Hydrological processes and their seasonal controls in a small Mediterranean mountain catchment in the Pyrenees

Abstract

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.

Hydrological dynamics in a small catchment with silvopastoral land use in SW Spain

“…The complexity in the generation of runoff was also reported for several drainage basins with Mediterranean mountain climate (Gallart et al, 2002;García Ruiz et al, 2005). Llorens and Gallart (1992) and Gallart et al (1994) already showed that the response of these catchments is largely driven by antecedent conditions, demonstrating that during the year, the dominant runoff generation mechanisms change gradually, as a result of both varying catchment antecedent wetness conditions and changing rainfall event characteristics (Gallart et al, 2005).…”

Response of Scots pine (Pinus sylvestris L.) and pubescent oak (Quercus pubescens Willd.) to soil and atmospheric water deficits under Mediterranean mountain climate

“…Climate is sub-Mediterranean, with an average air temperature of 7.3 • C (measured at 1440 m.a.s.l.) and 924 mm of annual rainfall [16]. The present landscape is mainly a mosaic of mesophilous grassland of the Aphyllantion type and Scots pine forests, which colonised old agricultural terraces after their abandonment [37].…”

Investigating hydrological regimes and processes in a set of catchments with temporary waters in Mediterranean Europe

“…Beven, 2002). Nevertheless, field studies have shown that overland flow may also be produced in these environments as the result of saturation mechanisms, such as the saturation of thin soils during large events (Martinez-Mena et al, 1998), the seasonal saturation of first order valley bottoms (Ceballos & Schnabel, 1998) or the seasonal formation of a water table and saturated areas throughout the catchment, with relevant contribution from subsurface flow (Gallart et al, 2002;Latron & Gallart, 2007). Hydrological systems are complex, and different hydrologists might not necessarily agree on which are the most important processes in a catchment (Beven, 2002).…”