Not exact matches
A new study has found that the massive Laurentide ice sheet that covered Canada during the last ice age initially began shrinking through
calving of
icebergs, and then abruptly shifted into a new regime
where melting on the continent took precedence, ultimately leading to the sheet's demise.
There is a lot of evidence that ice - ocean interaction is causing fractures
where you see
icebergs calving.
At its
calving front,
where the glacier effectively ends as it breaks off into
icebergs, some of the ice melts while the rest is pushed out, floating into the ocean.
Unlike the great ice sheet of Antarctica, the Greenland ice sheet is melting both on its surface and also at outlet glaciers that drain the ice sheet's mass through deep fjords,
where these glaciers extend out into the ocean and often terminate in dynamic
calving fronts, giving up gigaton - sized
icebergs at times.
Where to Stop: Ramshackle Copper Center for sourdough pancakes; Columbia Glacier to watch
icebergs calve and sea lions frolic; Cordova, a remote fishing village on the Orca Inlet.
From your link: «In some instances, bright red spots or streaks along the edge of the continent show
where icebergs calved or ice shelves disintegrated, meaning the satellite began seeing warmer ocean water
where there had previously been ice.»
Icebergs have always
calved off of glaciers
where they hit the sea, but the rate of
calving is accelerating with climate change.
Rapid sea - level rise from these processes is limited to those regions
where the bed of the ice sheet is well below sea level and thus capable of feeding ice shelves or directly
calving icebergs rapidly, but this still represents notable potential contributions to sea - level rise, including the deep fjords in Greenland (roughly 0.5 m; Bindschadler et al., 2013), parts of the East Antarctic ice sheet (perhaps as much as 20 m; Fretwell et al., 2013), and especially parts of the West Antarctic ice sheet (just over 3 m; Bamber et al., 2009).
Or the news from Antarctica this past May, when a crack in an ice shelf grew 11 miles in six days, then kept going; the break now has just three miles to go — by the time you read this, it may already have met the open water,
where it will drop into the sea one of the biggest
icebergs ever, a process known poetically as «
calving.»