Var iation Tr ends and Multi- scale Analysis of Flood Affected Area in Var ious Regions of Xinjiang

Expand
  • 1. Xinjiang Meteorological Information Centre, Urumqi 830002, China;
    2. Institute of Desert Meteorology, CMA, Urumqi 830002, China;
    3. Xinjiang Climate Center, Urumqi 830002, China

Received date: 2008-01-15

  Revised date: 2008-03-06

  Online published: 2008-07-25

Supported by

Foundation of Desert Meteorology, CMA, No.sqj2005004; National Natural Science Foundation of China, No.40475041

Abstract

In this paper, we selected and used 2038 flood disaster data from 84 counties of Xinjiang in 1950-2006, and adopted the gray relational evaluation model, taking county as a unit, to divide Xinjiang into heavy flood disaster subregion, secondary heavy flood disaster subregion, general flood disaster subregion, light disaster flood subregion and tiny flood subregion. We also adopted autoregression moving average model ARMA(p, q) and second order principal value function to analyze long-term trend of disaster affected area, as well as its oscillation cycle with Morlet wavelet. Results show that the flood affected area throughout the region and every subregion had a changing cycle of 12-15a, the flood frequent oscillation cycle was on interdecadal and interannual scale of climatic background after the 1980s, and the superposition of small oscillation cycle as 7-8a and 2-3a was comparatively frequent. In terms of the flood disaster variation trend of Xinjiang, the outlook is not optimistic for the general flood affected area presented a distinct increasing trend and each flood subregion was in the climatic background with frequent period of flood at present. The distributing trend of flood disaster affected area and the oscillation cycle in the north and south piedmonts of the Tianshan Mountains played a decisive role relating to the interannual long-term trend and its oscillation cycle in the flood affected area in Xinjiang. These regions were the keys in reinforcing facilities and strength for flood prevention and control. Otherwise, the general flood affected area would have a greater impact on the flooded area of entire Xinjiang, leading to an increasing trend in the future regardless of the short, medium or long period changes, hence great attention should be aroused.

Cite this article

WANG Qiuxiang, CUI Caixia, YAO Yanli . Var iation Tr ends and Multi- scale Analysis of Flood Affected Area in Var ious Regions of Xinjiang[J]. Acta Geographica Sinica, 2008 , 63(7) : 769 -779 . DOI: 10.11821/xb200807011

References


[1] Wen Shu, Chen Ping, Da Qingli. Prediction and analysis for the disaster area caused by flood and waterlogging in our country. Journal of Biomathematics, 2000, 15(4): 452-456.
[温书, 陈平, 达庆利. 我国洪涝灾害受灾及成灾面积的预 测分析. 生物数学学报, 2000, 15(4): 452-456.]

[2] Zhao Jing, Xu Jianhua. Study on fractal characteristics of inundated area of flood disaster in China from 1950 to 1997. Journal of Natural Disasters, 2003, 12(1): 31-35.
[赵晶, 徐建华. 1950-1997 年我国洪涝灾害成灾面积的分形特征研究. 自然灾害学报, 2003, 12(1): 31-35.]

[3] Jiang Fengqing, Zhu Cheng, Hu Ruji. Statistics and fractal features of the flood and drought disasters in Xinjiang from 1950 to 1997. Journal of Natural Disasters, 2002, 11(4): 96-100.
[姜逢清, 朱诚, 胡汝骥. 新疆1950-1997 年洪涝灾害 的统计与分形特征分析. 自然灾害学报, 2002, 11(4): 96-100.]

[4] Zhu Xiaohua. The research on characteristics of flood from 1840 to 1996 in China. Journal of Catastrophology, 1999, 14 (2): 7-17.
[朱晓华. 中国1840-1996 年洪水灾害若干特征分析灾害学, 1999, 14(2): 7-17.]

[5] Liu Huishan, Lin Zhenshan, Zhang Mingyang. Wavelet analysis of area affected by flood disaster in China after 1949. Scientia Geographica Sinica, 2005, 25(1): 43-48.
[刘会山, 林振山, 张明阳. 建国以来中国洪涝灾害成灾面积变化的小 波分析. 地理科学, 2005, 25(1): 43-48.]

[6] Jiang Fengqing, Zhu Cheng, Mu Guijin. Recent magnification of flood and drought calamities in Xinjiang: An analysis of anthropogenetic effects. Scientia Geographica Sinica, 2002, 57(1): 57-65.
[姜逢清, 朱诚, 穆桂金. 当代新疆洪旱扩大 化: 人类活动的影响分析. 地理学报, 2002, 57(1): 57-65.]

