Relatively warm salty water is pushed upwards by ocean currents moving over a ridge in the Weddell sea.
Not exact matches
A very cold but
relatively fresh
water layer covers a much
warmer and
saltier water mass, thus acting as an insulating layer,» explains Prof. Dr. Mojib Latif, head of the Research Division at GEOMAR.
The incoming
water, part of the global conveyor belt of currents circulating throughout the oceans, is
relatively warm and
salty compared with the rest of the Southern Ocean.
That
water is
relatively warm and
salty compared with other
water in the ocean, so researchers could map its path upward and around Antarctica.
Velicogna and her colleagues also measured a dramatic loss of Greenland ice, as much as 38 cubic miles per year between 2002 and 2005 — even more troubling, given that an influx of fresh melt
water into the
salty North Atlantic could in theory shut off the system of ocean currents that keep Europe
relatively warm.
This circumpolar deep
water, which is
relatively warm and
salty compared to other parts of the Southern Ocean, has
warmed and shoaled in recent decades, and can melt ice at the base of glaciers which reduces friction and allows them to flow more freely.