Abstract
In order to test the sensitivity of the transitional phase of the 2006 West African monsoon (WAM) onset to different mechanisms, weather research and forecasting (WRF) model simulations have been carried out addressing the role of the Saharan heat low (SHL) and its sensitivity to the albedo field and to the northern Africa orography, and the role of the sea surface temperature (SST) in the eastern tropical Atlantic and Mediterranean. Lowering albedo over the desert region induces a northward location of the inter-tropical convergence zone (ITCZ), while removing mountains in North Africa reduces rainfall over West Africa. Shifting SST forward by 15 days leads to a northward location of the ITCZ before the WAM onset. However none of these factors modifies the timing of the WAM onset in 2006. The transitional phase of the 2006 WAM onset has been examined in more detail. The enhancement of SHL intensity, combined with the development of the oceanic cold tongue in the Guinea gulf, leads to low-level moisture flux divergence in the ITCZ reducing rainfall and increasing low-level humidity over the Sahel. However, weakening of convection can be clearly attributed to dry-air intrusions in mid-levels, originating from the subtropical westerly jet and associated with Rossby wave pattern over North Africa. Sensitivity tests on the synoptic scale forcing outside of the WRF model domain confirm the dominating role of large-scale dynamics to control the transitional phase of the WAM onset and its timing. However it is shown that the regional factors can modulate this larger scale forcing.
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig1_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig2_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig3_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig4_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig5_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig6_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig7_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig8_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig9_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig10_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig11_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig12_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig13_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig14_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig15_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs00382-011-1255-2/MediaObjects/382_2011_1255_Fig16_HTML.gif)
Similar content being viewed by others
References
Brandt P, Caniaux G, Bourles B, Lazar A, Dengler M, Funk A, Hormann V, Giordani H, Marin F (2011) Equatorial upper-ocean dynamics and their interaction with the West African monsoon. Atmos Sci Lett. doi:10.1002/asl.287
Caniaux G, Giordani H, Redelsperger JL, Guichard F, Key E, Wade M (2011) Coupling between the Atlantic cold tongue and the West African monsoon in boreal spring and summer. J Geophys Res. 116, C04003. doi:10.1029/2010JC006570
Chauvin F, Roehrig R, Lafore JP (2010) Intraseasonal variability of the Saharan heat low and its link with midlatitudes. J Clim 23:2544–2561
Coëtlogon G, Janicot S, Lazar A (2010) Intraseasonal variability of the ocean-atmosphere coupling in the Gulf of Guinea during boreal spring and summer. Quart J Roy Meteor Soc. doi:10.1002/qj.554
Drobinski P, Sultan B, Janicot S (2005) Role of the Hoggar massif in the West African monsoon onset. Geophys Res Lett 32:L01705. doi:10.1029/2004GL020710
Drobinski P, Bastin S, Janicot S, Dabas A, Delville P, Reitebuch O (2009) On the late northward propagation of the West African monsoon in summer 2006 in the region of Niger/Mali. J Geophys Res 114:D09108. doi:10.1029/2008JD011159
Eltahir EAB, Gong C (1996) Dynamics of wet and dry years in West Africa. J Clim 9:1030–1042
Flaounas E, Bastin S, Janicot S (2011) Regional climate modelling of the 2006 West African monsoon: sensitivity to convection and planetary boundary layer parameterisation using WRF. Clim Dyn. doi:10.1007/s00382-010-0785-3
Fontaine B, Louvet S (2006) Sudan-Sahel rainfall onset: definition of an objective index, types of years, and experimental hindcasts. J Geophys Res 111:D20103. doi:10.1029/2005JD007019