[7] Jiang Fengqing, Hu Ruji. Climatic change and flood & drought disasters in Xinjiang during recent 50 years. Journal of Desert Research, 2004, 24(1): 35-40.
[姜逢清, 胡汝骥. 近50 年来新疆气候变化与洪旱灾害扩大化. 中国沙漠, 2004, 24(1): 35-40.]

[8] Wu Sufen, Zhang Guowei. Preliminary approach on the floods and their calamity changing tendency in Xinjiang region. Journal of Glaciology and Geocryology, 2003, 25(3): 342-346.
[吴素芬, 张国威. 新疆河流洪水与洪灾的变化趋势. 冰 川冻土, 2003, 25(2): 199-203.]

[9] Li Yan. Change of river flood and disaster in Xinjiang during past 40 years. Journal of Glaciology and Geocryology, 2003, 25(3): 342-346.
[李燕. 近40 年新疆河流洪水变化. 冰川冻土, 2003, 25(3): 342-346.]

[10] Dong Wenyu, Hu Jiang, Yang Shengfa. Genesis and characteristic analysis of flood in Xinjiang province. Journal of Chongqing Jiaotong University, 2004, 23(2): 118-122.
[董文玉, 胡江, 杨胜发. 新疆洪水成因及特性分析. 重庆交通 学院学报, 2004, 23(2): 118-122.]

[11] Chen Yaning, Yang Siquan. The application and model of grey association for evaluation of natural disaster. Progress in Geography, 1999, 18(2): 158-162.
[陈亚宁, 杨思全. 自然灾害的灰色关联灾情评估模型及应用研究. 地理科学进 展, 1999, 18(2): 158-162.]

[12] Qiu Yuanyao. Resplendence in Xinjiang for 50 Years. Urumqi: Xinjiang People's Press, 1999. 142-143.
[丘远尧. 新疆 辉煌50 年. 乌鲁木齐: 新疆人民出版社, 1999. 142-143.]

[13] Xinjiang Statistical Bureau. Xinjiang Statistical Yearbook 2006. Urumqi: Xinjiang People's Press, 2006. 185-186.
[新疆 统计局. 新疆统计年鉴(2006 年). 乌鲁木齐: 新疆人民出版社, 2006. 185-186.]

[14] Huang Jiayou. Methods of Meteorological Satistics, Analysis and Forecast. Beijing: China Meteorological Press, 2000 (2nd edn.). 48-52.
[黄嘉佑. 气象统计分析与预报方法. 北京: 气象出版社, 2000(第2 版). 48-52.]

[15] Zhang Lixu, Wei Wenshou. Change trend of snow cover and its relationship with air temperature and precipitation in the mid-mountain zone of the west Tianshan Mountains. Scientia Geographica Sinica, 2002, 22(1): 67-71.
[张丽旭, 魏 文寿. 天山西部中山带积雪变化趋势与气温和降水的关系. 地理科学, 2002, 22(1): 67-71.]

[16] Li Dongliang, Xie Jinnan, Wang Wen. A study of summer precipitation features and anomaly in Northwest China. Scientia Atmospherica Sinica, 1997, 21(3): 331-340.
[李栋梁, 谢金南, 王文. 中国西北夏季降水特征及其异常研究. 大气科学, 1997, 21(3): 331-340.]

[17] Yang Yang, Shi Neng. The secular variation of global land rainfall fields in September-November from 1948-2001. Scientia Meteorologica Sinica, 2003, 23(3): 253-262.
[杨扬, 施能. 1948-2001 年全球陆地9-11 月降水的长期变化. 气象科学, 2003, 23(3): 253-262.]

[18] Wei Fengying. Modern Climatic Statistical Diagnosis and Prediction Technology. Beijing: China Meteorological Press, 2000. 59-61.
[魏凤英. 现代气候统计诊断与预测技术. 北京: 气象出版社, 2000. 59-61.]

[19] Fan Lijun, Wei Zhigang, Dong Wenjie. The characteristic of temporal and spatial distribution of the differences between ground and air temperature in the arid region of northwest China. Plateau Meteorology, 2004, 23(3): 360-367.
[范丽军, 韦志刚, 董文杰. 西北干旱区地气温差的时空特征分析. 高原气象, 2004, 23 (3): 360-367.]

[20] Ma Shuhong, Xi Yuanwei. Some regularities of storm rainfall in Xinjiang. Acta Meteorologica Sinica, 1997, 55 (2): 239-247.
[马淑红, 席元伟. 新疆暴雨的若干规律性.气象学报, 1997, 55(2): 239-247.]

