人民长江 ›› 2022, Vol. 53 ›› Issue (9): 56-63.doi: 10.16232/j.cnki.1001-4179.2022.09.010

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1960~2018年河南省旱涝特征及其气候背景分析

楚纯洁;周金风   

  • 发布日期:2022-10-20

Evolution features of drought-flood in Henan Province and their climatic background during 1960 to 2018

CHU Chunjie, ZHOU Jinfeng   

  • Published:2022-10-20

摘要: 为探究河南省旱涝变化规律及其气候驱动因子,利用1960~2018年河南省17个国家基准气象台站逐日降水、气温资料,采用降水和潜在蒸发均一化旱涝指标,对河南省旱涝特征及其气候背景进行分析。结果表明:(1)河南省在1990 s中期前后出现了旱涝趋势转换,不同季节均呈不同程度的干旱增多、覆盖面积增大的特点,而且除冬、夏季之外,其他季节均呈显著干旱化趋势,但所有季节这一趋势均会在未来持续增强。(2)在空间分布上整体呈现中西部干旱连片多发、豫中与豫南东部雨涝多发特点。(3)海温关键区Ni1o3.4区海表温度指数异常偏低尤其形成拉尼娜(La Ni1a)事件时易发生干旱,反之在形成厄尔尼诺(El Ni1o)事件时易发生雨涝,旱涝发生对El Ni1o/La Ni1a事件具有明显的滞后响应及季节性变化。东部型El Ni1o/La Ni1a事件与中部型La Ni1a事件均对季节性旱涝存在显著差异性影响,而不同等级El Ni1a/La Ni1a事件对旱涝的影响没有明显差异。(4)太阳黑子极小值年m、m-1年及极大值年+1(M+1年)易发生雨涝与极端雨涝,而M年、M-1及m+1年易发生干旱与极端干旱,且m年、m-1年及M+1年发生雨涝的频率范围明显高于M年、M-1年,而M年、M-1年及m+1年发生干旱的频率范围明显高于m年及m-1年。(5)河南省旱涝演变对海表温度距平与太阳黑子活动具有阶段性的周期性响应,且具有明显的滞后性。研究成果可为河南省防洪抗旱工作提供参考。

关键词: 旱涝演变;气候变化;El Ni1o/La Ni1a事件;太阳黑子;河南省;

Abstract: In order to explore the variation law of drought-flood in Henan Province and its driving factors, based on the daily precipitation and temperature data of 17 national meteorological stations during 1960 to 2018, evolution features of drought-flood and their climatic background in Henan Province were analyzed by using homogenized drought-flood index (DFI) of precipitation and potential evaporation. The results showed that: ① The trend of drought and flood in Henan Province changed reversely around the mid-1990s, showing characteristics of increasing drought times and coverage in different degrees in all seasons. Moreover, except winter and summer, other seasons showed a significant drought trend. This trend would continue to increase in all seasons in the future. ② On the whole, the spatial distribution showed characteristics of drought in central and western regions, flood in central and east of southern Henan. ③When the Sea Surface Temperature (SST) in Ni?o3.4 area was abnormally low, especially in formation of La Ni?a event, it was prone to drought, on the contrary El Ni?o event was prone to flood. Drought and flood had obvious lag response and seasonal changes to El Ni?o / La Ni?a events. The eastern type of El Ni?o / La Ni?a events and central type of La Ni?a events had a prominent impact on drought and flood, however El Ni?o / La Ni?a events of different grades had not significant influence on drought and flood. ④ Flood and extreme flood were prone to occur in sunspot m, m-1 and M+1 years (m is the minimum year, M is the maximum year), while drought and extreme drought were prone to occur in M, M-1 and m+1 years. Moreover, the frequency range of flood in sunspot m, m-1 and M+1 years was significantly higher than that in M and M-1 years, while the frequency range of drought in M, M-1 and m+1 years was significantly higher than that in m and m-1 years. ⑤The evolution of drought and flood in Henan Province had periodic response to Sea Surface Temperature Anomaly (SSTA) and sunspot activity, and had obvious hysteresis. The research results can provide reference for flood control and drought resistance work in Henan Province.

Key words: drought-flood evolution; climate change; El Ni?o / La Ni?a events; sunspot; Henan Province