Multi-month memory effects on early summer vegetative activity in semi-arid South Africa and their spatial heterogeneity |
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| Authors: | Yves Richard Nadège Martiny Mathieu Rouault Nathalie Philippon Yann Tracol Thierry Castel |
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| Affiliation: | 1. Centre de Recherches de Climatologie , UMR 6282 Biogéosciences, CNRS/Université de Bourgogne , Dijon , France yves.richard@u-bourgogne.fr;3. Centre de Recherches de Climatologie , UMR 6282 Biogéosciences, CNRS/Université de Bourgogne , Dijon , France;4. Department of Oceanography , Mare Institute, University of Cape Town , Rondebosch , South Africa;5. Nansen-Tutu Centre for Marine Environmental Research , University of Cape Town , Rondebosch , South Africa;6. Centro de Estudios Avanzados en Zonas áridas (CEAZA) , La Serena , Chile;7. Alpine Ecosystems Research Centre (CREA) , Chamonix , France |
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| Abstract: | In semi-arid African regions (annual rainfall between 200 and 600 mm), variability of vegetative activity is mainly due to the rainfall of the current rainy season. In most of South Africa, the rainy season occurs from October to March. On average, vegetative activity lags rainfall by 1 to 2 months. The interannual variability in early summer (December to September) normalized difference vegetation index (NDVI) depends primarily on precipitation at the beginning (October to November) of the rainy season. However, once this primary control is removed, the residual interannual variability in NDVI highlights a double memory effect: a 1-year effect, referred to as Mem1, and a 7- to 10-month effect, referred to as Mem2. This article aims at better describing the influence of soil and vegetation characteristics on these two memory effects. The data sets used in this study are as follows: (1) a 19-year NDVI time series from National Oceanic and Atmospheric Administration (NOAA) satellites, (2) rainfall records from a network of 1160 rain-gauge stations compiled by the Water Research Commission (WRC), (3) vegetation types from Global Land Cover (GLC) 2000 and (4) soil characteristics from the soil and terrain database for Southern Africa (SOTERSAF). Results indicate that among 20–30% of NDVI variance that is not explained by the concurrent rainfall, one-third is explained by the two memory effects. Mem1 is found to have maximum effect in the northwest of our study domain, near the Botswana boundary, in the South Kalahari. Associated conditions are open grasslands growing on Arenosols. Mem1 is less important in the southeast, particularly in open grassland with shrubs growing on Cambisols. Thus, Mem1 mainly depends on soil texture. Mem2 is more widespread and its influence is the greatest in the centre, the south and the east of our domain. It is related to rainfall from January to April, which controls, beyond the intervening dry season, the interannual variations of NDVI (December to September) at the beginning of the next rainy season. Through these new findings, this article emphasizes again the high potential of remote-sensing techniques to monitor and understand the dynamics of semi-arid environments. |
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