Geosciences Institute, University of São Paulo, Rua do Lago 562, 05508-080, São Paulo, Brazil.
Andaluz Institute of Earth Sciences, CSIC-University of Granada, Granada, Spain.
Sci Rep. 2019 Feb 8;9(1):1698. doi: 10.1038/s41598-018-38003-6.
Recent paleoclimatic studies suggest that changes in the tropical rainbelt across the Atlantic Ocean during the past two millennia are linked to a latitudinal shift of the Intertropical Convergence Zone (ITCZ) driven by the Northern Hemisphere (NH) climate. However, little is known regarding other potential drivers that can affect tropical Atlantic rainfall, mainly due to the scarcity of adequate and high-resolution records. In this study, we fill this gap by reconstructing precipitation changes in Northeastern Brazil during the last 2,300 years from a high-resolution lake record of hydrogen isotope compositions of plant waxes. We find that regional precipitation along the coastal area of South America was not solely governed by north-south displacements of the ITCZ due to changes in NH climate, but also by the contraction and expansion of the tropical rainbelt due to variations in sea surface temperature and southeast trade winds in the tropical South Atlantic Basin.
最近的古气候研究表明,过去两千年中大西洋热带雨带的变化与北半球气候驱动的热带辐合带(ITCZ)纬向位移有关。然而,由于缺乏足够和高分辨率的记录,对于可能影响热带大西洋降雨的其他潜在驱动因素知之甚少。在这项研究中,我们通过重建过去 2300 年来自巴西东北部的高分辨率湖泊植物蜡氢同位素组成记录,填补了这一空白。我们发现,由于北半球气候的变化,导致 ITCZ 南北位移,南美洲沿海地区的区域降水并不是唯一的控制因素,热带雨带的收缩和扩张也受到热带南大西洋盆地海面温度和东南信风变化的影响。