自然资源学报 ›› 2013, Vol. 28 ›› Issue (11): 1922-1934.doi: 10.11849/zrzyxb.2013.11.009
叶正伟1,2,3, 许有鹏3, 潘光波3
收稿日期:
2012-06-08
修回日期:
2013-04-29
出版日期:
2013-11-20
发布日期:
2013-11-20
作者简介:
叶正伟(1973-),男,安徽黄山人,副教授,博士,主要从事水文气象与自然灾害方面的研究。E-mail:leafyzw@163.com
基金资助:
YE Zheng-wei1,2,3, XU You-peng3, PAN Guang-bo3
Received:
2012-06-08
Revised:
2013-04-29
Online:
2013-11-20
Published:
2013-11-20
摘要: 采用降水集中度、等级分析及小波相干等方法,探讨了江淮下游里下河腹部地区1957—2006 年间降水、水位的等级特征及两者关系。结果表明:①年降水量的集中期与集中度皆为减小趋势,两者在1980 年前后由同相位转为反相位相关。②汛期高等级降水的日数和贡献率皆以1980 年代最高。不同等级的降水日数皆为减少趋势,但高等级降水的贡献率在大洪涝年中异常偏高,表明降水强度加强。③低、高等级水位日数皆为减少趋势,但低、高等级水位的贡献率分别呈增加、减少趋势,而中等级水位的日数与贡献率都显著增加。较之降水日数,降水贡献率对水位等级变化更具决定性影响。④高等级降水与水位在日数上呈显著的同相位正相关,但低等级相反,而中等级为较弱正相关,且等级降水总量与相应水位贡献率的相位关系亦具类似特征。高、低等级降水与水位的贡献率皆为显著同相位正相关,但在中等级上,其相位特征较弱。
中图分类号:
叶正伟, 许有鹏, 潘光波. 江淮下游降水特征及其对水位的影响研究——以里下河腹部地区为例[J]. 自然资源学报, 2013, 28(11): 1922-1934.
YE Zheng-wei, XU You-peng, PAN Guang-bo. Precipitation Variations and Its Impact on Water Level in the Lower Reaches of Jianghuai Basin:A Case Study in the Inner Lixiahe Region[J]. JOURNAL OF NATURAL RESOURCES, 2013, 28(11): 1922-1934.
[1] IPCC. Climate Change 2007: The Physical Science Basis: Summary for Policy Makers[M]. Cambridge and New York: Cambridge University Press, 2007. [2] 丁一汇, 任国玉, 石广玉, 等. 气候变化国家评估报告(I): 中国气候变化的历史和未来趋势[J]. 气候变化研究进展, 2006, 2(1): 3-8.[DING Yi-hui, REN Guo-yu, SHI Guang-yu, et al. National assessment report of climate change (I): Climate change in China and its future trend. Advances in Climate Change Research, 2006, 2(1): 3-8.] [3] Milly P C D, Wetherald R T, Dunne K A, et al. Increasing risk of great floods in a changing climate[J]. Nature, 2002, 415: 514-517. [4] Ding Y, Wang Z, Sun Y. Inter-decadal variation of the summer precipitation in East China and its association with decreasing Asian summer monsoon. Part I: Observed evidences[J]. International Journal of Climatology, 2007, 28: 1139-1161. [5] 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.[SHE Dun-xian, XIA Jun, ZHANG Yong-yong, et al. The trend analysis and statistical distribution of extreme rainfall events in the Huaihe River Basin in the past 50 years. Acta Geographica Sinca, 2011, 66(9): 1200-1210.] [6] 杜鸿, 夏军, 曾思栋, 等. 淮河流域极端径流的时空变化规律及统计模拟[J]. 地理学报, 2012, 67(3): 398-409.[DU Hong, XIA Jun, ZENG Si-dong, et al. Temporal and spatial variations and statistical models of extreme runoff in Huaihe River Basin. Acta Geographica Sinca, 2012, 67(3): 398-409.] [7] 魏凤英, 张婷. 淮河流域夏季降水的振荡特征及其与气候背景的联系[J]. 中国科学D 辑, 2009, 39(10): 1360-1374.[WEI Feng-ying, ZHANG Ting. Oscillation characteristics of summer precipitation in the Huaihe River valley and relevant climate background. Science in China Series D, 2009, 39(10): 1360-1374.] [8] 汪方, 田红. 淮河流域1960—2007 年极端强降水事件特征[J]. 气候变化研究进展, 2010, 6(3): 228-229.[WANG Fang, TIAN Hong. Characteristics of extreme precipitation events in Huaihe River Basin in 1960-2007. Advances in Climate Change Research, 2010, 6(3): 228-229.] [9] 董全, 陈星, 陈铁喜, 等. 淮河流域极端降水与极端流量关系的研究[J]. 南京大学学报: 自然科学版, 2009, 45(6): 790-801.