Sandra Ardoin-Bardin

Current state of Mediterranean water resources and future trends under climatic and anthropogenic changes

Abstract The Mediterranean basin has been identified as one of the worlds regions most vulnerable to climatic and anthropogenic changes. A methodology accounting for the basin specific conditions is developed to assess the impacts of these changes on water resources. Based on global climate projections and water-use scenarios inspired by national reports, the current water stress state is addressed first and then it is explored for the medium-term. Currently, the southern and eastern rims are experiencing high to severe water stress. By the 2050 horizon, this stress could increase over the whole Mediterranean basin, notably because of a 30–50% decline in freshwater resources as a result of climate change. In addition, under a business-as-usual water-use scenario, total water withdrawals are projected to double on the southern and eastern rims. These worrying trends indicate the need to develop mitigation scenarios. In accord with the Mediterranean Strategy for Sustainable Development, an alternative water-use scenario based on improvements in the efficiency of water distribution networks and of irrigated agriculture is investigated. Such progress would stabilize total water withdrawals over the Mediterranean basin and even make them decrease (10–40%) in many northern catchments. Water stress could thus be tempered in some eastern catchments and remain low on the northern rim. This study highlights the importance of developing sustainable development strategies to cope with climatic and anthropogenic changes in order to explore their impacts at regional scales. It supports the need to focus on the most vulnerable areas within the Mediterranean basin. Editor Z.W. Kundzewicz Citation Milano, M., Ruelland, D., Fernandez, S., Dezetter, A., Fabre, J., Servat, E., Fritsch, J.-M., Ardoin-Bardin, S., and Thivet, G., 2013. Current state of Mediterranean water resources and future trends under climatic and anthropogenic changes. Hydrological Sciences Journal, 58 (3), 498–518.

Using general circulation model outputs to assess impacts of climate change on runoff for large hydrological catchments in West Africa

Abstract The problem of using data outputs from general circulation models (GCMs) to assess the impacts of climate change on runoff in West Africa is addressed. The annual and monthly precipitation data from four GCMs used in the Third Assessment Report of the IPCC were studied over the 1950–1998 period: the CSIRO-Mk2, ECHAM4, HadCM3 and NCAR-PCM models. Two weaknesses common to all these models are their inability to reproduce rainfall volumes in the Sahelian zone, and their difficulty in simulating the seasonal dynamics of rainfall in the Guinean zone. Two climate scenarios were then developed based on the changes predicted by the HadCM3-A2 model, which aimed to generate time series for rainfall and potential evapotranspiration up to the end of the 21st century, in order to simulate probable future climatic conditions. These scenarios were used as input to the hydrological model GR2M to assess the impacts of climate change on the discharge of four main rivers: the Senegal, the Gambia, the Sassandra and the Chari. The results show that the possible future changes in runoff are highly dependent on rainfall and, hence, on the quality of the output of a given GCM.