1960—2013年昭通市极端降雨时空演变规律研究

李绅东, 马燕, 孙光宝, 罗文兵, 贾韬

长江科学院院报 ›› 2018, Vol. 35 ›› Issue (7) : 19-24.

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长江科学院院报 ›› 2018, Vol. 35 ›› Issue (7) : 19-24. DOI: 10.11988/ckyyb.20171231
水资源与环境

1960—2013年昭通市极端降雨时空演变规律研究

  • 李绅东1, 马燕1, 孙光宝2, 罗文兵3, 贾韬1
作者信息 +

Spatio-temporal Variations of Extreme Rainfall in Zhaotong from 1960 to 2013

  • LI Shen-dong1, MA Yan1, SUN Guang-bao2, LUO Wen-bing3, JIA Tao1
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摘要

气候变化引起的极端降雨量级和频次变化已经引起了广泛的关注,极端降雨演变规律的研究对于区域防洪减灾和水资源管理具有重要意义。基于昭通市及其周边的16个气象站点1960—2013年共54 a的降雨数据,选取世界气象组织推荐的6个极端降雨指数,采用线性趋势分析、Mann-Kendll法和滑动T检验等方法分析了昭通市的极端降雨时间演变规律,并基于ArcGIS10.2采用反距离插值法(IDW)分析了昭通市极端降雨指数的空间分布格局。结果表明:在趋势演变方面,昭通市的总降雨量PRCPTOT有下降趋势;而反映极端降雨量级的3项指数SDII,RX5day,R95p均呈上升趋势,其中RX5day上升趋势显著;而R10mm和CWD这2项反映极端降雨频率的指数均呈下降趋势,其中R10mm下降趋势显著。在空间分布方面,昭通市6项极端降雨指数具有较高的空间异质性,东北部降雨量级和频率较高,中部趋缓,而西南部总体上相对较低。相关分析的结果表明昭通地区极端降雨指数与高程呈现负相关关系,极端降雨主要发生在低海拔地区。研究成果有助于加深对该区域极端降雨发生规律的认识,为区域防洪减灾和水资源管理提供参考。

Abstract

Changes in the magnitude and frequency of extreme rainfall caused by climate change have attracted wide attention around the world. Researching the evolution law of extreme rainfall is of great significance for regional flood control and water resources management. According to rainfall data in 54 years (1960-2013) at 16 meteorological stations in Zhaotong, Yunnan Province and its surrounding areas, we analyzed the spatial evolution of six extreme rainfall indicators recommended by the World Meteorological Organization by linear trend analysis, Mann-Kendall method, and moving-t test, and the spatial distribution pattern by inverse distance interpolation method based on ArcGIS10.2. Results manifest that total rainfall volume indicator PRCPTOT presented a downward trend; three indices reflecting the magnitude of extreme rainfall, namely, SDII, RX5day, and R95p, displayed increasing trends, among which RX5day increased significantly; R10mm and CWD, which reflect the frequency of extreme rainfall, both showed decreasing trends, of which R10mm decreased apparently in particular. In terms of spatial distribution, the six indicators are of high spatial heterogeneity: the magnitude and frequency of rainfall were high in northeast Zhaotong, but alleviated in central Zhaotong, and relatively low in the southwest. In addition, extreme rainfall indicators were negatively correlated with elevation: extreme rainfall mainly happened in area of low altitude.

关键词

气候变化 / 极端降雨 / 时空演变 / 极端降雨指数 / 相关性 / 昭通市

Key words

climate change / extreme rainfall / spatio-temporal variation / extreme precipitation indices / correlation / Zhaotong City

引用本文

导出引用
李绅东, 马燕, 孙光宝, 罗文兵, 贾韬. 1960—2013年昭通市极端降雨时空演变规律研究[J]. 长江科学院院报. 2018, 35(7): 19-24 https://doi.org/10.11988/ckyyb.20171231
LI Shen-dong, MA Yan, SUN Guang-bao, LUO Wen-bing, JIA Tao. Spatio-temporal Variations of Extreme Rainfall in Zhaotong from 1960 to 2013[J]. Journal of Changjiang River Scientific Research Institute. 2018, 35(7): 19-24 https://doi.org/10.11988/ckyyb.20171231
中图分类号: P333.2   

