这种地形意味着，升温的海水可日益侵蚀固定于基岩的冰块，一旦所有连接基岩的冰块被消融，冰原将四处游动。
That topography means that warm water could progressively melt spots where ice is stuck to the rock, allowing it to flow more freely.
这种地形意味着，升温的海水可日益侵蚀固定于基岩的冰块，一旦所有连接基岩的冰块被消融，冰原将四处游动。
That topography means that warm water could progressively melt spots where ice is stuck to the rock, allowing it to flow more freely.
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