增强的冰下排放放大了彼得曼冰架融化,当海洋热力强迫和时
Abhay Prakash1,2, Qin Zhou3, Tore Hattermann4,5
1Department of Physical Geography, Stockholm University, Stockholm, Sweden. abhay.prakash@natgeo.su.se.
Nature communications
|May 6, 2025
概括
大气变暖通过加剧海洋驱动的过程,放大了冰架基底融化. 排放驱动的电流增强了混合,显著增加了融化,特别是在基底通道.
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:
- 皮特曼冰架的基底融化主要与海洋温度上升有关.
- 亚冰川排放在加剧基底融化的作用及其气候变化影响尚未完全理解.
研究的目的:
- 调查子冰层排放影响彼得曼冰架基底融化的机制.
- 为了确定这些机制在气候变暖下如何演变.
主要方法:
- 使用了一个3D数值区域冰架-海洋模型.
- 将模型集中在彼得曼峡湾地区.
- 模拟了各种排放速度和海洋温度场景.
主要成果:
- 确定了当排放超过当前夏季峰值水平时,冰架腔内热流效率的制度转变.
- 排放强化的电流和热驱动,并通过增加流混合来增强化.
- 融率在基底通道峰处是最高的,这是由于融水的汇合放大了摩擦速度.
结论:
- 大气变暖加剧了海洋驱动的融化过程,在扩大未来的基础融化中发挥了关键作用.
- 基底融化的增加不仅仅是由于海洋变暖,而且受到大气变暖驱动的排放加剧的影响.
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