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| Titel |
Hydrological processes and their seasonal controls in a small Mediterranean mountain catchment in the Pyrenees |
| VerfasserIn |
F. Gallart, P. Llorens, J. Latron, D. Regüés |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1027-5606
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| Digitales Dokument |
URL |
| Erschienen |
In: Hydrology and Earth System Sciences ; 6, no. 3 ; Nr. 6, no. 3, S.527-537 |
| Datensatznummer |
250003569
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| Publikation (Nr.) |
 copernicus.org/hess-6-527-2002.pdf |
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| Zusammenfassung |
| The
Vallcebre catchments are located in a middle mountain area of the Pyrenean
ranges, built up by sedimentary rocks and loamy soils. The vegetation cover is
pastures and forests of Pinus sylvestris, mostly occupying former agricultural
terraces. Some relatively small, heavily eroded landscapes (badlands) occur in
the catchments, playing a relevant hydrological and geomorphic role. Annual
precipitation is 924 mm and potential (reference) evapotranspiration is about
700 mm. Rainfall interception in forests represents about 24% of precipitation;
interception rates were similar throughout the seasons because of a compensation
between rainfall intensities and atmospheric conditions. Soil moisture showed a
temporal pattern characterised by the occurrence of marked deficit periods in
summer and also, but less pronounced, in winter. During most of the year,
subsurface flows on hillslopes drove the spatial organisation of soil moisture
and the occurrence of saturated areas. Nevertheless, this spatial organisation
was also controlled by the patterns of vegetation cover. During dry periods,
subsurface flow ceased, saturated areas disappeared and the spatial patterns of
soil moisture changed. Stream flow from these catchments was dominated by storm
flow, and the runoff generating mechanisms showed a clear seasonal pattern,
controlled mainly by the soil moisture and the extent of saturated areas. During
the dry periods, runoff was produced only on impervious areas and badlands. At
the end of the dry periods, some large rainfall events generated significant
runoff because of the perched saturation of the shallow soil horizons.
Thereafter, runoff generation was dominated by the role of saturated areas.
Stream waters in catchments with badlands had very high suspended sediment
concentrations. The seasonal pattern of erosion processes in badlands was
characterised by physical weathering during winter, regolith breakdown and
vigorous hillslope erosion during spring and summer, and efficient transport of
sediments in autumn. |
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