Met Office Hadley Centre, Met Office, Fitzroy Road, Exeter, Devon EX1 3PB, UK.
Department of Physical Geography, University of Exeter, Peter Lanyon Building, Penryn Campus, Trelevier Road, Penryn, Cornwall TR10 9FE, UK.
Nat Commun. 2017 May 25;8:14966. doi: 10.1038/ncomms14966.
Summer rainfall in the Sahel region of Africa exhibits one of the largest signals of climatic variability and with a population reliant on agricultural productivity, the Sahel is particularly vulnerable to major droughts such as occurred in the 1970s and 1980s. Rainfall levels have subsequently recovered, but future projections remain uncertain. Here we show that Sahel rainfall is skilfully predicted on inter-annual and multi-year (that is, >5 years) timescales and use these predictions to better understand the driving mechanisms. Moisture budget analysis indicates that on multi-year timescales, a warmer north Atlantic and Mediterranean enhance Sahel rainfall through increased meridional convergence of low-level, externally sourced moisture. In contrast, year-to-year rainfall levels are largely determined by the recycling rate of local moisture, regulated by planetary circulation patterns associated with the El Niño-Southern Oscillation. Our findings aid improved understanding and forecasting of Sahel drought, paramount for successful adaptation strategies in a changing climate.
非洲萨赫勒地区的夏季降雨表现出气候变化最大的信号之一,由于该地区的人口依赖农业生产力,因此特别容易受到像 20 世纪 70 年代和 80 年代那样的严重干旱的影响。此后,降雨量已经恢复,但未来的预测仍然不确定。在这里,我们表明,萨赫勒地区的降雨在年际和多年(即> 5 年)时间尺度上可以得到很好的预测,并利用这些预测来更好地了解驱动机制。水汽收支分析表明,在多年时间尺度上,北大西洋和地中海变暖通过增加低层外部来源水汽的经向辐合来增强萨赫勒地区的降雨。相比之下,年际降雨水平主要取决于本地水汽的循环率,这由与厄尔尼诺-南方涛动相关的行星环流模式调节。我们的研究结果有助于更好地理解和预测萨赫勒地区的干旱,这对于在气候变化背景下成功实施适应战略至关重要。