Regional Consultation Meeting Climate Change Impacts in the Arab Region: Water Scarcity, Drought, and Population Mobility االجتماع التشاوري اإلقليمي " وتنقل السكان، والجفاف، ندرة المياه:"تأثيرات تغير المناخ في المنطقة العربية 15-16 September 2010 ٢٠١٠أيلول/سبتمبر16-15 سوريا،دمشقDamascus , Syria – WATER HARVESTING AND CC ADAPTATION IN THE DRY AREAS OF TUNISIA Dr. Mohamed OUESSAR Institut des Régions Arides (IRA) 4119 – Médenine – Tunisie Tél: 216-75633005; Fax: +216-75633006 Email: Med.Ouessar@ira.agrinet.tn • • • • • • • Introduction Basic principles Development Overview of WH in Tunisia CC in Tunisia WH & CC adaptation Conclusions & prospects The dry areas are characterized by: rainfall is rare, variable and torrential Insufficient to meet the basic needs for crop production, Poorly distributed over the growing season risky farming Runoff can cause erosion and be lost later by evaporation from swamps ‘salt sinks”, High temperature evapotranspiration Shallow and poor soils degradation, moisture stress desertification Dominating rainfed agriculture Depriving part of the land of its share of rain, which is usually small and non productive, and adding it to the share of another part in order to bring the available water amount closer to the water requirements of crops (Oweis et al., 2001) Collection area Reservoir Target area 200 150 mm Runoff harvesting – additional 35% of annual rainfall As long as the people have inhabited the dry areas and made cultivation, they have harvested water. In southern Jordan early WH structures are believed to have been constructed around 5000 years ago, Southern Mesopotamia: 4500 BC, Negev desert: 1000 BC, Yemen (Tihama): spreading system dating 1000 years BC Pakistan (Balauchistan): Khuskaba and salaiba systems Tunisia: Jessour, meskat and cisterns, Egypt (North west and Sina): wadi bed systems and cisterns, Moroccco, Syria, Iran, Oman, : Groundwater galleries (fouggara, falej, …). Ben Mechlia & Ouessar, 2004; Ouessar, 2007 1500 1000 750 500 400 300 200 100 200 Agro-ecological zones LEGENDS Cereals Forests Irrigation Fruit trees Rangelands Wadi 690 Altitude Sebkha 200 Isohyet 500000 700000 ME # # R E ER !@ # !@ A L G E R I A !@ # !. !@ Croppin g Area !. ! # !. !@ !. ± !@ ! ± ±# !. ±± ± !@ ± ! 3800000 !@ ! ! !. # !@ !@ !@ # ! ± ! !@ º' ! º' 400 100 !@ !@ # !@ A EA SE N S AN EA NE R RA N # Catchmen t D II TT !@ 4000000 300000 !@ ! !@ ± !@ ! ± 3600000 ! !@ ± Legend ! ! Flood spreading ! ± Jessour ! BB !@ Gabion check dams º' # µ Hill lake Recharge wells !. Large cistem ! Small to medium cistem ± A II A L Y Wadi Tabias Sebkha 0 30 60 Jessour 3400000 Meskat 120 Km Dike Minis. Agriculture, 2007 Temperature increase (in °C) for the 2020 (left) and 2050 (right) horizons. Average annual rainfall decrease (in %) for the 2020 (left) and 2050 (right) horizons. Snane et al., 1991 ETa in a Meskat system for different CCR and annual rainfall (green: 413 mm; Red: 290 mm) Nasri et al., 2004 400 with all tabias 350 without tabias harvested runoff in mm 300 250 200 150 100 50 0 0 10 20 30 40 50 rainfall in mm 60 70 80 90 100 Water balance in of jessour Hyd. Year Wet Dry Very dry ETrel (2/1) ETrel (3/1) ETrel (3/2) 1.1 2.3 2.5 1.1 12.0 15.6 1.3 Hyd. Year: type of the hydrological year ETrel: relative ETa 1: ETa with only rainfall on the terrace 2: ETa with rainfall and runoff on the terrace 3: ETa with rainfall, runoff and supplemental irrigation Schiettecatte et al., 2005; Ouessar, 2007; Ouessar et al. 2009 SC0 SC1 SC2 SC3 mm % mm % mm % mm % Rainfall 183.9 - 183.9 - 183.9 - 183.9 - ET 107.0a 58.2 147.2b 80.1 150.9 b 82.0 150.9 b 82.0 Outflow 34.3 a 18.7 4.0 b 2.2 Perco 14.5 a 7.9 24.3 b 13.2 TLOSS 28.0 a 15.2 8.2 b 4.4 3.1 c Seepage 0a 0.0 0a 0.0 1.1 b 0.1 c 0.0 0.1 c 0.0 28.2 b 15.4 28.3 b 15.4 1.7 3.2 c 1.7 0.6 0.9 b 0.5 100% 80% 60% Recharge SC0 40% Flowout ET 20% SC2 0% 100% VD VD D D D N N N N N W W W VW VW Year 80% SC2 60% Recharge Flowout ET 40% 20% 0% VD VD VD D D D D N N NN N N W W W W VWVW VW Sghaier et al., 2010 Water harvesting techniques have been developed since antiquity to cope with climate variability in the dry areas. They played major role in the development of rainfed agriculture in addition of providing other ecosystem services With the prospect of CC, those systems/techniques would be more useful. Therefore, they need to be well considered in the national/regional strategies for adaptation with CC. • Alaya, K., Viertmann, W., Waibel, Th. 1993. Les tabias. Imprimerie Arabe de Tunisie, Tunis, Tunisia. 192 pp. • Carton, D. 1888. Essai sur les travaux hydrauliques des Romains dans le Sud de la Régence de Tunis. Bulletin Archéologique du Comité des Travaux Historiques et Scientifiques, 438-465. • Chahbani, B. 1990. Contribution à l’étude de la destruction des jessour dans le sud tunisien. Revue des Régions Arides, 1: 137-172. • De Graaff, J., Ouessar, M. 2002 (eds). Water harvesting in Mediterranean zones: an impact assessment and economic evaluation. TRMP paper n°40, Wageningen University, The Netherlands. • Fleskens, L., Stroosnijder, L., Ouessar, M., De Graaff, J. 2005. Evaluation of the onsite impact of water harvesting in Southern Tunisia. Journal of Arid Environments, 62: 613-630. • Genin, D., Guillaume, H., Ouessar, M., Ouled Belgacem, A., Romagny, B., Sghaier, M., Taamallah, H. (eds) 2006. Entre la désertification et le développement : la Jeffara tunisienne. CERES, Tunis, 351 pp. • Nasri, S. 2002. Hydrological effects of water harvesting techniques. Ph.D. thesis, Lund University, Sweden, 104 pp. • Oweis, T., Hachum, A., Bruggeman, A. 2004. Indigenous water harvesting in West Asia and North Africa. ICARDA, Aleppo, Syria. • Ouessar M. 2007. Hydrological impacts of rainwater harvesting in wadi Oum Zessar watershed (southern Tunisia). Ph.D. thesis, Faculty of Bio-Engineering Sciences, Ghent University, Belgium, 154 pp. • El Amami, S. 1984. Les aménagements hydrauliques traditionnels en Tunisie. Centre de Recherche en Génie Rural (CRGR), Tunis, Tunisia. 69 pp. • Ennabli, N. 1993. Les aménagements hydrauliques et hydro-agricoles en Tunisie. 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