[DONG Quan, CHEN Xing, CHEN Tie-xi, et al. Relationship between extremes of precipitation and discharge in the Huaihe River Basin. Journal of Nanjing University: Natural Science, 2009, 45(6): 790-801.] [10] 章国材, 毕宝贵, 鲍媛媛, 等. 2003 年淮河流域强降水大尺度环流特征及成因分析[J]. 地理研究, 2004, 23(6): 795-804.[ZHAN Guo-cai, BI Bao-gui, BAO Yuan-yuan, et al. The features of the large-scale circulation leading to catastrophic flood over the Huaihe River Basin during the summer of 2003 and cause exploration. Geographical Research, 2004, 23(6): 795-804.] [11] 司东, 丁一汇, 柳艳菊. 中国梅雨雨带年代际尺度上的北移及其原因[J]. 科学通报, 2010, 55(1): 68-73.[SI Dong, DING Yi-hui, LIU Yan-ju. Decadal northward shift of the Meiyu belt and the possible cause. Chinese Sciences Bulletin, 2010, 55(1): 68-73.] [12] 胡娅敏, 丁一汇. 2000 年以来江淮梅雨带北移的可能成因分析[J]. 气象, 2009, 35(12): 37-43.[HU Ya-min, DING Yi-hui. Possible reasons for northward shift of Meiyu belt in Yangtze-Huaihe River region during 2000-2005. Meteorological Monthly, 2009, 35(12): 37-43.] [13] Osborn T J, Hulme M, Jones P D, et al. Observed trends in the daily intensity of United Kingdom precipitation[J]. International Journal of Climatology, 2000, 20: 347-364. [14] Zhang Qiang, Vijay P Singh, Peng Juntai, et al. Spatial-temporal changes of precipitation structure across the Pearl River Basin, China[J]. Journal of Hydrology, 2012, (440/441): 113-122. [15] 叶正伟, 许有鹏, 潘光波.江淮平原水网区汛期雨量与洪涝水位关系——以江苏里下河腹部地区为例[J]. 地理研 究, 2011, 30(6): 1137-1146.[YE Zheng-wei, XU You-peng, PAN Guang-bo. Relationship between flood rainfall and water level in a Jianghuai Plain river network region: A case study in the inner Lixiahe, Jiangsu. Geographical Research, 2011, 30(6): 1137-1146.] [16] 叶正伟, 许有鹏, 徐金涛. 江苏里下河地区洪涝灾害演变趋势与成灾机理分析[J]. 地理科学, 2009, 29(6): 880-885.[YE Zheng-wei, XU You-peng, XU Jin-tao. Flood changing trend and flooding mechanism in Lixiahe region, Jiangsu, China. Scientia Geographica Sinica, 2009, 29(6): 880-885.] [17] 潘光波, 许有鹏, 丁瑾佳, 等. 江淮下游平原地区降水时空变化——以江苏里下河腹部区为例[J]. 南京大学学报: 自然科学, 2010, 46(6): 671-680.[PAN Guang-bo, XU You-peng, DING Jin-jia, et al. Spatial-temporal variations of precipitation in the lower Jianghuai plain: A case study of the Inner Lixiahe Region, Jiangsu. Journal of Nanjing University: Natural Sciences, 2010, 46(6): 671-680.] [18] 陈家华, 陆菊中, 潘益农, 等. 江苏省里下河地区梅雨洪涝灾害成因与规律的探讨[J]. 气象科学, 1998, 18(2): 167-173.[CHEN Jia-hua, LU Ju-zhong, PAN Yi-nong, et al. Formative causes of Mei-yu flooding disaster in the Lixiahe River (Jiangsu) and its trend prediction. Scientia Meteorologica Sinica, 1998, 18(2): 167-173.] [19] 蔡敏, 丁裕国, 江志红. 我国东部极端降水时空分布及其概率特征[J]. 高原气象, 2007, 26(2): 309-318.[CAI Min, DING Yu-guo, JIANG Zhi-hong. Extreme precipitation experimentation over eastern China based on L-moment estimation. Plateau Meteorology, 2007, 26(2): 309-318.] [20] 尹义星, 许有鹏. 太湖流域腹部地区水位对降水变化及城镇化的响应[J]. 自然资源学报, 2011, 26(5): 669-779.