Fontaine B, Philippon N, Camberlin P (1999) An improvement of June–September rainfall forecasting in the Sahel based upon region April–May moist static energy content (1968–1997). Geophys Res Lett 26(14):2041–2044. doi:10.1029/1999GL900495
Fontaine B, Louvet S, Roucou P (2008) Definition and predictability of an OLR-based West African monsoon onset. Int J Climatol 28:1787–1798
Fontaine B, Garcia-Serrano J, Roucou P, Rodriguez-Fonseca B, Losada T, Chauvin F, Gervois S, Sivarajan S, Ruti P, Janicot S (2009) Impacts of warm and cold situations in the Mediterranean Basins on the West African monsoon: observed connection patterns (1979–2006) and climate simulations. Clim Dyn. doi:10.1007/s00382-009-0599-3
Gallee H, Moufouma-Okia W, Bechtold P, Brasseur O, Dupays I, Marbaix P, Messager C, Ramel R, Lebel T (2004) A high-resolution simulation of a West African rainy season using a regional climate model. J Geophys Res. 109. doi:10.1029/2003JD004,020
Gazeaux J, Flaounas E, Naveau P, Hannart A (2011) Inferring change points and nonlinear trends in multivariate time series: application to West African monsoon onset timings estimation. J Geophys Res. doi:10.1029/2010JD014723
Hagos SM, Cook KH (2007) Dynamics of the West African monsoon jump. J Clim 20:5264–5284
Holton JR (2004) An introduction to dynamic meteorology. Academic Press, London 535
Hoskins BJ, McIntyre ME, Robertson AW (1985) On the use and significance of isentropic potential vorticity maps. Quart J R Meteor Soc 111:877–946
Huffman GJ, Adler RF, Morrissey MM, Curtis S, Joyce R, McGavock B, Susskind J (2000) Global precipitation at 1 degree daily resolution from multi-satellite observations. J Hydrometeorol 2:36–50
Janicot S, Thorncroft C et al (2008) Large scale overview of the summer monsoon over the summer monsoon in West Africa during the AMMA field experiment in 2006. Ann Geophys 26:2569–2595
Janicot S, Mounier F, Hall NMJ, Leroux S, Sultan B, Kiladis GN (2009) Dynamics of the West African Monsoon. Part IV: analysis of 25–90-day variability of convection and the role of the Indian Monsoon. J Clim 22:1541–1565
Janicot S, Mounier F, Gervois S, Sultan S, Kiladis G (2010) The dynamics of the West African monsoon. Part V: the role of convectively coupled equatorial Rossby waves. J Clim 23:4005–4024
Jung T, Ferranti L, Tompkins AM (2006) Response to the summer 2003 Mediterranean SST anomalies over Europe and Africa. J Clim 19:5439–5454
Kain JS (2004) The Kain–Fritsch convective parameterization: an update. J Appl Meteorol 43:170–181
Klemp JB, Skamarock WC, Dudhia J (2007) Conservative split-explicit time integration methods for the compressible nonhydrostatic equations. Mon Weather Rev 135:2897–10519
Kummerow C, Barnes W, Kozu T, Shiue J, Simpson J (1998) The tropical rainfall measuring mission (TRMM) sensor package. J Atmos Ocean Technol 15:809–817
Laing AG, Fritsch JM (2000) The large-scale environments of the global populations of mesoscale convective complexes. Mon Weather Rev 128:2756–2776
Lavaysse C, Flamant C, Janicot S, Parker DJ, Lafore JP, Sultan B, Pelon J (2009) Seasonal evolution of the West African heat low: a climatological perspective. Clim Dyn. doi:10.1007/s00382-009-0553-4
Lavaysse C, Flamant C, Janicot S, Knippertz P (2010) Links between African easterly waves, mid-latitude circulation and the intra seasonal pulsations of the West African heat low. Quart J R Meteorol Soc 136:141–156. doi:10.1002/qj.555
Lavender SL, Matthews AJ (2009) Response of the West African monsoon to the Madden-Julian oscillation. J Clim 11:4097–4116
Le Barbé L, Lebel T, Tabsoba D (2002) Rainfall variability in West Africa during the years 1950–1990. J Clim 15:187–202
Louvet S, Fontaine B, Roucou P (2003) Active phases and pauses during the installation of the West African monsoon through 5-day CMAP rainfall data (1979–2001). Geophys Res Lett 30:2271–2275. doi:10.1029/2003GL018058
Lu J (2009) The dynamics of the Indian Ocean sea surface temperature forcing of Sahel drought. Clim Dyn 33:445–460
Matthews AJ (2004) Intraseasonal variability over tropical Africa during northern summer. J Clim 17:2427–2440
Mellor GL, Yamada T (1982) Development of a turbulence closure model for geophysical fluid problems. Rev Geophys 20:851–875
