大尺度半分布式WASMOD模型汇流方法改进与应用
Improvement and Application of Routing Method for Large Scale Semi-Distributed WASMOD
DOI: 10.12677/JWRR.2019.81006, PDF,   
作者: 李晶晶, 陈 华, 许崇育, 赵浩源:武汉大学水资源与水电工程科学国家重点实验室,湖北 武汉;李 璐:挪威联合研究中心和Bjerknes气候研究中心,挪威 卑尔根
关键词: WASMOD模型日尺度DEM汇流算法WASMOD Daily Scale DEM Routing Algorithm
摘要: WASMOD水量平衡模型,能满足流域尺度、区域尺度甚至全球尺度的水文模拟,已在全球气候变化影响研究中得到广泛的应用,但其日模型汇流算法没有考虑不同流域地形对流速影响程度的差异。本文以长江流域的湘江、汉江和雅砻江流域为研究对象,建立半分布式日尺度WASMOD模型,通过考虑流域下垫面的影响,研究和改进模型的汇流算法,并比较分析模型汇流方法改进前后的径流模拟效果。结果表明:原模型汇流算法不能适应多种地形情况下的汇流计算,在部分流域计算得到汇流时间相较实际经验值偏长;改进后的模型能合理计算流域汇流时间,从而提高径流模拟精度;汇流算法的改进提高了模型的适用性,改进后的模型能够适应多种地形情况下的径流模拟。
Abstract: WASMOD, a water balance model, which can meet hydrological simulations at the basin scale, regional scale and even global scale, has been widely used in hydrological response to climate change. But its routing algorithm of daily-scale model does not consider the effect of topography on flow velocity which is variable in different watersheds. This paper establishes a semi-distributed daily-scale WASMOD model in Xiangjiang, Hanjiang and Yalongjiang basins in the Yangtze River basin, improves the model’s routing algorithm by considering the basin underlayer, and compares the model efficiency before and after the improvement. The results show that the original model routing algorithm cannot adapt to the routing calculation under various topography conditions. The delay time calculated in some basins is longer than the empirical value. The modified model can calculate the basin delay time reasonably and improve the model efficiency. The modified model can be adapted to runoff simulation under various topography conditions.
文章引用:李晶晶, 陈华, 许崇育, 赵浩源, 李璐. 大尺度半分布式WASMOD模型汇流方法改进与应用[J]. 水资源研究, 2019, 8(1): 56-66. https://doi.org/10.12677/JWRR.2019.81006

参考文献

[1] ARNELL, N. W., GOSLING, S. N. The impacts of climate change on river flood risk at the global scale. Climatic Change, 2016, 134(3): 387-401. [Google Scholar] [CrossRef
[2] 许崇育, 夏军. 大尺度水文模型的发展现状以及与气候模型耦合的可能性、挑战和展望[C]//中国自然资源学会. 中国自然资源学会2011年学术年会: 2011年卷. XU Chongyu, XIA Jun. The development of large-scale hydrological models and the possibility, challenge and prospect of coupling them with climate models. 2011 annual conference of China natural resources association, 2011. (in Chi-nese)
[3] DÖLL, P., KASPAR, F. and LEHNER, B. A global hydrological model for deriving water availability indicators: Model tuning and validation. Journal of Hydrology, 2003, 270(1): 105-134. [Google Scholar] [CrossRef
[4] LIANG, X., LETTENMAIER, D. P. and WOOD, E. F. One-dimensional statistical dynamic representation of subgrid spatial variability of precipitation in the two-layer variable infiltration capacity model. Journal of Geophysical Research Atmospheres, 1996, 101(D16): 21403-21422.
[5] VÖRÖSMARTY, C. J., FEDERER, C. A. and SCHLOSS, A. L. Potential evaporation functions compared on US watersheds: Possible implications for global-scale water balance and terrestrial ecosystem modeling. Journal of Hydrology, 1998, 207(3-4): 147-169.
[6] ARNELL, N. W. A simple water balance model for the simulation of streamflow over a large geographic domain. Journal of Hydrology, 1999, 217(3): 314-335. [Google Scholar] [CrossRef
[7] XU, C. Y., SEIBERT, J. and HALLDIN, S. Regional water balance modelling in the NOPEX area: Development and application of monthly water balance models. Journal of Hydrology, 1996, 180(1-4): 211-236.
[8] WIDÉN-NILSSON, E., GONG, L., HALLDIN, S., et al. Model performance and parameter behavior for varying time aggregations and evaluation criteria in the WASMOD-M global water balance model. Water Resources Research, 2009, 45(5): 5418. [Google Scholar] [CrossRef
[9] GONG, WIDÉN-NILSSON, HALLDIN, et al. Large-scale runoff routing with an aggregated network-response function. Journal of Hydrology, 2009, 368(1): 237-250. [Google Scholar] [CrossRef
[10] XU, C. Y. Application of water balance models to different climatic regions in China for water resources assessment. Water Resources Management, 1997, 11(1): 51-67. [Google Scholar] [CrossRef
[11] WIDÉN-NILSSON, E., HALLDIN, S. and XU, C. Y. Global wa-ter-balance modelling with WASMOD-M: Parameter estimation and regionalisation. Journal of Hydrology, 2007, 340(1): 105-118. [Google Scholar] [CrossRef
[12] EREGNO, F. E., XU, C. Y. and KITTERØD, N. O. Modeling hydrological impacts of climate change in different climatic zones. International Journal of Climate Change Strategies & Management, 2013, 5(3): 344-365. [Google Scholar] [CrossRef
[13] KIZZA, M., GUERRERO, J. L., RODHE, A., et al. Modelling catchment inflows into Lake Victoria: Regionalisation of the parameters of a conceptual water balance model. Hydrology Research, 2013, 44(5): 789-808. [Google Scholar] [CrossRef
[14] 李占玲, 徐宗学, 周训. WASMOD水文模拟残差统计特征检验[J]. 水利水电科技进展, 2013, 33(1): 13-17. LI Zhanling, XU Zongxue and ZHOU Xun. Check of statistical features of model residuals of WASMOD. Advances in Science and Technology of Water Resources, 2013(1): 13-17.
[15] LI, L., NGONGONDO, C. S., GONG, L., et al. Comparison of the global TRMM and WFD precipitation datasets in driving a large-scale hydrological model in Southern Africa. Hydrology Research, 2013, 44(5): 770-788. [Google Scholar] [CrossRef
[16] 熊立华, 彭定志. 基于数字高程模型的等流时线推求与应用[J]. 武汉大学学报(工学版), 2003, 36(3): 1-3. XIONG Lihua, PENG Dingzhi. Derivation of DEM-based isochrones of watersheds. Journal of Wuhan University of Hydraulic & Electric Engineering, 2003, 36(3): 1-3.
[17] 陈洋波. 基于HYDRO1K的数字水文分析方法及实例[J]. 人民长江, 2002, 33(9): 52-54. CHEN Yangbo. Digital hydrological analysis methods and examples based on HYDRO1K. Yangtze River, 2002, 33(9): 52-54. (in Chinese)
[18] XU, C. Y., SINGH, V. P. and FREVERT, D. WASMOD: The water and snow balance modeling system. 2002.
[19] GONG, L. Large-scale runoff generation and routing: Efficient parameterization using high-resolution topography and hydrography. PhD. Thesis, Uppsala University, Uppsala, 2010.