lee wrote on Dec 6
th, 2018 at 2:52pm:
You keep trotting out this claim that the GRACE data "has a problem" ... but
now the data has been corroborated by other data (ice core data) which - together with laser and ice penetrating radar confirm that the melt rate is bad and getting worse.
So your claim is now redundant. 
Further:
"The response of the ice sheet to a warming climate is not linear," Dr Trusel said.
"What that means practically is that, say we have half a degree of warming today, that would produce twice as much or more melting than half a degree that occurred sometime in the past."
Most previous research has used satellite observations and computer modelling to calculate the rate of melting in Greenland.
This new research has allowed scientists to cross-reference their satellite observations against physical ice cores, according to Dr Trusel.
"A lot of our understanding of how [the Greenland ice sheet] is changing today comes from satellite observations, which are excellent but give only a limited view," he said.
Being able to trace melting rates back 350 years is a particular strength of this latest research, according to Matt King from UTAS, who wasn't involved in this study.
"We haven't had a widespread assessment, certainly going back this far almost to the time of Shakespeare," Professor King said.
"From these type of measurements we can learn a lot about how fast things are changing in Greenland."
And understanding how fast the ice sheet is melting is crucial for us to prepare for the impact of rising sea levels in the future, according to Professor King.
According to this year's IPCC report, warming of between 1.5C and 2C locks in the eventual total deglaciation of Greenland.
This means that eventually, the Greenland ice sheet will cause oceans around the world to rise by an average of more than 7 metres.
"So there's two questions: Have we passed the threshold [and] secondly how fast is that [melting] going to occur," Professor King said.
"It could be thousands of years or it could be hundreds of years and that's the sort of question we're trying to answer."
Although climate change has so far resulted in warming of around 1C on average since pre-industrial levels, that warming has not been uniform.
In the Arctic and Greenland, signatures of warming have been detected beginning in the 18th century, and average summer temperatures have risen by around 2C since the 1990s.
It's a process called polar amplification, and it means that small increases in global average temperature will have the greatest affect in polar regions.
And there are other positive feedbacks to consider as well.
Most of us know that as we climb a mountain, the temperature drops, and vice versa.
The Greenland ice sheet is up to 3 kilometres thick in places, but as it melts, the surface layer altitude is reduced.
In turn the surface comes in contact with warmer air and melting is increased.
The complexity of ice melting, and the potential affects on the planet of the melting Greenland ice sheet mean that we need to seriously consider what impacts our actions today will have on the future, according to Dr Trusel.
"We may think of Greenland as being remote and not very important, but when Greenland changes it impacts coastlines across the globe," Dr Trusel said.
"It will be responding to what we do now and in the next few decades for centuries and millenia."
According to Professor King, this research is yet another wake-up call from a year of loud wake-up calls.
"This does remind everyone in the global community once again that very unusual things are happening on this planet."
https://www.abc.net.au/news/science/2018-12-06/greenland-ice-sheet-melting-accel...