When such events do occur (such as flooding in Bangladesh,
ice shelf breakups in Antarctica) they occur in remote locations that are far from the concerns of average Americans, and making the link between these events and individual day to day concerns is very difficult to make.
Not exact matches
«There are suggestions
in the literature that accelerated
breakup of
ice shelves will lead to rise of sea level by several meters by the end of the century,» Godin said.
Since IPCC (2001) the cryosphere has undergone significant changes, such as the substantial retreat of arctic sea
ice, especially
in summer; the continued shrinking of mountain glaciers; the decrease
in the extent of snow cover and seasonally frozen ground, particularly
in spring; the earlier
breakup of river and lake
ice; and widespread thinning of antarctic
ice shelves along the Amundsen Sea coast, indicating increased basal melting due to increased ocean heat fluxes
in the cavities below the
ice shelves.
An additional new feature is the increasingly visible fast dynamic response of
ice shelves, for example, the dramatic breakup of the Larsen B Ice Shelf in 2002, and the acceleration of tributary glaciers and ice streams, with possible consequences for the adjacent part of the ice shee
ice shelves, for example, the dramatic
breakup of the Larsen B
Ice Shelf in 2002, and the acceleration of tributary glaciers and ice streams, with possible consequences for the adjacent part of the ice shee
Ice Shelf
in 2002, and the acceleration of tributary glaciers and
ice streams, with possible consequences for the adjacent part of the ice shee
ice streams, with possible consequences for the adjacent part of the
ice shee
ice sheets.
Reports of the
breakup of Antarctic
ice shelves and other signs of actual current warming
in polar regions begin to affect public opinion.
Ultimately, there is limited value
in debating whether human - driven warming has caused the uncloaking of any particular Arctic island, the retreat of a snowfield atop any single mountain — even one as charismatic as Kilimanjaro — or the
breakup of a particular
ice shelf in Antarctica, or any other regional anomaly.
This flow of
ice, fed by the continuous formation of new
ice on land and culminating
in the
breakup of the
shelves on the outer fringe and the calving of icebergs, is not new.
Small changes
in global sea level or a rise
in ocean temperatures could cause a
breakup of the two buttressing
ice shelves.
Subsequent work pointing
in the same direction included De Angelis and Skvarca (2003), who found that Antarctic grounded
ice surged after an
ice shelf breakup, and Bindschadler et al. (2003), who reported that a major West Antarctic
ice stream started and stopped flowing as the tide went up and down.
In this case the thinning and resultant structural weaknesses preconditioned the
ice to rapid
breakup, which proceeded to lose only the preconditioned portion of the
ice shelf.
IMO, the strongest argument for sea
ice decline over the last decade for being unusual and at least
in part attributable to global warming is this (from Polyakov et al.): The severity of present
ice loss can be highlighted by the
breakup of
ice shelves at the northern coast of Ellesmere Island, which have been stable until recently for at least several thousand years based on geological data.