Okumura Y, **e SP (2004) Interaction of the Atlantic Equatorial cold tongue and the African Monsoon. J Clim 17:3589–3602
Parsons DB, Yoneyama K, Redelsperger JL (2000) The evolution of the tropical western Pacific atmosphere-ocean system following the arrival of a dry intrusion. Quart J R Meteor Soc 126:517–548
Peyrillé P, Lafore JP, Redelsperger JL (2007) An idealized two-dimensional framework to study the West African monsoon. Part I: validation and key controlling factors. J Atmos Sci 64:2765–2782
Pohl B, Janicot S, Fontaine B, Marteau R (2009) Implication of the Madden-Julian Oscillation in the 40-day variability of the West African monsoon, and associated rainfall anomalies. J Clim 22:3769–3785
Ramel R, Gallee H, Messager C (2006) On the northward shift of the West African monsoon. Clim Dyn 26. doi:10.1007/s00,382-005-0093-5
Redelsperger JL, Thorncroft CD, Diedhiou A, Lebel T, Parker DJ, Polcher J (2006) African monsoon multidisciplinary analysis: an international research project and field campaign. Bull Am Met Soc 87:1739–1746
Roca R, Lafore JP, Piriou C, Redelsperger JL (2005) Extratropical dry-air intrusions into the West African monsoon midtroposphere: an important factor for the convective activity over the Sahel. J Atmos Sci 62:390–407
Rodwell MJ, Hoskins BJ (1996) Monsoons and the dynamics of deserts. Quart J R Meteorol Soc 122:1385–1404
Rowell DP (2003) The impact of Mediterranean SSTs on the Sahelian rainfall season. J Clim 16:849–862
Semazzi FH, Sun L (1997) The role of orography in determining the Sahelian climate. Int J Climatol 17:581–596
Sijikumar S, Roucou P, Fontaine B (2006) Monsoon onset over Sudan-Sahel:simulation by the regional scale model MM5. Geophys Res Lett 33:L03814. doi:10.1029/2005GL024819
Skamarock WC, Klemp JB (2008) A time-split nonhydrostatic atmospheric model for weather research and forecasting applications. J Comput Phys 227:3465–3485
Sultan B, Janicot S (2000) Abrupt shift of the ITCZ over West Africa and intra-seasonal variability. Geophys Res Lett 27:3353–3356
Sultan B, Janicot S (2003) The West African monsoon dynamics. Part II: the “preonset” and “onset” of the summer monsoon. J Clim 16:3389–3406
Sultan B, Baron C, Dingkuhn M, Sarr B, Janicot S (2005) Agricultural impacts of large-scale variability of the West African monsoon, agricultural and forest meteorology. doi: 10.1016/j.agrformet.2004.08.005
Thorncroft CD, Nguyen H, Zhang C, Peyrille P (2011) Annual cycle of the West African monsoon: regional circulations and associated water vapour transport. Q J R Meteorol Soc 137:129–147
Tomas RA, Webster PJ (1997) The role of inertial instability in determining the location and strength of near-equatorial convection. Quart J R Meteorol Soc 123:1445–1482
Vizy EK, Cook KH (2001) Mechanisms by which gulf of Guinea and eastern North Atlantic sea surface temperature anomalies can influence African rainfall. J Clim 14:795–821
Zheng X, Eltahir EAB, Emanuel KA (1999) A mechanism relating tropical Atlantic spring sea surface temperature and west African rainfall. Q J R Meteorol Soc 125:1129–1164
Acknowledgments
The authors are grateful for the help of Philippe Weill to install the model on the IPSL servers. We are also thankful to the Climate Diagnostics Center (NOAA, Boulder, CO) and to the NCEP for the OLR and Final Analyses (FNL) data. Finally we are grateful to all three reviewers for their constructive comments that contributed greatly to the improvement of this article. Based on French initiative, AMMA was built by an international scientific group and is currently funded by a large number of agencies, especially from France, UK, US and Africa. It has been the beneficiary of a major financial contribution from the European Community’s Sixth Framework Research Programme. Detailed information on scientific coordination and funding is available on the AMMA International website http://www.amma-international.org.
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Flaounas, E., Janicot, S., Bastin, S. et al. The West African monsoon onset in 2006: sensitivity to surface albedo, orography, SST and synoptic scale dry-air intrusions using WRF. Clim Dyn 38, 685–708 (2012). https://doi.org/10.1007/s00382-011-1255-2
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-011-1255-2