直接观察冰架基底裂中的融化,结和海洋循环
Peter Washam1,2, Justin D Lawrence3, Craig L Stevens4,5
1Department of Astronomy, Cornell University, Ithaca, NY, USA.
Science advances
|October 27, 2023
概括
在南极洲的基底裂.
科学领域:
- 海洋学 海洋学 海洋学
- 冰川学的冰川学
- 极地科学 极地科学
背景情况:
- 南极冰架接地区域的海洋条件对于冰盖质量平衡至关重要.
- 在这些偏远地区进行直接的海洋观测很少,这限制了对冰与海洋相互作用的理解.
研究的目的:
- 为了调查罗斯冰架接地区的基底裂内的细度海洋状况.
- 了解基底裂如何影响海洋循环和融化/结过程.
主要方法:
- 使用水下车辆进行详细的空间海洋学调查.
- 在罗斯冰架接地区域的基底裂内进行现场数据收集.
主要成果:
- 观察到微小的海洋变化导致裂内的不对称融化和结.
- 确定了由淡水释放和盐分排斥驱动的翻转循环.
- 检测到一个主导的通过流喷射直角的潮流.
结论:
- 底层裂显著影响海洋循环和混合在接地区域.
- 这些过程影响南极冰架的稳定性和质量平衡.
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