New research has revealed that the rapid melting of West Antarctica's ice shelves, driven by human-induced global warming, is becoming inevitable. This acceleration of melting poses severe consequences for rising sea levels worldwide. The study, published in the journal Nature Climate Change on Monday, indicates that even if the world successfully achieves ambitious targets to curb global heating, significant ocean warming and ice shelf melting will still occur in West Antarctica.
Ice shelves are icy extensions that protrude into the ocean at the terminus of glaciers, serving as supportive structures that impede the escape of ice from land and decelerate its movement towards the sea. Additionally, they play a crucial role in safeguarding against the rise of sea levels. The melting of ice shelves leads to their depletion and a subsequent reduction in their capacity to act as buttresses. Although recent studies have suggested that ice loss in West Antarctica may be irreversible, the extent to which this can be curtailed through climate policies has remained uncertain.
The researchers examined the phenomenon known as "basal melting," wherein warm ocean currents cause the ice to melt from below. They studied the rate at which the oceans are warming and the ice shelves are melting, considering various climate change scenarios. These scenarios encompassed a range of possibilities, from optimistic ones where global warming is limited to 1.5 degrees Celsius above pre-industrial levels, to worst-case scenarios where extensive burning of fossil fuels contributes to significant planet-heating.
The findings revealed that even if global temperature rise is limited to 1.5 degrees Celsius, a goal that is not currently being met, climate change could still result in ocean warming at a rate three times faster than the historical average.
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Scientists are urgently trying to determine the cause of the Argentina-sized loss of sea ice in Antarctica. The report states that reducing planet-heating pollution at present will only have a limited impact in preventing the collapse of the West Antarctic ice sheet due to warmer oceans.
Kaitlin Naughten, an ocean modeler with the British Antarctic Survey and lead author of the study, stated that it seems we have potentially lost control of the melting of the West Antarctic ice throughout the 21st century. West Antarctica is currently the largest contributor to the rise in global sea levels and contains enough ice to cause an average increase of 5.3 meters, or over 17 feet. It is home to the Thwaites Glacier, which is commonly referred to as the "Doomsday glacier" due to the possibility of its collapse leading to a significant rise in sea levels. This would require coastal communities and low-lying island nations to either adapt to rising sea levels or relocate.
The study primarily examined the melting of ice shelves and did not directly measure the impact on rising sea levels. However, it is highly likely that sea levels will increase due to the acceleration of ice loss into the ocean from West Antarctica, according to Naughten. Ted Scambos, a glaciologist at the University of Colorado Boulder who was not part of the study, described the findings as "sobering" and stated that they reinforce previous research that highlights the concerning state of Antarctica.
It is disheartening to see the certainty of sea level rise, especially in the next century, as stated by Scambos in an interview with CNN. He highlighted the fact that current generations will witness a significant acceleration in sea level rise across coastal cities worldwide.
According to Scambos, the key to halting the rapid melting of ice is not only reducing planet-heating pollution but also removing the existing buildup. However, he acknowledged that this task will pose a significant challenge.
The floating ice edge at Thwaites Glacier margin, photographed in February 2019.
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Tiago Segabinazzi Dotto, a senior research scientist at the National Oceanography Centre in the UK, advised approaching the study with caution due to its reliance on a single model. Nonetheless, he highlighted that the study's findings align with previous research in the area, emphasizing the importance of considering it for policymakers.
Naughten and her colleagues concede that their study has limitations in predicting future rates of melting in West Antarctica due to the complexity of the process and the impossibility of accounting for every potential outcome. However, after considering various scenarios, the authors of the report assert that the melting of ice shelves is now inevitable.
"When it comes to conveying such bleak news, I have dedicated considerable thought to the matter," Naughten remarked, referring to the question of doom and gloom surrounding their study.
"I see little hope in this story, contrary to conventional wisdom which is supposed to inspire hope," she expressed. "However, it is the scientific evidence and the message I must convey to the world."
According to Naughten, the melting of the West Antarctic ice shelf is an undeniable consequence of climate change that "we will most likely have to accept and prepare for, possibly resulting in unavoidable sea level rise."
Despite the grim outlook, Naughten emphasized that humanity must not abandon its efforts to reduce fossil fuel emissions. She pointed out that it is still possible to mitigate devastating consequences in other regions of Antarctica and worldwide.