Mooney then explains why Will's focus on
global sea ice levels in 1979 compared to today is misleading and unimportant (even though Will did get his facts wrong).
According to the center,
global sea ice levels at the end of 2008 were «near or slightly lower than» those of 1979.
The center generally does not make its statistics available, but in a Jan. 12 statement the center confirmed that
global sea ice levels were within a difference of less than 3 percent of the 1980 level.
A graph showing
global sea ice levels hitting unprecedented lows for this time of year has caused a social media storm.
Not exact matches
But when you compare it to the 7.3 metres (24 feet) that
global sea levels are predicted to rise if the entire Greenland
Ice Sheet were to melt away all at once... well, it puts things into perspective.
If those
ice sheets were to collapse,
global sea levels could change dramatically.
We have much better — and more conclusive — evidence for climate change from more boring sources like
global temperature averages, or the extent of
global sea ice, or thousands of years» worth of C02
levels stored frozen in
ice cores.
According to the Center for Remote Sensing of
Ice Sheets (CReSIS), an NSF Science and Technology Center led by the University of Kansas, the melt from Greenland's ice sheet contributes to global sea level rise at a rate of 0.52 millimeters annual
Ice Sheets (CReSIS), an NSF Science and Technology Center led by the University of Kansas, the melt from Greenland's
ice sheet contributes to global sea level rise at a rate of 0.52 millimeters annual
ice sheet contributes to
global sea level rise at a rate of 0.52 millimeters annually.
A 2016 study shocked researchers by forecasting that
ice loss from the Antarctic alone could add a metre to
global sea level by 2100.
If so, the interaction between hydrofracturing and
ice - cliff collapse could drive
global sea level much higher than projected in the Intergovernmental Panel on Climate Change (IPCC)'s 2013 assessment report and in a 2014 study led by Kopp.
GREENLAND lost 1500 cubic kilometres of
ice between 2000 and 2008, making it responsible for one - sixth of
global sea -
level rise.
The team found that results from the two methods roughly matched and showed that Greenland is losing enough
ice to contribute on average 0.46 millimetres per year to
global sea -
level rise.
«
Ice loss from this part of West Antarctica is already making a significant contribution to
sea -
level rise — around 1 mm per decade, and is actually one of the largest uncertainties in
global sea -
level rise predictions.
Computer model simulations have suggested that
ice - sheet melting through warm water incursions could initiate a collapse of the WAIS within the next few centuries, raising
global sea -
level by up to 3.5 metres.»
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.
Scientists from Rice University and Texas A&M University - Corpus Christi's Harte Research Institute for Gulf of Mexico Studies have discovered that Earth's
sea level did not rise steadily but rather in sharp, punctuated bursts when the planet's glaciers melted during the period of
global warming at the close of the last
ice age.
Anthropogenic climate change and resulting
sea level rise are now happening much more rapidly than at the transition from the last
ice age to the modern
global climate.
This
global cooling led to an expansion of the West Antarctic
Ice Sheet that caused
global sea level to fall exposing many of the Maldives» reefs.
Evidence of past glacial advance and retreat is also more easily observed in the Dry Valleys, providing a window into the past behavior of the vast Antarctic
ice sheets and their influence on
global sea levels.
Consequently we will see increase in the
ice - sheet contribution to
global sea -
level rise.
Whereas most studies look to the last 150 years of instrumental data and compare it to projections for the next few centuries, we looked back 20,000 years using recently collected carbon dioxide,
global temperature and
sea level data spanning the last
ice age.
Given the potentially catastrophic contribution of such land
ice to
global sea level rise, a better understanding of
ice dynamics is one of the key goals of the IPY.
In this dark place, so far from human eyes, significant environmental change may already be underway, which could impact how quickly the
ice sheet slips into the
sea and, subsequently, how quickly
global sea levels may rise.
In a new paper, Hansen and colleagues warn that the current international plan to limit
global warming isn't going to be nearly enough to avert disasters like runaway
ice - sheet melting and consequent
sea -
level rise.
