Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
Clim. Past, 9, 1417-1430, 2013
https://doi.org/10.5194/cp-9-1417-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
05 Jul 2013
Megalake Chad impact on climate and vegetation during the late Pliocene and the mid-Holocene
C. Contoux1,2, A. Jost2, G. Ramstein1, P. Sepulchre1, G. Krinner3, and M. Schuster4 1Laboratoire des Sciences du Climat et de l'Environnement/IPSL, UMR8212, CEA/CNRS/UVSQ – Gif-sur-Yvette Cedex, France
2Sisyphe, UPMC Paris 6/CNRS, Paris, France
3Laboratoire de Glaciologie et de Géophysique de l'Environnement, UJF-Grenoble1/CNRS, Grenoble, France
4Institut de Physique du Globe de Strasbourg, UMR7516, CNRS – Université de Strasbourg/EOST, 1 rue Blessig, 67084 Strasbourg Cedex, France
Abstract. Given the growing evidence for megalakes in the geological record, assessing their impact on climate and vegetation is important for the validation of palaeoclimate simulations and therefore the accuracy of model–data comparison in lacustrine environments. Megalake Chad (MLC) occurrences are documented not only for the mid-Holocene but also for the Mio-Pliocene (Schuster et al., 2009). At this time, the surface covered by water would have reached up to ~350 000 km2 (Ghienne et al., 2002; Schuster et al., 2005; Leblanc et al., 2006), making it an important evaporation source, possibly modifying climate and vegetation in the Chad Basin. We investigated the impact of such a giant continental water area in two different climatic backgrounds within the Paleoclimate Model Intercomparison Project phase 3 (PMIP3): the late Pliocene (3.3 to 3 Ma, i.e. the mid-Piacenzian warm period) and the mid-Holocene (6 kyr BP). In all simulations including MLC, precipitation is drastically reduced above the lake surface because deep convection is inhibited by overlying colder air. Meanwhile, convective activity is enhanced around MLC because of the wind increase generated by the flat surface of the megalake, transporting colder and moister air towards the eastern shore of the lake. The effect of MLC on precipitation and temperature is not sufficient to widely impact vegetation patterns. Nevertheless, tropical savanna is present in the Chad Basin in all climatic configurations, even without MLC presence, showing that the climate itself is the driver of favourable environments for sustainable hominid habitats.

Citation: Contoux, C., Jost, A., Ramstein, G., Sepulchre, P., Krinner, G., and Schuster, M.: Megalake Chad impact on climate and vegetation during the late Pliocene and the mid-Holocene, Clim. Past, 9, 1417-1430, https://doi.org/10.5194/cp-9-1417-2013, 2013.
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