气候与水文

贺兰山银川段不同重现期山洪灾害风险与影响区划研究

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  • 1 宁夏气象防灾减灾重点实验室,宁夏 银川 750002;
    2 宁夏气候中心,宁夏 银川 750002;
    3 宁夏气象灾害防御技术中心,宁夏 银川 750002
崔洋(1982–),男,宁夏吴忠人,正研级高工,主要从事气候变化、生态环境变化、数值模拟研究. E-mail:cuiyang@cma.gov.cn

收稿日期: 2019-10-01

  修回日期: 2020-02-29

  网络出版日期: 2020-11-18

基金资助

宁夏自然科学基金项目(2020AAC03465); 宁夏自治区青年拔尖人才培养专项(RQ0022); 宁夏气象局气象科技创新领军人才专项资助

Risk and impact zoning of different return period flash flood disasters in Yinchuan Section of Helan Mountain

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  • 1 Key Laboratory of Meteorological Disaster Preventing and Reducing in Ningxia,Yinchuan 750002,Ningxia,China;
    2 Ningxia Climate Center,Yinchuan 750002,Ningxia,China;
    3 Ningxia Meteorological Disaster Prevention Technology Center,Yinchuan 750002,Ningxia,China

Received date: 2019-10-01

  Revised date: 2020-02-29

  Online published: 2020-11-18

摘要

为评估贺兰山银川段山洪灾害风险程度及其影响,利用高分辨率数字高程模型(DEM)、行政区划、水系和自动气象站历史降水数据,以及居民点、学校、桥梁等社会经济信息资料,采用FloodArea模型模拟与ArcGIS空间叠加统计分析相结合的方法,分析研究了贺兰山银川段不同重现期山洪灾害风险分布特征,及其对人口、土地利用和国内生产总值(GDP)的影响。结果表明:(1)贺兰山银川段10~100 a一遇山洪灾害低、中、高风险区面积分别为109.5~276.3 km2、45.0~231.0 km2、13.4~204.3 km2,同一风险等级的山洪灾害区划面积随着重现期增大呈显著增大趋势。(2)贺兰山10 a和20 a一遇山洪灾害风险区主要位于海拔1 130~1 450 m的山洪沟及其两侧区域,50 a一遇山洪灾害风险区主要集中在山洪沟下游和山前海拔1 130~1 180 m的冲击扇区,100 a一遇山洪灾害风险区覆盖整个山前海拔1 120~1 350 m的区域和冲击扇区。随着重现期增大,贺兰山山洪灾害风险区具有向上游(下游)区域扩展较慢(更快)的显著特征。(3)银川市受贺兰山10 a、20 a、50 a和100 a一遇山洪灾害影响总人口分别为7.30×104人、9.87×104人、1.65×105人和2.39×105人。随着山洪重现期增大,受灾害影响总人口呈显著增加趋势,低、中、高风险区受影响人口增速分别在-12.4%~20.5%、 48.6%~91.8%、163%~300%之间。(4)农田、草地受贺兰山山洪灾害影响最大,二者合计占受影响土地总面积的比例在82.1%~86.9%之间;其次是建设用地和耕地,两者占受影响土地总面积的比例在4.4%~9.1%和1.1%~4.6%之间,是银川市贺兰山山洪灾害防御的重点区域。(5)银川市受贺兰山10 a、20 a、50 a、100 a一遇山洪灾害中、高风险区影响的GDP合计分别为1.12×109元、2.00×109元、4.70×109元、8.74×109元;发生超50 a一遇山洪灾害时,沿山农业和工业产业、基础公共设施等会遭受较大经济损失。

本文引用格式

崔洋, 常倬林, 左河疆, 王建英 . 贺兰山银川段不同重现期山洪灾害风险与影响区划研究[J]. 干旱区地理, 2020 , 43(4) : 859 -870 . DOI: 10.12118/j.issn.1000-6060.2020.04.01

