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Home All issues Volume 7 (2010) Climatologie, 7 (2010) 39-55 References
Open Access
Issue
Climatologie
Volume 7, 2010
Page(s) 39 - 55
DOI https://doi.org/10.4267/climatologie.445
Published online 09 October 2015
  • Bechtold P., Bazile E., Guichard F., Mascart P. et Richard E., 2001 : A mass flux convection scheme for regional and global models. Quaterly J. Roy. Meteor. Soc., 127, 869–886. [CrossRef] [Google Scholar]
  • Bigot S., Brou Y. T., Oszwald J. et Diedhiou A., 2005 : Facteurs de la variabilité pluviométrique en Côte d’Ivoire et relations avec certaines modifications environnementales. Sécheresse, 5, 5–13. [Google Scholar]
  • Brasseur O., Tricot C., Ntezimana V., Gallee H. et Schayes G., 1998 : Importance of the convective adjustment scheme in the simulation of the diurnal convective activity in Africa. Conference on tropical climatology, meteorology and hydrology, 18, 299–312. [Google Scholar]
  • Brasseur O., 2001 : Development and application of a physical approach to estimating wind gusts. Monthly Weather Review, 129, 5–25. [CrossRef] [Google Scholar]
  • Charney J. G., 1975 : Dynamics of desert and drought in the Sahel. Quaterly J. Roy. Meteor. Soc., 101, 193–202. [CrossRef] [Google Scholar]
  • De Ridder K. et Schayes G., 1997 : The IAGL land surface model. J. Appl. Meteor., 36, 167–182. [CrossRef] [Google Scholar]
  • De Ridder K. etSchayes G., 1998 : Land surface-induced regional climate change in Southern Israel. J. Appl. Meteor., 37, 1470–1485. [CrossRef] [Google Scholar]
  • Dhonneur G., 1971 : General circulation and types of weather over Western and Central Africa. GARPGATE Annex-IV, GARPGATE 23 Design, 22 pages. [Google Scholar]
  • Fontaine B. et Janicot S., 1996 : Sea Surface Temperature fields associated with West African rainfall anomaly types. J. Climate, 11, 2935–2940. [CrossRef] [Google Scholar]
  • Fouquart Y. et Bonnel B., 1980 : Computation of the solar heating of the Earth’s atmosphere: A new parametrization. Beitr. Phys. Atmos., 53, 35–62. [Google Scholar]
  • Gallee H. et Schayes G., 1994 : Development of a three-dimensional meso-gamma primitive equations model. Katabatic winds simulation in the area of Terra Nova Bay, Antarctica. Monthly Weather Review, 122, 671–685. [CrossRef] [Google Scholar]
  • Gallee H., 1995 : Simulation of the mesocyclonic activity in the Ross Sea, Antarctica. Monthly Weather Review, 123, 2051–2069. [CrossRef] [Google Scholar]
  • Gibson J. K., Kallberg P., Uppala S., Nomura A., Hernandez A. et serrano E., 1997 : ERA Description, ECMWF Re-Analysis Project Report Series, N°1, 72 pages. [Google Scholar]
  • Giorgi F. et Mearns L. O., 1999 : Introduction to special section: Regional climate modelling revisited. J. Geophys. Res., 104, 6335–6352. [CrossRef] [Google Scholar]
  • Gowing J., 2003 : Food security for sub-Saharan Africa: does water scarcity limit the options? Land Use and Water Resources Research, 3, 2.1–2.7. [Google Scholar]
  • Hagemann S., Arpe K. et Bengtsson L., 2005 : Validation of the hydrological cycle of ERA-40. ERA-40 Project Report Series N°24, ECMWF, Shinfield Park (Reading, Angleterre), 42 pages. [Google Scholar]
  • Kessler E., 1969 : On the distribution and continuity of water substance in atmospheric circulations. American Meteorological Society Meteorol. Monogr., 10(32), 84 pages. [Google Scholar]
