic and Environmental Research, 17(3), 315–326, https://doi.org/10.3878/j.issn.1006-9585.2011.10134. (in Chinese with English abstract)
Yang, J., D. Y. Gong, W. S. Wang, M. Hu, and R. Mao, 2012b: Extreme drought event of 2009/2010 over southwestern China. Meteorol. Atmos. Phys., 115, 173–184, https://doi.org/10.1007/s00703-011-0172-6.
Zhang, R. N., R. H. Zhang, and Z. Y. Zuo, 2017: Impact of Eurasian spring snow decrement on East Asian Summer precipitation. J. Climate, 30(9), 3421–3437, https://doi.org/10.1175/JCLI-D-16-0214.1.
Zhang, R. N., C. H. Sun, J. S. Zhu, R. H. Zhang, and W. J. Li, 2020: Increased European heat waves in recent decades in response to shrinking Arctic sea ice and Eurasian snow cover. NPJ Climate and Atmospheric Science, 3(1), 7, https://doi.org/10.1038/s41612-020-0110-8.
Zhou, Y. Q., and G. Y. Ren, 2011: Change in extreme temperature event frequency over mainland China, 1961–2008. Climate Research, 50(2–3), 125–139, https://doi.org/10.3354/cr01053.
Zhu, Z. W., R. Lu, S. S. Fu, and H. Chen, 2023: Alternation of the atmospheric teleconnections associated with the Northeast China spring rainfall during a recent 60-year period. Adv. Atmos. Sci., 40, 168–176, https://doi.org/10.1007/s00376-022-2024-3.
Zhu, Z. W., R. Lu, H. P. Yan, W. K. Li, T. M. Li, and J. H. He, 2020: Dynamic origin of the interannual variability of West China autumn rainfall. J. Climate, 33(22), 9643–9652, https://doi.org/10.1175/JCLI-D-20-0097.1.
Acknowledgements
This work was supported by the National Natural Science Foundation of China (Grant Nos. 42088101 and 42175033) and the High-Performance Computing Center of Nanjing University of Information Science & Technology.
Author information
Authors and Affiliations
Corresponding author
Additional information
Article Highlights
• EHDs in southwestern China appear mainly in April and May, which are connected with a local anomalous positive geopotential height.
• The Atlantic tripolar SST tendency and the central Asian snow depth anomalies are the two physical precursors of EHDs.
• The precursors could satisfactorily predict the EHDs during the independent prediction period.
Electronic Supplementary Material to
Rights and permissions
About this article
Cite this article
Zhou, Z., Li, J., Chen, H. et al. Seasonal Prediction of Extreme High-Temperature Days in Southwestern China Based on the Physical Precursors. Adv. Atmos. Sci. 40, 1212–1224 (2023). https://doi.org/10.1007/s00376-022-2075-5
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00376-022-2075-5