Claim: With marine ice cliff instability, sea-level rise for the next century is potentially much larger than we thought it might be five or 10 years ago

Relevance (1 = gold evidence, 0 = mined hard negative): 1
Passage: Over the 21st century, the IPCC projects that in a very high emissions scenario the sea level could rise by 61–110 cm.

Relevance (1 = gold evidence, 0 = mined hard negative): 1
Passage: For instance, a 2016 study led by Jim Hansen concluded that based on past climate change data, sea level rise could accelerate exponentially in the coming decades, with a doubling time of 10, 20 or 40 years, respectively, raising the ocean by several meters in 50, 100 or 200 years.

Relevance (1 = gold evidence, 0 = mined hard negative): 1
Passage: According to the Fourth (2017) National Climate Assessment (NCA) of the United States it is very likely sea level will rise between 30 and 130 cm (1.0–4.3 feet) in 2100 compared to the year 2000.

Relevance (1 = gold evidence, 0 = mined hard negative): 1
Passage: For instance, Mercer published a study in 1978 predicting that anthropogenic carbon dioxide warming and its potential effects on climate in the 21st century could cause a sea level rise of around 5 metres (16 ft) from melting of the West Antarctic ice-sheet alone.

Relevance (1 = gold evidence, 0 = mined hard negative): 1
Passage: A number of later studies have concluded that a global sea level rise of 200 to 270 cm (6.6 to 8.9 ft) this century is "physically plausible".

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: Sea level rise will continue over many centuries.

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: In 2018, scientists concluded that high sea levels some 125,000 years ago, which were 6–9 m (20–30 ft) higher than today, were most likely due to the absence of the WAIS, and found evidence that the ice sheet collapsed under climate conditions similar to those of today.

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: Secondly, melting of the ice shelves, the floating extensions of the ice sheet, leads to a process named the Marine Ice Cliff Instability.

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: Since the last glacial maximum about 20,000 years ago, the sea level has risen by more than 125 metres (410 ft), with rates varying from less than a mm/year to 40+ mm/year, as a result of melting ice sheets over Canada and Eurasia.

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: It is difficult to predict time of collapse in such a nonlinear problem … An ice sheet response time of centuries seems probable, and we cannot rule out large changes on decadal time-scales once wide-scale surface melt is underway.

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: Unusually rapid (up to 4.1 cm/year) present glacial isostatic rebound due to recent ice mass losses in the Amundsen Sea embayment region of Antarctica coupled with low regional mantle viscosity is predicted to provide a modest stabilizing influence on marine ice sheet instability in West Antarctica, but likely not to a sufficient degree to arrest it.

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: Sea level rise will continue beyond 2100 even if global warming is limited to 1.5°C.

Relevance (1 = gold evidence, 0 = mined hard negative): 0
Passage: Human-induced warming and associated sea level rises are expected to continue through the 21st century...