[21] Yang Jianping, Ding Yongjian, Chen Rensheng et al. Analysis on periodic variations of annual hydrologic and meteorological series in source regions of Yangtze and Yellow rivers. Journal of Desert Research, 2005, 25 (3): 351-355.
[ 杨建平, 丁永建, 陈仁升等. 长江黄河源区水文和气象序列周期变化分析. 中国沙漠, 2005, 25(3): 351-355.]

[22] Dong Anxiang, Zhu Xiaoni, Guo Hui. Sun activity and precipitation in northwest China. Journal of Gansu Sciences, 1999, 11(4): 14-17.
[董安祥, 祝小妮, 郭慧. 太阳活动与西北地区降水. 甘肃科学学报, 1999, 11(4): 14-17.]

[23] Wang Yongguang, Gong Zhensong, Xu Li et al. Analysis of long trend of temperature and precipitation in China and its influencing factors. Journal of applied Meteorological Science, 2005, (suppl.): 85-90.
[王永光, 龚振淞, 许力等. 中 国温度、降水的长期气候趋势及其影响因子分析.应用气象学报, 2005, (增刊): 85-90.]

[24] Jiang Fengqing, Yang Yuehui. Potential links of flood and drought disasters in Xinjiang to some larger-scale climatic driving forces. Arid Land Geography, 2004, 27(2): 148-152.
[姜逢清, 杨跃辉. 新疆洪旱灾害与大尺度气候强迫因子 的联系. 干旱区地理, 2004, 27(2): 148-152.]

[25] Zhou Yuchao. River Hydrology and Water Resources in Xinjiang. Urumqi: Xinjiang Technology and Hygiene Press, 1999. 1-444.
[周聿超. 新疆河流水文水资源. 乌鲁木齐: 新疆科技卫生出版社, 1999. l-444.]

[26] Liu Yunyun, He Jinhai, Wang Qianqian. Analysis of temporal-spatial features and circulation characteristics of summer precipitation in Xinjiang. Journal of Nanjing Institute of Meteorology, 2006, 29(1): 24-32.
[刘芸芸, 何金海, 王谦谦. 新疆地区夏季降水异常的时空特征及环流分析. 南京气象学院学报, 2006, 29(1): 24-32.]

[27] Tang Jianjun, Ma Shuhong, Wang Zhisheng et al. The characteristic and evolution tendency of precipitation along the Tianshan road. Desert and Oasis Meteorology, 2006, 29(4): 3-6.
[唐建军, 马淑红, 王治升等. 天山公路沿线年降水 量分布特征及其变化趋势. 沙漠与绿洲气象, 2006, 29(4): 3-6.]

[28] Leng Zhongxiao, Ge Lima, Haimid Yimit. Changes of average air temperature and rainfall in Urumqi under background of global warming. Journal of Arid Land Resources and Environment, 2007, 21(4): 60-65.
[冷中笑, 格丽玛, 海米提· 依米提. 全球变暖背景下的乌鲁木齐市气温及降水气候特征分析. 干旱区资源与环境, 2007, 21(4): 60-65.]

[29] Yuan Yujiang, Li Jiangfeng, Hu Ruji et al. Reconstruction of precipitation in the recent 350a from tree-rings in the middle Tianshan Mountains. Journal Glaciology and Geocryology, 2001, 23(1): 34-40.
[ 袁玉江, 李江风, 胡汝骥等. 用树木年轮重建天山中部近350a 来的降水量. 冰川冻土, 2001, 23(1): 34-40.]

[30] Ma Haixia, Zhang Baoshan. Economic division of Xinjiang and the shapement of north and south economic slope of Tianshan Mountain. Area Research and Development, 2006, 25(4): 48-52.
[马海霞, 张宝山. 新疆经济区划与天山南 北坡经济带的形成. 地域研究与开发, 2006, 25(4): 48-52.]

[31] Feng Huaizhen, Ma Haixia. Institution innovations and coordinative development of production and construction corps, local government and petrolium administration in economic zone of Tianshan Mountain. Journal of Xinjiang Vocational University, 2006, (4): 5-7.
[冯怀珍, 马海霞. 制度创新与新疆天山南北坡经济带及其协调发展. 新疆职业 大学学报, 2006, (4): 5-7.]

[32] Xiao Jiping, Peng Jianwen, Li Jie. An analysis of the economic growth in the southern Tianshan Mountain economic belt of Xinjiang. Journal of Xinjiang Normal University, 2005, 26(3): 44-48.
[肖冀平, 彭建文, 李杰. 新疆天山南坡经 济带经济增长分析. 新疆师范大学学报, 2005, 26(3): 44-48.]

Outlines

/