罗斯冰架正面区域受到海洋表面水域日益增长的融化
Peter M F Sheehan1, Karen J Heywood1
1Centre of Oceanic and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, UK.
Science advances
|November 8, 2024
概括
温暖的地表水在南极洲的冰架下面因风而沉降,导致融化. 这一过程是由海洋热量增加所驱动的,几十年来一直在加剧,影响了海平面上升预测.
科学领域:
- 海洋学 海洋学 海洋学
- 冰川学的冰川学
- 气候科学 气候科学
背景情况:
- 太阳加热的地表水在南极冰架下沉没,这是一个观察不到的现象.
- 这种潜水过程的跨年变化及其对基底融的贡献仍未评估.
研究的目的:
- 观测和量化罗斯冰架下方温暖地表水的入侵.
- 为了评估热传输到冰架腔中的跨年变化.
- 了解基底融化的驱动因素及其对海平面上升的贡献.
主要方法:
- 在罗斯冰架下方直接观察50米厚的热水入.
- 分析温度概况以确定冰基的热量损失.
- 评估Ekman强迫和区域风应力以量化热传输.
主要成果:
- 在罗斯冰架下方观察到大量温暖的表面水的入侵.
- 由埃克曼强迫驱动的热传输到腔内,对基底融有相当大的贡献.
- 这种热传输在过去的40年里有所增加,与海洋热量含量上升有关.
结论:
- 太阳能加热的地表水的风力驱动的沉积是基础冰架融化的关键驱动因素.
- 海洋热量含量的增加加剧了这种融化过程,这对未来的海平面上升有影响.
- 这些发现为验证气候模型和减少海平面上升预测的不确定性提供了关键数据.
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