Yet according to JPL, the main cause of this is believed to be volcanic activity under the western side of the continent. [0]
The best quote from the article was this: "I didn't see how we could have that amount of heat and still have ice on top of it."
One of the issues with this theory is that the average temperature of the ocean is below 4 deg C, and in this regime the coefficient of expansion is negative. So we might actually see a small sea level drop due to ocean warming.
>ice sheet is gaining in mass due to the melting/compaction of snow
How does melting/compaction affect the mass?
What offsets that is that ice flows under pressure, so the entire sheet has a tendency to head for the ocean. Things are a bit complicated in Antarctica since some of the landscape where the sheet is grounded is below sea level. There are concerns that the seawater is getting warm enough to cause melting there, increasing the flow rate.
If, in fact, ice sheet mass is increasing, that's great in terms of sea level rise. There's no other way to spin it.
the coastal ice shelf and continental interior are two distinct physical systems.
isostatic rebound is a confound to the measurement of snow/ice accumulation when change of altitude is corelated to snow deposition.
http://rses.anu.edu.au/geodynamics/tregoning/7.pdf [PDF]
https://www.worldatlas.com/articles/what-is-post-glacial-reb...
BTW Re: " and I'm hoping someone can more authoritatively describe the paradox because I'm feeling unsatisfied."
you wont get anymore of an authoritative take on it than discussing it with a scientist, as you are currently doing right now.
Took me a few reads to reconcile that myself.
this is one of the major activites during thesis defense, tearing apart semantics to be sure that verbal descriptors are representative of observations, and free of qualifiers or modulations.
Also defense of scientific thesis involves a discourse between supporters and deniers as a matter of course. This is the way science works, two opposing positions meet somewhere in between. usually a third external will weaken or reinforce one side over the other. The ultimate goal is not to proclaim who is right or wrong but to refine interpretations into representations of real physical processes
1992-2001: +112 b tons / year 2003-2008: +82 b tons / year Prior to 2012: -84 b tons / year 2012-2018: -241 b tons / year
It flipped from positive to negative somewhere between 2008 and 2012, correct?
2015 article: the Antarctic ice sheet showed a net gain of 112 billion tons of ice a year from 1992 to 2001. That net gain slowed to 82 billion tons of ice per year between 2003 and 2008.
2018 article: Prior to 2012, ice was lost at a steady rate of about 83.8 billion tons (76 billion metric tons) per year... Since 2012, the amount of ice loss per year has tripled to 241.4 billion tons (219 billion metric tonnes)
- They point out that the Antarctic ice sheet is gaining in mass due to the melting/compaction of snow from the past 10,000 years, not because of anything having to do with global temperatures.
- Ice losses to calving (ice breaking off and falling/drifting into the ocean and ultimately melting) are still massive, increasing, and "will catch up with the long-term gain in East Antarctica in 20 or 30 years -- I don’t think there will be enough snowfall increase to offset these losses.”
- Also, this article is from 2015. Here's a more recent analysis from 2018: https://www.nasa.gov/press-release/ramp-up-in-antarctic-ice-.... You can even see the East Antarctica trend that the 2015 article talks about in this plot from the 2018 article: https://www.nasa.gov/sites/default/files/thumbnails/image/su...