基于网格降水产品的资水流域实况面雨量计算方法研究
Research on Method of Live Surface Rainfall in Zishui Basin Based on Grid Precipitation Products
DOI: 10.12677/AG.2019.910097, PDF,    科研立项经费支持
作者: 徐靖宇, 周长青*, 陈静静:湖南省气象台,湖南 长沙;陈红专, 欧小锋:怀化市气象局,湖南 怀化
关键词: 资水流域面雨量格点平均法网格降水实况Zishui River Basin Surface Rainfall Grid Point Average Method Grid Precipitation Reality
摘要: 本研究利用2008~2018年中国地面与CMORPH融合逐小时降水网格实况产品与DEM高程数据开展资水流域实况面雨量计算方法研究。首先利用GIS技术对资水流域DEM高程数据进行建模,计算汇流信息并建立栅格河网,进而生成河流分水岭,利用反向搜索技术从流域的出口沿河道向上游搜索每一条河道的集水区范围,对搜到的所有栅格所占区域的边界进行勾画确定总的流域界限,将资水流域划分为6个子流域。其次利用湖南范围降水网格产品,通过GIS技术将降水网格映射到其所属流域范围,建立网格与流域之间的索引。最后利用格点平均法,逐一计算各流域内所有网格点的降雨量平均值,进而得到该流域的流域面雨量实况。
Abstract: This paper uses the hourly precipitation grid live product and DEM elevation data of China ground and CMORPH fusion in 2008-2018 to study the calculation method of the actual surface rainfall in Zishui Basin. Firstly, the GIS technology is used to model the DEM elevation data of the Zishui Basin, calculate the sink information and establish a grid river network, and then generate the river watershed, use the reverse search technology to search the upstream of the river basin from the outlet of the basin. The scope of the water area, the boundary of the area occupied by all the found grids is delineated to determine the total basin boundary, and the water basin is divided into 6 sub-basins. Secondly, using the Hunan-based precipitation grid product, the precipitation grid is mapped to the scope of the watershed by its GIS technology, and the index between the grid and the basin is established. Finally, using the grid point averaging method, the average rainfall value of all grid points in each basin is calculated one by one, and then the basin surface rainfall in the basin is obtained.
文章引用:徐靖宇, 周长青, 陈静静, 陈红专, 欧小锋. 基于网格降水产品的资水流域实况面雨量计算方法研究[J]. 地球科学前沿, 2019, 9(10): 921-927. https://doi.org/10.12677/AG.2019.910097

参考文献

[1] 蔡敷川, 黄帅, 肖明丽. 基于GIS技术的东江流域面雨量监测系统的设计[J]. 广东水利水电, 2018(10): 61-65.
[2] 袁定波, 艾萍, 洪敏. 基于地理空间要素的雅砻江流域面雨量估算[J]. 水利水电快报, 2019, 40(3): 5.
[3] 王增凯, 马超, 王晓鹏, 等. 不同量级降水推算面雨量的算法浅析[J]. 地下水, 2019, 44(4): 166-167+190.
[4] 张晓鑫. 基于多源降水资料的江西省流域面雨量计算方法对比分析[D]: [硕士学位论文]. 兰州: 兰州大学, 2018.
[5] Xie, P.P. and Xiong, A.Y. (2011) A Conceptual Model for Constructing High-Resolution Gauge-Satellite Merged Precipitation Analyses. Journal of Geophysical Research, 116, 1-14. [Google Scholar] [CrossRef
[6] 旷达, 沈艳, 牛铮, 等. 卫星反演降水产品误差随时空分辨率和雨强的变化特征分析[J]. 遥感信息, 2012, 27(4): 75-81.
[7] 宇婧婧, 沈艳, 潘旸, 等. 概率密度匹配法对中国区域卫星降水资料的改进[J]. 应用气象学报, 2013, 24(5): 544-553.
[8] 吕一兵, 张斌, 陈智虎, 等. 基于DEM的不同地貌类型区小流域划分及分布特征研究——以贵州省赤水河流域为例[J]. 测绘通报, 2017(9): 110-115.
[9] 张智超, 闫丹丹. 流域面雨量的计算方法[J]. 水利科技与经济, 2016(12): 34-37.
[10] 王志, 赵琳娜, 张国平, 等. 汶川地震灾区堰塞湖流域面雨量计算方法研究[J]. 气象, 2010(6): 7-12.
[11] 芮孝芳. 随机产汇流理论[J]. 水利水电科学进展, 2016(5): 8-12.