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Subglacial Lake CECs: Discovery and in situ survey of a privileged research site in West Antarctica

机译:冰河湖下的CEC:在南极西部的一个特权研究地点的发现和现场调查

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We report the discovery and on-the-ground radar mapping of a subglacial lake in Antarctica, that we have named Lake CECs (Centro de Estudios Cientificos) in honor of the institute we belong to. It is located in the central part of the West Antarctic Ice Sheet, right underneath the Institute Ice Stream and Minnesota Glacier ice divide, and has not experienced surface elevation changes during the last 10 years. The ratio between the area of the subglacial lake and that of its feeding basin is larger than those for either subglacial lakes Ellsworth or Whillans, and it has a depth comparable to that of Ellsworth and greater than that of Whillans. Its ice thickness is approximate to 600 m less than that over Ellsworth. The lake is very likely a system with long water residence time. The recent finding of microbial life in Lake Whillans emphasizes the potential of Subglacial Lake CECs for biological exploration.
机译:我们报告了南极洲冰下湖泊的发现和地面雷达测绘,我们将其命名为Lake CEC(Centro de Estudios Cientificos),以纪念我们所属的研究所。它位于南极西部冰盖的中部,就在研究所冰河和明尼苏达州冰川冰分界线的正下方,并且在过去十年中没有经历过海拔高度变化。冰河下湖面积与其食盆面积之比大于冰河下湖泊埃尔斯沃思或惠兰山脉的面积之比,其深度可与埃尔斯沃斯媲美,且大于韦兰斯。它的冰厚度比Ellsworth上的冰厚度小约600 m。该湖很可能是水停留时间长的系统。威兰斯湖微生物生活的最新发现强调了冰下湖CEC在生物勘探中的潜力。

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