Ice shelves grow through a combination of land ice flowing to the sea and snow accumulating on their surface.
A long - running rift in the Larsen C
ice shelf grew suddenly in December and now just 20 km of ice is keeping the 5,000 sq km piece from floating away.
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.»
Not exact matches
While demand is
growing and their might be a ketogenic friendly
ice cream hitting the
shelves relatively soon, this is a great homemade version.
In 2015, glaciologist Daniela Jansen reported that a large rift was rapidly
growing across one of the Antarctic Peninsula's
ice shelves, known as Larsen C.
We can see that the remaining cracks continue to
grow towards a feature called Bawden
Ice Rise, which provides important structural support for the remaining ice she
Ice Rise, which provides important structural support for the remaining
ice she
ice shelf.
In 2014, a crack that had been slowly
growing into the
ice shelf for decades suddenly started to spread northwards, creating the nascent iceberg.
Suture zones are complex and more heterogeneous than the rest of the
ice shelf, containing
ice with different properties and mechanical strengths, and therefore play an important role in controlling the rate at which rifts
grow.
Over the past few years, a large fracture has
grown across a large floating
ice shelf on the Antarctic Peninsula.
Science Ticker Science News Staff Antarctica's Larsen C
ice shelf is within days of completely cracking The crack in Antarctica's Larsen C
ice shelf (our No. 3 story for 2017)
grew 17 kilometers at the end of May (SN Online: 6/1/17).
The main rift in the Larsen C
ice shelf hasn't
grown longer since February.
Rift through Larsen C
ice shelf has
grown to 175 kilometers, and collapse of nearby
ice shelves could offer a glimpse of its future
After obtaining precise
ice shelf height data, the researchers used a regional climate model to work out how much of the variability on a year - to - year basis was due to snowfall (which causes
ice shelves to
grow taller) versus ocean - driven melting (which causes
ice shelves to thin from below).
The findings, published Monday in Nature Geoscience, reveal that the 1997 - 98 El Niño led to a substantial loss of mass from the bottom of the
ice shelves in West Antarctica's Amundsen sea sector, even as the
shelves appeared to
grow about ten inches taller from additional snowfall.
Scientists have watched as a crack in the Antarctic Peninsula's Larsen C
ice shelf has
grown across the
shelf, allowing a massive amount of
ice to break away.
A long - running rift in Larsen C
ice shelf suddenly
grew in December, becoming almost as huge as Delaware and now poised to break off from Antarctica anytime soon.
Ice shelves have
grown and shrunk through the ages, mirroring the natural cooling and warming of the climate.
You can't fake spring coming earlier, or trees
growing higher up on mountains, or glaciers retreating for kilometres up valleys, or shrinking
ice cover in the Arctic, or birds changing their migration times, or permafrost melting in Alaska, or the tropics expanding, or
ice shelves on the Antarctic peninsula breaking up, or peak river flow occurring earlier in summer because of earlier snowmelt, or sea level rising faster and faster, or any of the thousands of similar examples.
The Larsen C
ice shelf in Antarctica had a
growing rift for years, that finally completed its path to the ocean and broke off a huge chunk of
ice.
The crack on Larsen C, one of the world's greatest
ice shelves found on the northern major
ice shelf of the Antarctic Peninsula, is
growing to around 350 kilometers.
Today, a huge rift has nearly bisected a large frontal section of the Larsen C
Ice shelf — an ice system many times the size of its now deceased companions Larsen A and Larsen B. And during December — a period when Antarctica was warming into Austral Summer — this massive crack grew by 18 kilomete
Ice shelf — an
ice system many times the size of its now deceased companions Larsen A and Larsen B. And during December — a period when Antarctica was warming into Austral Summer — this massive crack grew by 18 kilomete
ice system many times the size of its now deceased companions Larsen A and Larsen B. And during December — a period when Antarctica was warming into Austral Summer — this massive crack
grew by 18 kilometers.
Like a driver facing a crack in a windshield, scientists have been watching a rift
growing across a giant
ice shelf in Western Antarctica for years, waiting for the day that it would break.
Notable this year were measurements of a crack
growing across the
ice shelf of Petermann Glacier.
A
growing cavity beneath the
ice shelf has allowed more warm water to melt the
ice, the researchers say — a process that feeds back into the ongoing rise in global sea levels.
Large cracks
grow through Antarctic
ice shelves as warmer ocean currents melt the towering glaciers from below.