Linear and nonlinear input/output models for karstic springflow and flood prediction at different time scales

被引：0

作者：

D. Labat

R. Ababou

A. Mangin

机构：

[1] Institut de Mécanique des Fluides de Toulouse,

[2] Allée du Professeur Camille Soula,undefined

[3] F-31400 Toulouse,undefined

[4] France Tel: +33 (0)5 61 28 58 45; Fax: +33 (0)5 61 28 58 99 e-mail: labat@imft.fr,undefined

[5] ababou@imft.fr,undefined

[6] Laboratoire Souterrain de Moulis,undefined

[7] F-09200 Moulis,undefined

[8] France,undefined

来源：

Stochastic Environmental Research and Risk Assessment | 1999年 / 13卷

关键词：

Key words: karst hydrology; floods; kernel identification; nonlinear models; Volterra expansions.;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

Karstic formations function as three-dimensional (3D) hydrological basins, with both surface and subsurface flows through fissures, natural conduits, underground streams and reservoirs. The main characteristic of karstic formations is their significant 3D physical heterogeneity at all scales, from fine fissuration to large holes and conduits. This leads to dynamic and temporal variability, e.g. highly variable flow rates, due to several concurrent flow regimes with several distinct response times.

引用

页码：337 / 364

页数：27

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