Such accelerated flow leads to increased
ice discharge into the ocean, but the relevant dynamical processes are not properly understood nor included in continental ice - sheet models, the main difficulty being the treatment of grounding - line migration in response to increased melting of ice by the ocean.
«Konrad and colleagues have extended a method that has promise for future monitoring of
ice discharge into the ocean on a continent - wide scale,» Ryan Walker, a NASA ice researcher, wrote in an accompanying review piece.
The melting of a rather small ice volume on East Antarctica's shore could trigger a persistent
ice discharge into the ocean, resulting in unstoppable sea - level rise for thousands of years to come.
Not exact matches
The cracking of the
ice or the falling of pieces
into the sea makes a noise like breakers or a distant
discharge of guns, which may often be heard a short distance.
Studying surging glaciers could also offer insights
into grander - scale
ice flows with global consequences: the movements of the
ice sheets in Antarctica and Greenland, which can change abruptly, altering the
ice discharges that affect sea level.
Dr Gudmundsson said: «Although floating
ice shelves have only a modest impact on of sea - level rise,
ice from Antarctica's interior can
discharge into the ocean when they collapse.
For scientific purposes, the Antarctic
ice sheet is often divided
into catchment basins so that comparative measurements can be taken to work out how the
ice in each basin is changing and
discharging ice to the oceans.
A new NASA - led study has discovered an intriguing link between sea
ice conditions and the melting rate of Totten Glacier, the glacier in East Antarctica that
discharges the most
ice into the ocean.
«If that happens, the glacier's flow could be significantly destabilized, causing it to
discharge even more
ice into the ocean,» he said.
It currently
discharges enough
ice into the surrounding ocean to fill Lake Erie in just over a week.
Writing in Nature Climate Change, two scientists from the Potsdam Institute for Climate Impact Research (PIK) say the melting of quite a small volume of
ice on the East Antarctic shore could ultimately trigger a
discharge of
ice into the ocean which would result in unstoppable sea - level rise for thousands of years ahead.
More back - of - the - napkin trivia — two trillion tons of
ice over 5 years is roughly equivalent to the total
discharge of the Mackenzie River, which flows directly
into the Arctic basin, over a 6 year period (annual mean of ~ 10,000 cms).
The margins usually slope more steeply, and most
ice is
discharged through fast - flowing
ice streams or outlet glaciers, in some cases
into the sea or
into ice shelves floating on the sea.
Nearly all
ice shelves are in Antarctica, where most of the
ice discharged seaward flows
into ice shelves.
This «grounding line» is very important:
Ice that sits on terra firma is thicker than floating ice, and melting of this ice would discharge more liquid water into the s
Ice that sits on terra firma is thicker than floating
ice, and melting of this ice would discharge more liquid water into the s
ice, and melting of this
ice would discharge more liquid water into the s
ice would
discharge more liquid water
into the sea.
These approaches, however, haven't taken
into account some physical processes that can quickly increase
ice sheet
discharge, such as the collapse of terminal
ice cliffs and the breakup of floating
ice shelves caused by a process known as hydrofracturing.
Scientists have recently observed major changes in these glaciers: several have broken up at the ocean end (the terminus), and many have doubled the speed at which they are retreating.2, 5 This has meant a major increase in the amount of
ice and water they
discharge into the ocean, contributing to sea - level rise, which threatens low - lying populations.2, 3,5 Accelerated melting also adds freshwater to the oceans, altering ecosystems and changing ocean circulation and regional weather patterns.7 (See Greenland
ice sheet hotspot for more information.)
It is driven by poorly understood processes occurring at the
ice - ocean interface, such as subglacial
discharge into the ocean, turbulent plume dynamics, submarine melting, and iceberg calving.
These rapid changes are the result of increased
discharge from grounded
ice into the ocean and from increased
ice melting, which more than outweigh increases in surface accumulation.