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晋江西溪流域不同暴雨过程LUCC的洪水响应

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以晋江西溪流域为研究区,构建晋江西溪流域暴雨次洪分布式模型,选择3场不同暴雨强度、雨型分布、历时的暴雨过程,模拟研究区在1988年和2006年土地利用/覆被情景下70年代3场次暴雨的洪水过程,分析其在1988—2006年土地利用/覆被变化( LUCC)情景下的洪水响应。研究结果为:1988—2006年晋江西溪流域LUCC最明显的特征是林地、耕地减少而园地及建设用地增加; LUCC对流域出口流量过程的影响主要表现为洪量、洪峰流量增加,而对洪峰滞时及汇流时间的影响不显著;相同的LUCC对不同场次暴雨洪水过程的洪峰流量、洪量的影响程度不同, LUCC对流域出口流量过程的影响受暴雨强度、雨型分布、历时等因素的影响。
Simulation of Effects of LUCC on Flood Evolution in Xixi Watershed, Jinjiang River
This research takes Xixi watershed of Jinjiang River in the south of Fujian province as study area. The HEC-HMS model is built for flood simulation during heavy rain time, based upon which, effects of LUCC on floods process caused by heavy rain are studied. Results show that:1) in the study period, the most obvious characteristics of LUCC in the watershed are the reduction of forest and culti-vated lands, compared to the increase of garden and construction lands. The conversions mainly in-clude woodland to garden, cultivated land to garden, cultivated land to forest land and cultivated land to construction land; 2 ) from 1988 to 2020 , the effects of LUCC on flood process at the export of Xixi basin are mainly the increase of flood discharge and peak flow, but the impact on flood peak lag time and flood confluence time is not significant. And the effects are at the same time influenced by heavy rain intensity, heavy rain type distribution and heavy rain duration.

HEC-HMSLUCCrain intensityflood evolution

陈芬、陈兴伟、陈莹

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福建师范大学 地理研究所,福州350007

福建省亚热带资源与环境重点实验室,福州350007

福建师范大学 地理科学学院,福州350007

HEC-HMS模型 LUCC 暴雨过程 洪水响应

国家自然科学基金福建省自然科学基金

413010312013J01155

2015

亚热带资源与环境学报
福建师范大学

亚热带资源与环境学报

CSTPCD
影响因子:0.425
ISSN:1673-7105
年,卷(期):2015.10(4)
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