But scientists increasingly attribute much of the observed grounding line retreat — particularly in West Antarctica — to the influence of
warmer ocean water seeping beneath the ice shelves and lapping against the bases of glaciers, melting the ice from the bottom up.
But scientists increasingly attribute much of the observed grounding line retreat — particularly in West Antarctica — to the influence of
warmer ocean water seeping beneath the ice shelves and lapping against the bases of glaciers, melting the ice from the bottom up.
Not exact matches
Their mission: find vulnerabilities where
warmer (but still near freezing)
water from the deep
ocean may be
seeping in under the ice shelf and melting it from below.