Articles | Volume 383
https://doi.org/10.5194/piahs-383-61-2020
https://doi.org/10.5194/piahs-383-61-2020
Pre-conference publication
 | 
16 Sep 2020
Pre-conference publication |  | 16 Sep 2020

Study of the spatial and temporal variability of rainfall in the Middle and Lower Cheliff (Algeria)

Ali Hadour, Gil Mahé, and Mohamed Meddi

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Cited articles

Bodian, A.: Caractérisation de la variabilité temporelle récente des précipitations annuelles au Sénégal (Afrique de l'Ouest), Physio-Géo. Géographie physique et environnement, 8, 297–312, 2014. 
Boyer, J.-F.: Logiciel Khronostat d’analyse statistique de séries chronologiques. IRD UR2 Programme 21 FRIEND AOC, Equipe Hydrologie UMRGBE, Université de Montpellier II, Ecole des Mines de Paris, France, 1998. 
IPCC: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Solomon, S., Qin, D., Manning, M., Chen, Z., Marquis, M., Averyt, K. B., Tignor, M., and Miller, H. L., Cambridge University Press, Cambridge, UK and New York, NY, USA, 996 pp., 2007. 
IPCC: Climate Change 2014: Mitigation of Climate Change. Contribution of Working Group III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Edenhofer, O., Pichs-Madruga, R., Sokona, Y., Farahani, E., Kadner, S., Seyboth, K., Adler, A., Baum, I., Brunner, S., Eickemeier, P., Kriemann, B., Savolainen, J., Schlömer, S., von Stechow, C., Zwickel, T., and Minx, J. C., Cambridge University Press, Cambridge, UK and New York, NY, USA, 161 pp., 2014. 
Davis, J. C.: Statistics and Data Analysis in Geology, John Wiley and Sons, New York, USA, 656 pp., 1986. 
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Short summary
The downward of rainfall trend occurred in the study area in 1972, affecting a few coastal stations. In 1976, this decline extended to the South West and throughout the coastal region. In 1980, the drop covered the entire basin. This decline has resulted in an estimated deficit of 30 % on average in the eastern region, the coastal region and the Mina. However, the central part of the basin experienced a 20 % decrease compared to the period before the break (1968–1980).