[1]LIU Shi-yu,ZHANG Jun-xia,LUO Zhi-jun,et al.Response of Runoff to Rainfall in Dakeng Small Watershed in Northwestern Jiangxi Province over the Last 50 Years[J].Research of Soil and Water Conservation,2012,19(01):19-22.
Copy
Response of Runoff to Rainfall in Dakeng Small Watershed in Northwestern Jiangxi Province over the Last 50 Years
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
19
Number of periods:
2012 01
Page number:
19-22
Column:
Public date:
2012-02-20
- Title:
- Response of Runoff to Rainfall in Dakeng Small Watershed in Northwestern Jiangxi Province over the Last 50 Years
- CLC:
- P468.0+24
- DOI:
- -
- Abstract:
- Based on the data from 1957—2005 in Dakeng Small Watershed in Northwestern Jiangxi Province, the analysis of precipitation variation and its runoff response were carried out by mean of time-serial eigenvalue, statistical regression. The results suggested that: (1) annual mean precipitation is 1 596.3 mm, which monthly variation has presented a single-peak pattern during a year, and the difference of quarterly precipitation is very obvious. What’s more, the annual variation of precipitation is bigger and presents increasing tendency totally; (2) annual mean runoff depth is 814.3 mm, which monthly variation has presented a single-peak pattern during a year, and the difference of quarterly runoff depth is very obvious. What’s more, the anuual variation of runoff depth is bigger and presents increasing tendency totally; (3) runoff depth changes are closely correlated with precipitation variations. While annual hydrological precipitation increased or decreased by 10%, annual runoff depth shows 17.8% of positive response. Meanwhile, while anuual hydrological precipitation increased or decreased by 20%(30%), the corresponding anuual runoff depth shows 35.6%(53.4%)of positive response.
- References:
-
[1] 张运福, 王颖, 赵春雨.辽宁省雨日数的气候特征[J].自然灾害学报, 2008, 17 (5):75-81.
[2] 唐湘玲, 魏文寿.玛纳斯河流域气候变化对径流变化的影响[J].石河子大学学报:自然科学版, 2005, 23 (6):730-734.
[3] Kamran H S, Goodrich D C, Myers D E, et al. Spatial characteristics of thunderstorm rainfall fields and their relation to runoff[J]. Journal of Hydrology, 2003, 271 (1):1-21.
[4] Marin C T, Boutena W, Sevinka J. Gross rainfall and its partitioning into throughfall, stemflow and evaporation of intercepted water in four forest ecosystems in western Amazonia[J]. Journal of Hydrology, 2000, 237 (1):40-57.
[5] 任国玉, 郭军, 徐铭志, 等.近50年来中国地面气候变化基本特征[J].气象学报, 2005, 63 (6):942-956.
[6] 王顺德, 王彦国, 王进, 等.塔里木河流域近40 a来气候、水文变化及其影响[J].冰川冻土, 2003, 25 (3):315-320.
[7] 徐素宁, 杨景春, 李有利.近50 a来玛纳斯河流量变化及对气候变化的响应[J].地理与地理信息科学, 2004, 20 (6):65-68.
[8] 康玲玲, 余辉, 王金花, 等.气候变化对黄河唐乃亥以上地区径流量的影响[J].水力发电, 2005, 31 (7):22-24.
[9] 叶柏生, 李翀, 杨大庆, 等.我国过去50 a来降水变化趋势及其对水资源的影响.Ⅰ:年系列[J].冰川冻土, 2004, 26 (5):587-594.
[10] 叶柏生, 李翀, 杨大庆, 等.我国过去50 a来降水变化趋势及其对水资源的影响.Ⅱ:月系列[J].冰川冻土, 2005, 27 (1):100-105.
[11] 王怀清, 赵冠男, 彭静.近50年鄱阳湖五大流域降水变化特征研究[J].长江流域资源与环境, 2009, 18 (7):616-619.
[12] 林承坤, 吴小根.长江径流量特性及其重要意义的研究[J].自然杂志, 1999, 21 (4):200-205.
- Similar References:
Memo
-
Last Update:
1900-01-01