海平面的冰川变化调节了东南亚秋季季风降雨的千年级变化
Elizabeth W Patterson1, Kathleen R Johnson1, Michael L Griffiths2
1Department of Earth System Science, University of California, Irvine, CA 92617.
概括
东南亚的古气候研究表明,海平面的变化对秋季季风的降雨有很大影响. 海平面下降导致了更干燥的条件,而海平面上升导致了突然的潮湿,影响了区域的水气候.
科学领域:
- 古气候学 古气候学
- 气候科学 气候科学
- 东南亚的水气候 东南亚的水气候
背景情况:
- 在东南亚古气候研究中,对非夏季季风季的关注有限.
- 越南中部的降雨主要发生在秋季 (9月至11月).
研究的目的:
- 为了重建过去45,000年越南中部秋季降雨的变化.
- 研究海平面和气候变化对这种水气候的影响.
主要方法:
- 从越南中部 (公元前45,0004,000年) 的多代理石记录分析.
- 气候模型模拟以评估海平面和融水强迫影响.
主要成果:
- 在最后一个冰川最大期期间,长期的干旱时期,随后在公元前14000年左右出现了突然的潮湿.
- 海平面的变化被确定为冰川轨道尺度秋季季风的变化的主要驱动因素.
- 千年规模的变化与海因里希体育场 (干) 和丹斯加尔德-奥什格尔事件 (湿) 相关.
- 海平面调节了千年级的湿/干阶段,特别是在低海平面期间.
结论:
- 海平面的变化对于了解东南亚秋季季风的动态至关重要.
- 大陆架的冰川暴露和随后的洪水大大改变了水分的传递.
- 融水对海面温度的影响影响了千年规模的水气候变化.
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