Since 1995, researchers found that Greenland has lost a total of about 4,000 gigatons of
ice, which has become the biggest single contributor to the rise in
global sea levels.
Alaskan and the Canadian Arctic land - based glacier melt ranks with that of the Greenland
Ice Sheet as important contributors to
global sea -
level rise that is already underway.
It also reviews recent scientific literature on «worst - case»
global average
sea -
level projections and on the potential for rapid
ice melt in Greenland and Antarctica.
New research indicates that climate change has triggered an unstoppable decay of the West Antarctic
Ice Sheet, eventually leading to at least three meters of
global sea level rise
If there's anything more complicated than the
global forces of thermal expansion,
ice sheet melt and ocean circulation that contribute to worldwide
sea -
level rise, it might be the forces of real estate speculation and the race - based historical housing patterns that color present - day gentrification in Miami.
The last glacial maximum was about 18,000 years ago, when the Patagonian
ice sheet expands to include about 10 meters [33 feet] of
global sea level.
Since Larsen C's
ice already floats in the ocean, the big break - off won't immediately raise
global sea levels.
SPEED UP The collapse of West Antarctica's glaciers may be unavoidable, and the
ice sheet's demise could raise
global sea level by as much as 4 meters, researchers reported.
This is reassuring, because if the
ice cap did melt completely in the near future, it would raise
global sea levels by 60 metres.
If both
ice sheets melted — a process already underway at an alarming rate in West Antarctica —
global sea levels would rise 200 feet.
Because the
ice shelf was already floating, its break - up will not cause
global sea levels to rise.
Although the disappearance of the
ice around Antarctica will have only a marginal effect on
sea levels, it is important because it was predicted to be one of the first signs of
global warming.
If all of Greenland's
ice were to melt,
global sea levels would rise about six meters; if all of Antarctica went, it would contribute about 60 meters.
In comparison,
global sea levels are rising by about 3 millimetres a year, and a recent study estimated that one - third of that comes from
ice loss in Antarctica and Greenland.
Your feature on uneven
global distribution of
sea level rise as
ice sheets melt highlights a double whammy for northern...
Subglacial lakes are likely to influence the flow of the
ice sheet, impacting
global sea level change.
The plight of Larsen C is another sign that
global warming is destabilizing
ice along the eastern Antarctic Peninsula and raising
sea levels.
Greenland is more than twice as large as Texas and if the entire
ice sheet melted, scientists estimate
global sea levels would rise roughly 24 feet.
Rising
global temperatures,
ice field and glacial melting and rising
sea levels are among the climatic changes that could ultimately lead to the submergence of coastal areas that are home to 1.3 billion people today, according to the report, published online today by the journal Nature Climate Change.
Furthermore, unraveling the causes of
sea ice retreat should help us understand the mechanisms behind climate change on a
global level, which is interrelated to the
ice reduction in the Arctic ocean.»
The impacts of climate change include
global warming, rising
sea levels, melting glaciers and
sea ice as well as more severe weather events.
At a
global scale, the increased melting of the
ice sheet contributes to rising
sea level and may impact
global ocean circulation patterns through the so - called «thermohaline circulation'that sustains among others, the Gulf Stream, which keeps Europe warm.
Recent estimates suggest the West Antarctic
Ice Sheet alone could contribute 3.3 metres to long - term
global sea level rise.
It could lead to a massive increase in the rate of
ice sheet melt, with direct consequences for
global sea level rise.»
Global warming causes mountain glaciers to melt, which, apart from the shrinking of the Greenlandic and Antarctic ice sheets, is regarded as one of the main causes of the present global sea - level
Global warming causes mountain glaciers to melt, which, apart from the shrinking of the Greenlandic and Antarctic
ice sheets, is regarded as one of the main causes of the present
global sea - level
global sea -
level rise.
«Warming greater than 2 degrees Celsius above 19th - century
levels is projected to be disruptive, reducing
global agricultural productivity, causing widespread loss of biodiversity and — if sustained over centuries — melting much of the Greenland
ice sheet with ensuing rise in
sea levels of several meters,» the AGU declares in its first statement in four years on «Human Impacts on Climate.»