Abstract

In order to assess the impacts and risks associated with flash flood disasters in the Yinchuan section of the Helan Mountain,Ningxia Province,China,we considered a high-resolution digital elevation model (DEM),as well as information on the administrative divisions,the distribution of torrents,the historical precipitation data from automatic weather stations,and socioeconomic information (e.g., on residential areas,schools,and bridges). The risk distribution characteristics of flash flood disasters over the Yinchuan section of the Helan Mountain and their impact on the population,land use,and gross domestic product (GDP) were analyzed and assessed by a FloodArea model simulation and an ArcGIS spatial overlay statistical analysis. The results showed the following:(1) The areas subjected to a low,medium,and high risk of flash flood disasters with a return period of 10-100 a were of 109.5-276.3 km2,45.0-231.0 km2,and 13.4-204.3 km2,respectively; moreover,the zoning areas of flash flood disasters with the same risk level showed a significant increase with the lengthening of the return period. (2) The areas of the Helan Mountain subjected to the risk of flash flood disasters with return periods of 10 a and 20 a were mainly located in correspondence and on the sides of flood ditches (at altitudes of 1 130-1 450 m); moreover,those subjected to the risk of flash flood disasters with return periods of 50 a were mainly located downstream of the flood ditches and in correspondence of an impact fan along the mountain front (at altitudes of 1 130-1 180 m). The areas at risk of flash flood disasters with return periods of 100 a were located at altitudes of 1 120-1 350 m and in correspondence of the impact fan along the mountain front. Overall,with the increase of the return period,the zones of the Helan Mountain at risk of flash flood disasters showed a significant slow (fast) expansion toward the upstream (downstream) area. (3) In Yinchuan City,~73 000,98 700,165 300,and 239 000 people will be affected by flash flood disasters with return periods of 10 a,20 a,50 a,and 100 a,respectively. With the increase of the return period of flash flood disasters,the number of people affected by them and living around the Helan Mountain grew significantly (growth rates: -12.4% to 20.5%,48.6% to 91.8%,and 163% to 300% in the low,medium,and high risk areas,respectively). (4) Farmlands and grasslands were the most affected by flash flood disasters that originated on the Helan Mountain: together,they accounted for 82.1%-86.9% of the total affected area. They were followed by construction and cultivated lands,which accounted for 4.4%-9.1% and 1.1%-4.6% of the total affected area,respectively. These lands are key for the prevention of flash flood disasters (originated on the Helan Mountain) in Yinchuan City. (5) In Yinchuan City,the total GDP was affected by flash flood disasters with return periods of 10 a,20 a,50 a,and 100 a that occurred in medium- and high-risk areas. The GDP losses corresponded to 1.12 billion,2.00 billion,4.70 billion,and 8.74 billion yuan,respectively. In case of flash flood disasters with return periods>50 a,the agricultural/industrial industries,infrastructures,and public facilities located in Yinchuan City (close to the mountain) will suffer great economic losses.

