Articles | Volume 10, issue 3
Clim. Past, 10, 1165–1182, 2014
Clim. Past, 10, 1165–1182, 2014

Research article 18 Jun 2014

Research article | 18 Jun 2014

Impact of precession on the climate, vegetation and fire activity in southern Africa during MIS4

M.-N. Woillez1,2,3, G. Levavasseur4, A.-L. Daniau1, M. Kageyama5, D. H. Urrego1,2,3, M.-F. Sánchez-Goñi2, and V. Hanquiez1 M.-N. Woillez et al.
  • 1Centre National de la Recherche Scientifique (CNRS), Environnements et Paléocenvironements Océaniques et Continentaux (EPOC), Unité Mixte de Recherche, UMR5805, CNRS – Université Bordeaux 1, 33400 Talence, France
  • 2Ecole Pratique des Hautes Etudes (EPHE), EPOC, UMR 5805, 33400 Talence, France
  • 3CNRS, de la Préhistoire à l'Actuel: Culture, Environnement et Anthropologie (PACEA), UMR 5199, 33400 Talence, France
  • 4Institut Pierre Simon Laplace, Pôle de Modélisation du Climat, Université Pierre et Marie Curie, 4 Place Jussieu, Paris, France
  • 5LSCE/IPSL INSU, UMR 8212, CE Saclay, l'Orme des Merisiers, 91191 Gif-sur-Yvette Cedex, France

Abstract. The relationships between climate, vegetation and fires are a major subject of investigation in the context of climate change. In southern Africa, fire is known to play a crucial role in the existence of grasslands and Mediterranean-type biomes. Microcharcoal-based reconstructions of past fire activity in that region have shown a tight correlation between grass-fueled fires and the precessional cycle, with maximum fire activity during maxima of the climatic precession index. These changes have been interpreted as the result of changes in fuel load in response to precipitation changes in eastern southern Africa. Here we use the general circulation model IPSL_CM5A (Institut Pierre Simon Laplace Climate Model version 5A) and the dynamic vegetation model LPJ-LMfire to investigate the response of climate, vegetation and fire activity to precession changes in southern Africa during marine isotopic stage 4 (74–59 kyr BP). We perform two climatic simulations, for a maximum and minimum of the precession index, and use a statistical downscaling method to increase the spatial resolution of the IPSL_CM5A outputs over southern Africa and perform high-resolution simulations of the vegetation and fire activity. Our results show an anticorrelation between the northern and southern African monsoons in response to precession changes. A decrease of the precession climatic index leads to a precipitation decrease in the summer rainfall area of southern Africa. The drying of climate leads to a decrease of vegetation cover and fire activity. Our results are in qualitative agreement with data and confirm that fire activity in southern Africa during MIS4 is mainly driven by vegetation cover.