[YIN Yi-xing, XU You-peng. Response of water levels to precipitation changes and regional urbanization in the core regions of the Taihu Lake basin. Journal of Natural Resources, 2011, 26(5): 669-779.] [21] Mann H B. Nonparametric tests against trend[J]. Econometrica, 1945, 13: 245-259. [22] Oliver, J E. Monthly precipitation distribution: A comparative index[J]. Professional Geographer, 1980, 32: 300-309. [23] Zhang L J, Qian Y F. Annual distribution features of the yearly precipitation in China and their interannual variations[J]. Acta Meteorologica Sinica, 2003, 17(2): 146-163. [24] Karl T R, Knight R W. Secular trends of precipitation amount frequency and intensity in the United States[J]. Bulletin of the American Meteorological Society, 1998, 79: 231-241. [25] Torrence C, Compo G P. A practical guide to wavelet analysis[J]. Bulletin of the American Meteorological Society, 1998, 79: 61-78. [26] Grinsted A, Moore J C, Jevrejeva S. Application of the cross wavelet transform and wavelet coherence to geophysical time series[J]. Nonlinear Processes in Geophysics, 2004, 11: 561-566. [27] Chin A. Urban transformation of river landscapes in a global context[J]. Geomorphology, 2006, 79: 460-487. [28] 秦莉莉, 陈云霞, 许有鹏. 城镇化对径流的长期影响研究[J]. 南京大学学报: 自然科学版, 2005, 41(3): 279-285.[QIN Li-li, CHEN Yun-xia, XU You-peng. A Research of long-term impact on runoff in urbanized areas. Journal of Nanjing University: Natural Sciences, 2005, 41(3): 279-285.] [29] 肖卉, 姜爱军, 沈真, 等. 江苏省最大日降水量时空分布特征及其统计拟合[J]. 气象科学, 2006, 26(2): 177-182.[XIAO Hui, JIANG Ai-jun, SHEN Zhen, et al. The space-time distribution characters of maximum diurnal precipitation in Jiangsu Province and the statistic assimilation. Scientia Meteorologica Sinica, 2006, 26(2): 177-182.] |
[1] | 李海宏, 吴吉东. 2007—2016年上海市暴雨特征及其与内涝灾情关系分析[J]. 自然资源学报, 2018, 33(12): 2136-2148. |
[2] | 许涛, 蔡健榕, 孙晓双, 崔梦月, 雷国良, 姜修洋. 台风“杜鹃”降水δ18O的云雨区效应初探[J]. 自然资源学报, 2018, 33(12): 2238-2248. |
[3] | 李芮, 潘兴瑶, 邸苏闯, 杨默远, 苏遥. 北京城区典型内涝积水原因诊断研究——以上清桥区域为例[J]. 自然资源学报, 2018, 33(11): 1940-1952. |
[4] | 苗茜, 谢志清, 曾燕, 王珂清, 孙佳丽. 基于统计-FloodArea模型的平原水网区致灾临界雨量研究[J]. 自然资源学报, 2018, 33(9): 1563-1574. |
[5] | 李沛, 黄生志, 黄强, 马岚, 吴洪石, 栾金凯. 大通河流域降水结构的演变特征及其驱动力探究[J]. 自然资源学报, 2018, 33(9): 1588-1598. |
[6] | 李文龙, 石育中, 鲁大铭, 刘倩, 乌铁红. 北方农牧交错带干旱脆弱性时空格局演变[J]. 自然资源学报, 2018, 33(9): 1599-1612. |
[7] | 莫兴国, 胡实, 卢洪健, 林忠辉, 刘苏峡. GCM预测情景下中国21世纪干旱演变趋势分析[J]. 自然资源学报, 2018, 33(7): 1244-1256. |
[8] | 贺敏, 宋立生, 王展鹏, 辜清, 王大菊, 郭博. 基于多源数据的干旱监测指数对比研究——以西南地区为例[J]. 自然资源学报, 2018, 33(7): 1257-1269. |
[9] | 张扬, 李宝富, 陈亚宁. 1970—2013年西北干旱区空中水汽含量时空变化与降水量的关系[J]. 自然资源学报, 2018, 33(6): 1043-1055. |
[10] | 柳媛普, 王素萍, 王劲松, 王芝兰. 气候变暖背景下西南地区干旱灾害风险评估[J]. 自然资源学报, 2018, 33(2): 325-336. |
[11] | 马荣, 张明军, 王圣杰, 王杰, 杨森, 陈荣. 近50 a西北干旱区冬季积雪日数变化特征[J]. 自然资源学报, 2018, 33(1): 127-138. |
[12] | 卢晓宁, 张静怡, 王玲玲, 孟成真, 曾德裕. 综合考虑植被、温度和降水的四川省月尺度伏旱遥感监测[J]. 自然资源学报, 2017, 32(7): 1145-1157. |
[13] | 唐敏, 张勃, 张耀宗, 王国强, 马彬, 贾艳青. 基于SPEI和SPI指数的青海省东部农业区春夏气象干旱特征的评估[J]. 自然资源学报, 2017, 32(6): 1029-1042. |
[14] | 景丞, 陶辉, 王艳君, 苏布达, 黄金龙, 姜彤. 基于区域气候模式CCLM的中国极端降水事件预估[J]. 自然资源学报, 2017, 32(2): 266-277. |
[15] | 周扬, 徐维新, 张娟, 白爱娟, 刘晓敬, 徐国元. 2013—2015年青藏高原玛多地区两次动态融雪过程及其与气温关系对比分析[J]. 自然资源学报, 2017, 32(1): 101-113. |
|