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Exploration of ocean currents beneath the 'Doomsday Glacier'

机译:“世界末日冰川”下的海洋电流探索

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For the first time, researchers have been able to obtain data from underneath Thwaites Glacier, also known as the "Doomsday Glacier". They find that the supply of warm water to the glacier is larger than previously thought, triggering concerns of faster melting and accelerating ice flow. With the help of the uncrewed submarine Ran that made its way under Thwaites glacier front, the researchers have made a number of new discoveries. Professor Karen Heywood of the University of East Anglia, UK, comments: "This was Ron's first venture to polar regions and her exploration of the waters under the ice shelf was much more successful than we had dared to hope. We plan to build on these exciting findings with further missions under the ice next year."The AUV has, among other things, measured the strength, temperature, salinity and oxygen content of the ocean currents that go under the glacier.Global sea level is affected by how much ice there is on land, and the biggest uncertainty in the forecasts is the future evolution of the West Antarctic Ice Sheet, says Anna Wahlin, professor of oceanography at the University of Gothenburg, Sweden, and lead author of the new study now published in Science Advances.
机译:首次,研究人员已经能够从地下冰川下面获得数据,也称为“世界末日冰​​川”。他们发现,冰川的温水供应大于先前认为,引发更快熔化和加速冰流的担忧。在未焊接的潜水艇的帮助下,在冰川前面的冰川前沿,研究人员已经做了一些新的发现。英国东安格利亚大学的Karen Heywood教授:“这是罗恩的第一个对极地地区的冒险,她对冰架下的水域探索比我们敢于希望更成功。我们计划在这些方面建立令人兴奋的调查结果与明年冰下的进一步任务。“AUV在其他方面,测量了在冰川下方的海洋电流的强度,温度,盐度和氧气含量受到那里有多少冰的影响在土地上,预测中最大的不确定性是西南极冰盖的未来演变,哥德兰堡大学,瑞典大学海洋教授安娜·沃阿林说,新学习的领导作者在科学进步上发表。

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    《International ocean systems 》 |2021年第3期| 11-12| 共2页
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