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罗斯冰

罗斯冰

罗斯冰

罗斯冰

1

THAT THE AREA of the West Antarctic ice sheet drained by the Ross ice streams is in less danger of imminent collapse is good news.

南极洲西部冰原被罗斯冰流带走的面积，还没有到达立即崩解的地步，这可是一项好消息；

2

By the time the Marsh joins the immense Nimrod Glacier , some 35 miles from our camp , the ice is on a rapid charge to the Ross Sea Ice Shelf .

待马什冰川汇合入庞大的尼姆罗德冰川后（距我们的营地约 35 英里处），冰层快速冲向罗斯冰架。

4

The lakes are under moving sections of ice , called ice streams, that flow into the Ross Ice Shelf .

这些湖泊在冰流的下面，冰流是移动的冰层，流向 “罗斯冰架 ”。

5

More than 180 kilometers [112 miles] long , the glacier flows down from the polar plateau (left ) to the Ross Ice Shelf (right ).

它超过 180 公里（112 英里）长，从极地高原（图的左边）一直流到罗斯冰架（图的右边）。

6

Melt pools on the Ross Ice Shelf .

罗斯冰架（RossIceShelf ）上的融冰池。

7

The B9 iceberg broke from the Ross Ice Shelf in West Antarctica some time in 1987 .

B9 冰山是在 1987年从西南级大陆的罗斯冰架断裂而形成的。

8

These realizations left wide open the possibility of swift drainage along the Ross ice streams .

这些认知让研究人员更加怀疑罗斯冰流会使冰原快速消失。

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