  • Lamb J. P., 1978 : Cases studies of tropical Atlantic surface circulation patterns during recent Sub-Saharan weather anomalies: 1967 and 1968. Monthly Weather Review, 106, 482–491. [CrossRef] [Google Scholar]
  • Lebel T., Delclaux F. et Polcher J., 2000 : From GCM scale to hydrological scales: Rainfall variability in West Africa. Stochastic Environmental Research and Risk Assessment, 14, 275–295. [CrossRef] [Google Scholar]
  • Lebel T., Diedhiou A. et Laurent H., 2003 : Seasonal cycle and interannual variability of the Sahelian rainfall at hydrological scales. J. Geophys. Res., 108, 8389–8392. [CrossRef] [Google Scholar]
  • Levkov L., Rockel B., Kapitza H. et Raschke E., 1992 : 3D mesoscale numerical studies of cirrus and stratus clouds by their time and space evolution. Contrib. Atmos. Phys., 65, 35–58. [Google Scholar]
  • Lim H. S. et Ho C. H., 2000 : Comparison of tropical rainfall between the observed GPCP data and the assimilation products of ECMWF, NCEP/NCAR, and NASA-GEOS-1. J. Meteor., 78, 661–672. [Google Scholar]
  • Marbaix P., Gallee H., Brasseur O. et Ypersele J. P., 2003 : Lateral boundary conditions in regional climate models: A details study of the relaxation procedure. Monthly Weather Review, 131, 461–479. [CrossRef] [Google Scholar]
  • Mathon V., Laurent H. et Lebel T., 2002 : Mesoscale convective system rainfall in the Sahel. J. Appl. Meteor., 41 (11), 1081–1092. [CrossRef] [Google Scholar]
  • Morcrette J., 1984 : Sur la paramétrisation du rayonnement dans les modèles de circulation générale atmosphérique. Thèse de doctorat, Université des Sciences et Technologies de Lille, 373 pages. [Google Scholar]
  • Moron V., Philippon N. et Fontaine B., 2004 : Simulation of West-African circulation monsoon in four atmospheric GCMs forced by prescribed SST. Journal of Geophysical Research, 108, D24105. [CrossRef] [Google Scholar]
  • Moustaoui M., Royer J. F. et Chauvin F., 2002 : African easterly wave activity in a variable resolution GCM. Climate Dynamics, 19(3), 289–301. [CrossRef] [Google Scholar]
  • New M. et Hulme M., 2000 : Representing twentieth-century space time climate variability. part II: Development of 1901–1996 monthly grids of terrestrial surface climate. J. Climate, 13, 2217–2238. [CrossRef] [Google Scholar]
  • Nicholson S. E., 1981 : Rainfall and atmospheric circulation during drought periods and wetter years in West Africa. Monthly Weather Review, 109, 2191–2208. [CrossRef] [Google Scholar]
  • Nicholson S. E., 1983 : Comments on the South Indian convergence zone and interannual rainfall variability over South Africa and the question of ENSO’s influence on Southern Africa. J. Climate, 6, 1463–1466. [CrossRef] [Google Scholar]
  • Palmer T. N., 1986 : The influence of the Atlantic, Pacific and Indian Oceans on Sahel rainfall. Nature, 322, 251–253. [CrossRef] [Google Scholar]
  • Paeth H. et Hense A., 2004 : SST versus Climate Change Signals in West African Rainfall: 20th-Century Variations and Future Projections. Earth and Environmental Science, 65(1–2), 179–208. [Google Scholar]
  • Paeth H. et Friederichs P., 2004 : Seasonality and time scales in the relationship between global SST and African rainfall. Climate Dynamics, 23, 815–837. [CrossRef] [Google Scholar]
  • Philippon N. et Fontaine B., 2002 : The relationship between the Sahelian and previous 2nd Guinean rainy seasons: a monsoon regulation by soil wetness? Annales Geophysicae, 20(4), 575–582. [CrossRef] [Google Scholar]
