大西洋水温升高,格陵兰东北部最后一个浮动冰舌下面融化
Claudia Wekerle1, Rebecca McPherson2, Wilken-Jon von Appen2
1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany. claudia.wekerle@awi.de.
Nature communications
|February 20, 2024
概括
格陵兰岛 - 格陵兰岛是什么?
科学领域:
- 冰川学的冰川学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 格陵兰岛的79北冰川 (79NG) 拥有最大的浮动冰舌.
- 观察结果显示79NG冰舌从下面显著变薄.
- 海洋变暖和海底冰川下放量的增加都会导致基底融化,但主要的驱动因素尚不清楚.
研究的目的:
- 解开海洋变暖和大气变暖对79NG基底融化的影响.
- 确定过去50年基础融的年间变化的主要驱动因素.
主要方法:
- 利用具有700米分辨率的全球模拟来明确模拟海洋循环.
- 分析了冰舌腔内的海洋循环.
- 追溯了大西洋中间水流入东北格陵兰大陆架的起源.
主要成果:
- 该研究发现,基底融的年间变化主要与大西洋中间水流入温度的变化有关.
- 这一流入源于东部的弗拉姆海峡.
- 在弗拉姆海峡的变化和79NG基底融化之间发现了3年的滞后.
结论:
- 大西洋中间水温的变化是79NG基础变性的主要驱动因素.
- 海洋变暖,特别是通过大西洋中间水,在79NG的稀释中起着至关重要的作用.
- 了解这些海洋学联系对于预测格陵兰岛未来的冰损失至关重要.
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