Water and sediment budgets unveiling contrasting hydro-sedimentary patterns in a mountainous Mediterranean catchment.

Mountain regions have a key role in the generation of runoff, and in the production and transfer of sediments to fluvial networks, especially in Mediterranean catchments where these processes are affected by marked changes in climate and land use (i.e. global change).

The extreme floods in the Ebro River basin since 1600 CE.

Reliable and complete knowledge of the historical floods is necessary for understanding the extreme hydrological dynamics of the rivers, their natural variability and anthropic changes. In this work we reconstruct the most important floods of the Ebro basin during the last 400 years in different areas of the basin. The analysis is based on four different areas: the Ebro River at Zaragoza, the Cinca River at Fraga, the Segre River at Lleida, and the Ebro River near its mouth at Tortosa.

Rainfall, runoff and sediment transport in a Mediterranean mountainous catchment.

The relation between rainfall, runoff, erosion and sediment transport is highly variable in Mediterranean catchments. Their relation can be modified by land use changes and climate oscillations that, ultimately, will control water and sediment yields. This paper analyses rainfall, runoff and sediment transport relations in a meso-scale Mediterranean mountain catchment, the Ribera Salada (NE Iberian Peninsula).

Effects of afforestation on runoff and sediment load in an upland Mediterranean catchment.

This paper assesses annual and seasonal trends in runoff and sediment load resulting from climate variability and afforestation in an upland Mediterranean basin, the Ribera Salada (NE Iberian Peninsula). We implemented a hydrological and sediment transport distributed model (TETIS) with a daily time-step, using continuous discharge and sediment transport data collected at a monitoring station during the period 2009-2013. Once calibrated and validated, the model was used to simulate the hydrosedimentary response of the basin for the period 1971-2014 using historical climate and land use data.

First Report of a Branch Dieback of Olive Trees in Tunisia Caused by a Phoma sp.

From 2007 to 2008, a new dieback of branches of olive trees was observed in several orchards in central and southern Tunisia. The appearance of this new syndrome coincided with warm temperatures and frequent rainfall from February to April 2007. Affected trees were observed in seven commercial orchards; disease incidence ranged from 1 to 9% and affected trees were randomly distributed in each orchard.