  • Poccard I. et Janicot S., 2004 : Comparison of rainfall structures between NCEP/NCAR reanalyses and observed data over tropical Africa. Climate Dynamics, 16, 897–915. [CrossRef] [Google Scholar]
  • Ramel R., 2005 : Impacts des processus de surface sur le climat en Afrique de l’Ouest. Thèse de doctorat, Université Joseph Fourier (Grenoble 1), 149 pages. [Google Scholar]
  • Rowell D. P., Folland C. K., Maskell K. et Ward M. N., 1995 : Variability of summer rainfall over tropical North Africa (1906–92): observation and modelling. Quaterly J. Roy. Meteor. Soc., 121, 669–700. [Google Scholar]
  • Saha K. R. et Saha S., 2001 : African monsoons. Part 1: Climatological structure and circulation. Mausam, 52, 479–510. [Google Scholar]
  • Schnitzler K. G., Knorr W., Latiff M., Bader J. et Zeng N., 2001 : Vegetation feedback on Sahelian rainfall variability in a coupled climate land-vegetation model. Max Planck Inst. F. Meteoro, Report N°329, 13 pages. [Google Scholar]
  • Semazzi F. H. M., Lin Y. L. et Giorgi F., 1993 : A nested model study of the Sahelian climate response to sea-surface temperature anomalies. Geoph. Res. Lett., 20, 2897–2990. [CrossRef] [Google Scholar]
  • Simmons A. J. et Gibson J. K., 2000 : The ERA-40 Project Plan. ERA-40 Project Report Series N°1, ECMWF, Shinfield Park (Reading, Angleterre), 62 pages. [Google Scholar]
  • Simmons A. J., Jones P. D., Da Costa Bechtold V., Beljaars A. C. M., Kallberg P. W., Saarinen S., Uppala S. M., Viterbo P. et Wedi N., 2004 : Comparison of trends and low-frequency variability in CRU, ERA-40, and NCEP/NCAR analyses of surface air temperature. J. Geophys. Res., 109, D24115. doi:10.1029/2004JD005306. [CrossRef] [Google Scholar]
  • Sud Y. C. et Molod A., 1988 : A GCM simulation study of the influence of Saharan evapotranspiration and surface-albedo anomalies on July circulation and rainfall. Monthly Weather Review, 116, 2388–2400. [CrossRef] [Google Scholar]
  • Sultan B. et Janicot S., 2000 : Abrupt shift of the ITCZ over West Africa and intra-seasonal variability. Geoph. Res. Lett., 27, 3353–3356. [CrossRef] [Google Scholar]
  • Tippett M. K. et Giannini A., 2006 : Potentially predictable components of African summer rainfall in an SST-forced GCM simulation. J. Climate, 13, 3133–3144. [CrossRef] [Google Scholar]
  • Vizy R. K. et Cook K. H., 2001 : Mechanisms by which Gulf Guinea and Eartern North Atlantic sea surface temperature anomalies can influence African rainfall. J. Climate, 14, 795–821. [CrossRef] [Google Scholar]
  • Vizy R. K. et Cook K. H., 2002 : Development and application of a meso-scale climate model for the tropics: Influence of sea surface temperature anomalies on the West African monsoons. J. Geophys. Res., 107 (D3), ACL 2.1–2.22. [CrossRef] [Google Scholar]
  • Wang G. et Eltahir E. A. B., 2000 : Role of vegetation dynamics in enhancing the low-frequency variability of the Sahel rainfall. Water Resources Research, 36, 1013–1021. [CrossRef] [Google Scholar]
  • Xue Y. et Shukla J. , 1993 : The influence of land surface properties on Sahel climate. Part I: desertification. Journal of Climate, 6, 2232–2245. [CrossRef] [Google Scholar]
  • Zheng X. et Eltahir E. A. B., 1998 : The role of vegetation in the dynamics of West African monsoons. Journal of Climate, 11, 2078–2096. [CrossRef] [Google Scholar]

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