This extraordinary
ice calving event happened in spite of it being the middle of winter at the South Pole.
Not exact matches
It's vital we achieve this or we are likely to see more
calving of large
ice shelves, similar to the recent Larsen C
event.»
Reporting this week in the journal Nature Climate Change Dr Hogg and Dr Gudmundsson, examine the
events leading up to this dramatic natural phenomenon and discuss how
calving of huge icebergs affects the stability of Antarctic
ice shelves.
Their article asserts that a
calving event is not necessarily due to changes in environmental conditions and may simply reflect the natural growth and decay cycle of an
ice shelf.
Even relatively large
calving events, where tabular
ice chunks the size of Manhattan or bigger
calve from the seaward front of the shelf, can be considered normal if the
ice sheet is in overall balance.
«Now we want to understand how the
ice shelf will react to this
calving event.»
Their observations show that since the
calving event, the berg has started to drift away from the Larsen - C, with open ocean clearly visible in the ~ 5 kilometre gap between the berg and the
ice - shelf.
The team's next steps include looking more closely at specific ocean swell
events and sea
ice conditions during known
ice shelf collapses and large iceberg
calving events.
The goal is to track the dynamic response of the
ice to the
calving event, both short - term and long - term.
«In the ensuing months and years, the
ice shelf could either gradually regrow, or may suffer further
calving events which may eventually lead to collapse — opinions in the scientific community are divided,» Luckman said.
«The new branch is heading off more toward the
ice front, so it's more dangerous and more likely to cause this
calving event to occur» than the main branch, he says.
Larsen B collapsed shortly after its major
calving event while the Wilkins
ice shelf has continued to shed large chunks of
ice since 2008.
However, this iceberg
calving event is a natural process, part of how the
ice shelf regularly calves — this
ice shelf spawns huge icebergs every 6 - 10 years.
Scientists have become growingly concerned about
ice shelf collapse, and in 2016, they proposed a new rule allowing for special study areas following collapse or massive
calving events.
Calving from the floating termini of outlet glaciers and
ice shelves is just the beginning of an interesting chain of
events that can subsequently have important impacts on human life and property.
As during the last
ice age when sea levels were around 100 m lower icebergs were grounding at 44s, these would have
calved from similar size as during the 2001
event (160kmx30km) hardly evidence of change.
«The 2017 Pine Island Glacier and Larsen C
Ice Shelf
Calving Events» presented by Christopher Shuman.
For example a large 1987
calving event removed 100 years of
ice accumulation from the Ross Ice Shelf in just one day, an amount second only to the loss of the Larsen Ice She
ice accumulation from the Ross
Ice Shelf in just one day, an amount second only to the loss of the Larsen Ice She
Ice Shelf in just one day, an amount second only to the loss of the Larsen
Ice She
Ice Shelf.
[Response: You are confusing a normal and periodic
calving event with the total collapse of an
ice shelf — kind of like the difference between a haircut and decapitation.