热带海洋季节性温度变化的降冰增长
Lars Wörmer1, Jenny Wendt2, Brenna Boehman2,3
1MARUM - Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, Bremen, Germany. lwoermer@marum.de.
Nature
|November 30, 2022
概括
年轻干旱的终结没有改变热带大西洋海面温度 (SST). 然而,海洋的季节性和跨年变化显著增加,影响了各大洲的气候.
科学领域:
- 古气候学
- 海洋学
- 气候科学
背景情况:
- 从年轻干旱期 (YD) 过渡到全新纪,北半球突然变暖.
- 这种转变对低度海洋温度和气候变化的影响仍在争论中.
- 热带大西洋海面温度 (SST) 的变化对全球气候模式有重大影响.
研究的目的:
- 在YD-Holocene过渡期间重建热带大西洋SST变异性.
- 了解突然气候变化对亚年至十年海洋温度动态的影响.
- 评估热带大西洋SST对冰川间气候变化的敏感性.
主要方法:
- 在卡里亚科盆地沉积物中高分辨率 (100-μm) 质谱成像 (MSI).
- 分析沉积物核心以重建过去的海面温度和变化.
- 量化SST的季节性和跨年变化.
主要成果:
- 在 YD-Holocene 过渡期间,热带大西洋的年平均 SST 保持稳定.
- 海洋的季节性增加了一倍,
- 年间的SST变化在Holocene早期加剧.
- 这些变化可能是由于热带融合区 (ITCZ) 的变化造成的.
结论:
- 亚十年热带大西洋的SST变化对突然的背景气候变化很敏感.
- 而不是每年的平均变化,而是在YD-Holocene过渡过程中增加了SST的季节性和跨年变化.
- 这些发现突显了地区对重大冰川间气候事件的复杂反应.
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