南极大陆架和冰架空洞的浴度测量来自环极重力异常和其他数据
Raphaelle Charrassin1,2, Romain Millan3, Eric Rignot1,2,4,5
1Department Earth System Science, University of California Irvine, Irvine, CA, 92697, USA.
Scientific reports
|January 8, 2025
概括
一项新的南极水位测量揭示了更深的低谷,增加了冰川对海洋变暖的脆弱性. 这一发现表明,由于冰川融化增加,南极洲的海平面上升预测可能会更高.
科学领域:
- 地质物理学和海洋学
- 冰层科学 冰层科学
- 南极研究南极研究
背景情况:
- 浴度测量对于理解温暖的环极深水入南极货架至关重要.
- 这种入侵导致冰架融化,接地线撤退,随后海平面上升.
- 对南极洲的现有浴度数据,特别是冰架空洞内的,是不完整的.
研究的目的:
- 创建一个新的,全面的南极洲的浴度.
- 将所有已知的冰架空洞和以前未测量的大陆架区域纳入其中.
- 为了更好地了解南极冰洋相互作用及其对海平面上升的影响.
主要方法:
- 进行了环极重力异常的3D反转.
- 数据受到南大洋国际水度图 (IBCSO) 的限制.
- 从BedMachine南极洲的测量和离散的海底数据 (地震,机器人探测器) 进行了整合.
主要成果:
- 创建了一个全面的南极浴度数据集.
- 鉴定出了以前未知的冰架空洞较厚的低谷,特别是在东南极洲.
- 这项研究揭示了大陆架底部和冰架空洞的更深处.
结论:
- 新地图上的低谷表明,南极冰川对海洋地下变暖的脆弱性增加了.
- 由于水温升高而增强的融化可能导致南极海平面上升的修订,更高的预测.
- 这项研究为气候模型和海平面上升评估提供了关键数据.
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