参考文献

[1] 张建云,王银堂,贺瑞敏,等. 中国城市洪涝问题及成因分析[J]. 水科学进展,2016,27(4):485-491.
[2] 韩会庆,苏志华,张娇艳,等.1960—2013年贵州省强降水天数时空变化特征[J].长江科学院院报,2017,34 (11): 1-5.
[3] 宋 扬,周维博,马亚鑫,等.50年来灞河流域降水变化特征分析[J].长江科学院院报,2017,34(7):12-18.
[4] 黄 强, 陈子燊. 全球变暖背景下珠江流域极端气温与降水事件时空变化的区域研究[J]. 地球科学进展, 2014, 29(8):956-967.
[5] 翟盘茂,潘晓华.中国北方近50年温度和降水极端事件变化[J].地理学报,2003,58(增):1-10.
[6] QU B, LV A, JIA S, et al. Daily Precipitation Changes over Large River Basins in China, 1960-2013[J]. Water, 2016, 8(5):185.
[7] CHEN F, CHEN H, YANG Y. Annual and Seasonal Changes in Means and Extreme Events of Precipitation and Their Connection to Elevation over Yunnan Province, China[J]. Quaternary International, 2015, 374(1):46-61.
[8] WANG Y, XU Y, LEI C, et al. Spatio-temporal Characteristics of Precipitation and Dryness/Wetness in Yangtze River Delta, Eastern China, During 1960-2012[J]. Atmospheric Research, 2016, 172/173:196-205.
[9] 刘 琳,徐宗学. 西南5省市极端气候指数时空分布规律研究[J]. 长江流域资源与环境,2014,23(2):294-301.
[10]罗奕群. 昭通市暴雨特性分析[J]. 水资源研究,2011,32(3):13-14.
[11]舒远华. 云南昭通市暴雨洪水特性分析[J]. 人民长江,2012,(增2):51-52.
[12]雷 云. 昭通市滑坡泥石流预警系统减灾效益分析[J]. 中国水利, 2009, 40(21):59-61.
[13]李绅东. 云南省昭通市多尺度极端降水时空特征分析[J]. 长江科学院院报,2016,33(11):127-132.
[14]ZHANG X, ALEXANDER L, HEGERL G C, et al. Indices for Monitoring Changes in Extremes Based on Daily Temperature and Precipitation Data[J]. Wiley Interdisciplinary Reviews Climate Change, 2011, 2(6):851-870.
[15]栗忠魁, 胡卓玮, 魏 铼,等. 1951—2013年华北地区极端降水事件的变化[J]. 遥感技术与应用, 2016, 31(4):773-783.
[16]STORCH H V, NAVARRA A. Analysis of Climate Variability: Applications of Statistical Techniques[M]∥ Analysis of Climate Variability. Heidelberg: Springer, 1995:11-26.
[17]佘敦先, 夏 军, 张永勇,等. 近50年来淮河流域极端降水的时空变化及统计特征[J]. 地理学报, 2011, 66(9):1200-1210.
[18]ZHANG K, PAN S, CAO L, et al. Spatial Distribution and Temporal Trends in Precipitation Extremes over the Hengduan Mountains Region, China, from 1961 to 2012[J]. Quaternary International, 2014, 349:346-356.
[19]LIU W, ZHANG M, WANG S, et al. Changes in Precipitation Extremes over Shaanxi Province, Northwestern China, During 1960-2011[J]. Quaternary International, 2013, 313/314(10):118-129.

基金

国家自然科学基金项目(51509010);中央级公益性科研院所基本科研业务费项目(CKSF2016028/NS);湖北省自然科学基金项目(2016CFB606)

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