在东南太平洋中度的亚热带和亚南极洲水源的轨道调制
Jérôme Kaiser1, Enno Schefuß2, James Collins3,4
1Leibniz Institute for Baltic Sea Research Warnemünde, Rostock, Germany. jerome.kaiser@io-warnemuende.de.
Nature communications
|August 29, 2024
概括
智利过去的降雨模式显示了5万年来水分来源和数量的变化. 轨道周期影响了降水,影响了气候动态,揭示了关键的水气候驱动因素.
科学领域:
- 古气候学 古气候学
- 水气候的动力学
- 同位素地球化学 同位素地球化学
背景情况:
- 了解过去的降雨变化和水分来源对于预测未来的气候至关重要.
- 海洋沉积物核心为重建古气候条件提供了宝贵的档案.
研究的目的:
- 重建雨量变化和识别智利过去5万年的水分来源.
- 调查轨道周期对该地区水气候动态的影响.
主要方法:
- 分析陆地植物叶中的 (同位素) 含量.
- 在智利沿海获取的两个海洋沉积物核心的检查.
- 沉积物核心的年代测定,以确定环境变化的时间表.
主要成果:
- 重建的记录显示,在前cession最大值期间,智利中部的湿度增加.
- 智利南部表现出降雨的斜度调制,这表明不同的轨道影响.
- 南西风被认为是智利南部的主要水分来源.
- 亚热带地区作为一个额外的湿度来源,为智利中部在前行最大期间,由强化的亚热带喷气驱动.
结论:
- 湿度来源和降雨量轨道调节显著解释了过去的水气候变化.
- 这些发现澄清了智利中南部最后一次冰川潮湿最大值和早期Holocene潮湿最小值背后的机制.
- 这项研究增强了我们对该地区长期气候变化及其驱动因素的理解.
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