参考文献

[1] 唐邦兴,崔鹏. 山洪泥石流滑坡灾害及防治[M]. 北京:科学出版社,1994:1–10.
[TANG Bangxing,CUI Peng.Debris flow and slide hazards and countermeasures[M]. Beijing:Science Press,1994:1–10.]
[2] 赵士鹏. 中国山洪灾害系统的整体特征及其危险度区划的初步研究[J].自然灾害学报,1996,5(3):93–99.
[ZHAO Shipeng.An elementary study on whole characteristics of mountain torrents disaster system in China and its hazard regionalization[J]. Journal of Natural Disasters,1996, 5(3):93–99.]
[3] 赵士鹏. 基于GIS 的山洪灾情评估方法研究[J]. 地理学报,1996,51(5):471–479.
[ZHAO Shipeng.An integration of GIS and analytical models for evaluation of disasters caused by mountain torrents[J]. Acta Geographica Sinica,1996,51(5):471–479.]
[4] 张平仓,任洪玉,胡维忠,等. 中国山洪灾害防治区划初探[J].水土保持学,2006,20(6):196–200.
[ZHANG Pingcang,REN Hongyu,HU Weizhong,et al.An elementary study on Chinese mountain torrents disaster prevention regionalization[J]. Journal of Soil and Water Conservation,2006,20(6): 196–200.]
[5] 孙东亚,张红萍. 欧美山洪灾害防治研究进展及实践[J]. 中国水利,2012,12(23):16–17.
[SUN Dongya, ZHANG Hongping.Research progress and practice of flash flood prevention in Europe and America[J]. China Water Resources,2012,12(23):16–17.]
[6] 国家防汛抗旱总指挥部办公室. 全国山洪灾害防治项目实施方案(2016—2020)编制大纲[R]. 2015.
[State Flood Control and Drought Prevention Office. Outline for the implementation plan of national mountain torrent disaster prevention project(2016–2020)[R]. 2015.]
[7] 张红萍. 山区小流域洪水风险评估与预警技术研究[D]. 北京:中国水利水电科学研究院,2013.
[ZHANG Hongping.Study on the flood risk management and technology of the small mountain watershed[D]. Beijing:China Institute of Water Resource and Hydro-power Research, 2013.]
[8] RICHARDS B D.洪水的估算与控制[M]. 北京:水利电力出版社,1958.
[RICHARDS B D.Flood estimation and control[M].Beijing:China Water & Power Press,1958.]
[9] ELDEEN M.Predisaster physical planning:Integration of disaster risk analysis into physical planning:A case[J]. Disasters,1980,4(2):211–222.
[10] WIECZOREK G F.Evaluating danger landslide catalogue map[J]. Bulletin of the Association of Engineering Geologists,1984,1(1):337–342.
[11] ELLEN S D,WIECZOREK G F. Landslides,floods,and marine effects of the storm of January 3–5,1982,in the San Francisco Bay region,California[R]. Geological Survey(US),1988.
[12] GUZZETTI F,STARK C P,SALVATI P.Evaluation of flood and landslide risk to the population of Italy[J]. Environmental Management,2005,36(1):15–36.
[13] CAPELLO M,CUTRONEO L,FERRETTI G,et al.Changes in the physical characteristics of the water column at the mouth of a torrent during an extreme rainfall event[J]. Journal of Hydrology,2016,541(12):146–157.
[14] 赵士鹏. 山洪灾情评估的系统集成方法研究[D]. 北京:中国科学院地理研究所,1995.
[ZHAO Shipeng.Studies on system integration method for assessment of disasters caused by mountain torrents[D]. Beijing:Institute of Geographic Sciences and Natural Resources Research, CAS,1995.]
[15] 姜付仁,向立云. 洪水风险区划方法与典型流域洪水风险区划实例[J]. 水利发展研究. 2002,2(7):27–30.
[JIANG Furen,XIANG Liyun.Zonation methodology of flood risk and its case study for typical basin[J]. Water Resources Development Research,2002,2(7):27–30.]
[16] 王劲峰. 中国自然灾害区划—灾害区划、影响评价、减灾对策[M]. 北京:中国科学技术出版社,1995.
[WANG Jingfeng.China natural disaster zoning-disaster zoning,impact assessment, disaster mitigation countermeasures[M].Beijing: China Science and Technology Press,1995.]
[17] 张行南,罗健,陈雷,等. 中国洪水灾害危险程度区划[J]. 水利学报,2000,31(3):1–7.
[ZHANG Xingnan,LUO Jian,CHEN Lei,et al.Zoning of Chinese flood hazard risk[J]. Journal of Hydraulic Engineering,2000, 31(3):1–7.]
[18] 谭徐明,张伟兵,马建明,等. 全国区域洪水风险评价与区划图绘制研究[J]. 中国水利水电科学研究院学报,2004,2(1):50–60.
[TAN Xuming,ZHANG Weibin,MA Jianming,et al.Research on regional assessment of flood risk and regionalization mapping in China[J]. Journal of China Institute of Water Resources and Hydropower Research,2004,2(1):50–60.]
[19] 田丰,张军,冉有华,等. 不同空间尺度的山洪灾害风险评价模型对比研究[J].干旱区地理,2019,42(3) 559–569.
[TIAN Feng,ZHANG Jun,RAN Youhua,et al.Model comparison of mountain torrent disaster risk assessment in different spatial scale[J]. Arid Land Geography,2019,42(3):559–569.]
[20] 杜俊,任洪玉,林庆明,等. 山洪灾害防御研究进展[J]. 灾害学,2019,34(2):161–167.
[DU Jun,REN Hongyu,LIN Qingming,et al.Research progress on the prevention of flash flood Disasters[J]. Journal of Catastrophology,2019,34(2):161–167.]
[21] 刘少军,张京红,张明洁,等. 海南岛山洪灾害风险区划研究[J]. 水土保持研究,2013,20(5):165–169.
