Hydrological response to precipitation event on june 2013 in central Pyrenees

被引:0
|
作者
Serrano Notivoli, Roberto [1 ,2 ]
Mora Mur, Daniel [1 ,2 ,3 ]
Ollero Ojeda, Alfredo [1 ,2 ]
Sanchez Fabre, Miguel [1 ,2 ]
Saz Sanchez, Miguel Angel [1 ,2 ]
机构
[1] Univ Zaragoza, Dept Geog & Ordenac Terr, Zaragoza, Spain
[2] Univ Zaragoza, Inst Univ Ciencias Ambientales, Zaragoza, Spain
[3] Medio Ambiente Terr & Geog SL, Zaragoza, Spain
来源
关键词
Pyrenees; hydrological flood; Cinca; Esera; Esca; Benasque; Aragon;
D O I
10.14198/INGEO2014.62.01
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
In this paper is analyzed the hydrological response of Cinca and Esca headwaters, and Ese basin to intense precipitation epode, produced in central Pyrenees from 17th to 19th june 2013. 122 meteorological stations are used to study rainfall behavior in different temporal scales, and 7 gauges to view temporality and intensity on flow responses. Rainfall discharge was not unusual in historical series, but it joined to a snowmelt, which produced an increase on flow at highest headwaters. The consequences of floods have reactivated fluvial geomorphic processes, reoccupying former floodplain, although the intense territorial occupation of the last 50 years in the Valley of Benasque has produced that exposure to risk is much higher as a result of poorly controlled urban growth.
引用
收藏
页码:5 / 21
页数:17
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