Articles | Volume 13, issue 7
https://doi.org/10.5194/hess-13-1261-2009
© Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License.
21 Jul 2009
The hydrological response of baseflow in fractured mountain areas
Related subject area
Disciplinary Fields: Hydrology and Soil Processes | Domains of Integration: Catchment and River Basin
A modeling study of heterogeneity and surface water-groundwater interactions in the Thomas Brook catchment, Annapolis Valley (Nova Scotia, Canada)
The significance and lag-time of deep through flow: an example from a small, ephemeral catchment with contrasting soil types in the Adelaide Hills, South Australia
Hydrol. Earth Syst. Sci., 13, 1583–1596, 2009
Hydrol. Earth Syst. Sci., 13, 1201–1214, 2009
Cited articles
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Aguilar, C.: Efectos de escala en procesos hidrológicos, Aplicación a la cuenca del río Guadalfeo, M. S. in Hydrology, University of Cordoba, 40–42, 2006. http://www.cuencaguadalfeo.com/archivos/DEA_Cristina_Aguilar.pdf
Al Alwani, G. K.: Hidrología e Hidrogeología en la Cuenca del Río Guadalfeo: Aplicación del modelo HPSF para la simulación de la fusión de nieve y del balance hídrico, Ph. D. Thesis, University of Granada, Granada, 1997.
Bako, M. D. and Hunt, D. N.: Derivation of baseflow recession constant using computer and numerical analysis, Hidrol. Sci. J., 33(4), 357–367, 1988.
Castillo, A., Cruz, S. J., and Benavente, J.: Aguas de Sierra Nevada; Aguas de Lanjarón, in Lanjarón: los paisajes del agua, edited by: Balneario de Lanjarón, S. A., Granada, 320, 35–64, 1999.