[LIU Shaojun,ZHANG Jinghong,ZHANG Mingjie,et al.Research on risk zonation of mountain torrent disasters in Hainan island[J]. Research of Soil and Water Conservation,2013,20(5):165–169.]
[22] 宫清华,黄光庆,郭敏,等. 基于GIS技术的广东省洪涝灾害风险区划[J].自然灾害学报,2009,18(1): 58–63.
[GONG Qinghua,HUANG Guangqing,GUO Min,et al.GIS-based risk zoning of flood hazard in Guangdong Province[J]. Journal of Natural Disasters,2009,18(1):58–63.]
[23] 岳琦,张林波,刘成程,等. 基于GIS的福建闽江上游山洪灾害风险区划[J]. 环境工程技术学报. 2015,5(4):293–298.
[YUE Qi,ZHANG Linbo,LIU Chengcheng,et al.GIS-based risk zoning of flood disasters in upstream of the Minjiang River[J]. Journal of Environmental Engineering Technology,2015,5(4):293–298.]
[24] 唐川,朱静. 基于GIS的山洪灾害风险区划[J]. 地理学报,2005,60(1):87–94.
[TANG Chuan,ZHU Jing.A GIS based regional torrent risk zonation[J]. Acta Geographica Sinica,2005,60(1):87–94.]
[25] 丁文峰,杜俊,陈小平,等. 四川省山洪灾害风险评估与区划[J].长江科学院院报,2015,32(12):41–45.
[DING Wenfeng,DU Jun,CHEN Xiaoping,et al.Risk assessment and regionalization of mountain torrent disaster in Sichuan Province[J]. Journal of Yangtze River Scientific Research Institute,2015,32(12):41–45.]
[26] 邹朝望,孙媛媛,谢伯承. 湖南省洪涝灾害风险评估研究[J]. 人民长江,2010,41(11):63–65.
[ZOU Chaowang,SUN Yuanyuan,XIE Bocheng.Study on risk evaluation of flood disaster in Hunan Province[J]. Yangtze River,2010,41(11):63–65.]
[27] 刘敏,杨宏青,向玉春. 湖北省雨涝灾害的风险评估与区划[J].长江流域资源与环境,2002,11(5):476–481.
[LIU Min,YANG Hongqing,XIANG Yuchun.Risk assessment and regionalization of waterlogging disasters in Hubei Province[J]. Resources and Environment in the Yangtze Basin,2002,11(5):476–481.]
[28] 管岷,陈兴旺. 江西省山洪灾害风险区划初步研究[J]. 暴雨灾害,2007,26(4):339–343.
[GUAN Min,CHEN Xingwang.Research of regional torrent risk zonation in Jiangxi Province[J].Torrential Rain and Disasters,2007,26(4):339–343.]
[29] 谢五三,田红,卢燕宇. 基于FloodArea模型的大通河流域暴雨洪涝灾害风险评估[J]. 暴雨灾害,2015,34(4):384–387.
[XIE Wusan,TIAN Hong,LU Yanyu.Risk evaluation of rainstorm and flood disasters in Datong River basin based on the FloodArea model[J]. Torrential Rain and Disasters,2015,34(4):384–387.]
[30] 王胜,吴蓉,谢五三,等. 基于Floodarea的山洪灾害风险区划研究——以淠河流域为例[J]. 气候变化研究进展,2016,12(5):432–441.
[WANG Sheng,WU Rong,XIE Wusan,et al.Rainstrom-induced mountain flood disaster risk zoning based on FloodArea inundation model:Taking Pihe River valley as a case[J].Climate Change Research,2016,12(5):432–441.]
[31] 曹罗丹,李加林. 基于遥感与GIS 的浙江省洪涝灾害综合风险评估研究[J].自然灾害学报,2015,24(4):111–119.
[CAO Luodan,LI Jialin.Integrated risk assessment of flood disaster in Zhejiang Province based on RS and GIS[J]. Journal of Natural Disasters,2015,24(4):111–119.]
[32] 张洪玲,宋丽华,刘赫男,等. 黑龙江省暴雨洪涝灾害风险区划[J].中国农业气象,2012,33(4):623–629.
[ZHANG Hongling,SONG Lihua,LIU Henan,et al.Risk zoning of flood and waterlog in Heilongjiang Province[J]. Chinese Journal of Agrometeorology,2012,33(4):623–629.]
[33] 周金星. 山洪及泥石流灾害空间预报技术研究[J]. 水土保持学报,2001,15(2):112–116.
[ZHOU Jinxing.Technique of space prediction on flush flood and debris flow disaster[J]. Journal of Soil and Water Conservation,2001,15(2):112–116.]
[34] 张世才,褚建华,张同泽. 祁连山区山洪灾害临界雨量计算和风险区划分[J]. 水土保持学报,2007,21(5):196–200.
[ZHANG Shicai,CHU Jianhua,ZHANG Tongze.Calculation of critical rainfall amounts and risk area partition of flood disaster in Qilian mountain area[J]. Journal of soil and Water Conservation,2007,21(5):196–200.]
[35] 李永红. 基于ArcGIS的陕西山洪灾害易发程度区划[J]. 灾害学,2008,23(1):37–42.
[LI Yonghong.Susceptible degree zoning of mountain torrent disasters in Shaanxi based on ArcGIS[J].Journal of Catasirophology,2008,23(1):37–42.]
[36] GEMMER M.Decision support for flood risk management at the Yangtze River by GIS/RS based flood damage estimation[M]. Giessen:Shaker,2004:108–127.
[37] GEOMER G H.Floodarea-ArcGIS extension for calculating flooded areas(User mannual Version 9.5)[M]. Heidelberg:Geomer,2008.
[38] 苏布达,姜彤,郭业友,等. 基于GIS栅格数据的洪水风险动态模拟及应用[J]. 河海大学学报(自然科学版),2005,33(4):370–374.
[SU Buda,JIANG Tong,GUO Yeyou,et al.GIS raster data-based dynamic flood risk simulation model and its application[J]. Journal of Hohai University(Natural Sciences),2005,33(4):370–374.]
[39] GEOMER. Floodarea-Arcview extension for calculating flooded areas(User manual Version 2.4)[M]. Heidelberg:Heidelberg University,2003.
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