Collaborative Research: Totten Glacier System and the Marine Record of Cryosphere - Ocean Dynamics

该项目将调查东南极洲托滕冰川和莫斯科大学冰架的海洋部分。该系统至关重要，因为它排干了南极东部冰盖的八分之一，其体积相当于潜在海平面上升近 7 米，比整个南极西部冰盖还要大。这个几乎完全未被探索的地区是最大且了解最少的海洋冰川系统，并且可能不稳定。尽管对南极西部冰原的海洋系统进行了严格的审查，但人们对托滕冰川系统知之甚少。这项研究将大大补充该地区现有的微薄的海洋学和海洋地质学和地球物理学数据，并将显着促进对这一知之甚少的冰川系统及其对环境变化的潜在敏感反应的了解。独立的天基平台表明托滕系统的质量损失正在加速。最近对极光冰下盆地（该盆地包含南极洲最深的冰并流入托滕系统）的航空地球物理调查为测量的表面变化提供了冰下环境，并表明托滕冰川是至少两个先前冰流状况的最重要的排水通道。然而，人们对离岸环境的了解却少之又少。来自附近陆架/坡折处的有限物理海洋学数据表明，在明显通往托滕冰川的槽口厚厚的底层内存在改良的环极深水，这表明相对温暖的水可能流入冰下底部，这一过程被认为是导致西南极冰盖接地线退缩的原因。该项目将对该地区进行船基海洋地质和地球物理调查，并结合物理海洋学研究，以评估冰川系统的近期和长期行为及其与邻近海洋系统的关系。 这项工作将补充其他南极冰架的研究、南极半岛附近的海洋学研究以及正在进行的冰盖和其他海洋模型的开发。

This project will investigate the marine component of the Totten Glacier and Moscow University Ice Shelf, East Antarctica. This system is of critical importance because it drains one-eighth of the East Antarctic Ice Sheet and contains a volume equivalent to nearly 7 meters of potential sea level rise, greater than the entire West Antarctic Ice Sheet. This nearly completely unexplored region is the single largest and least understood marine glacial system that is potentially unstable. Despite intense scrutiny of marine based systems in the West Antarctic Ice Sheet, little is known about the Totten Glacier system. This study will add substantially to the meager oceanographic and marine geology and geophysics data available in this region, and will significantly advance understanding of this poorly understood glacial system and its potentially sensitive response to environmental change.Independent, space-based platforms indicate accelerating mass loss of the Totten system. Recent aerogeophysical surveys of the Aurora Subglacial Basin, which contains the deepest ice in Antarctica and drains into the Totten system, have provided the subglacial context for measured surface changes and show that the Totten Glacier has been the most significant drainage pathway for at least two previous ice flow regimes. However, the offshore context is far less understood. Limited physical oceanographic data from the nearby shelf/slope break indicate the presence of Modified Circumpolar Deep Water within a thick bottom layer at the mouth of a trough with apparent access to Totten Glacier, suggesting the possibility of sub-glacial bottom inflow of relatively warm water, a process considered to be responsible for West Antarctic Ice Sheet grounding line retreat. This project will conduct a ship-based marine geologic and geophysical survey of the region, combined with a physical oceanographic study, in order to evaluate both the recent and longer-term behavior of the glacial system and its relationship to the adjacent oceanographic system. This endeavor will complement studies of other Antarctic ice shelves, oceanographic studies near the Antarctic Peninsula, and ongoing development of ice sheet and other ocean models.