1cm?
What is the +/- on the margin of error?
What is the +/- on the margin of error?
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Gimme $32 to buy the whole article, and I'll tell you.
Time to do what denialists hate most, which is ignore their hysterical deflections and just talk about the issue. Here's the paper being discussed.
http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate2094.html#affil-auth
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Retreat of Pine Island Glacier controlled by marine ice-sheet instability
Over the past 40 years Pine Island Glacier in West Antarctica has thinned at an accelerating rate, so that at present it is the largest single contributor to sea-level rise in Antarctica. In recent years, the grounding line, which separates the grounded ice sheet from the floating ice shelf, has retreated by tens of kilometres. At present, the grounding line is crossing a retrograde bedrock slope that lies well below sea level, raising the possibility that the glacier is susceptible to the marine ice-sheet instability mechanism. Here, using three state-of-the-art ice-flow models, we show that Pine Island Glaciers grounding line is probably engaged in an unstable 40 km retreat. The associated mass loss increases substantially over the course of our simulations from the average value of 20 Gt/yr observed for the 19922011 period, up to and above 100 Gt/yr, equivalent to 3.510 mm eustatic sea-level rise over the following 20 years. Mass loss remains elevated from then on, ranging from 60 to 120 Gt/yr.
Gimme $32 to buy the whole article, and I'll tell you.
So you don't even know what the article says, you just assume that it's true. Your logic is impeccable. You're a regular Mr. Spock.
So the ass end IS in the water.. CORRECT? If its already in the water, how does that raise sea level if it melts?
So the ass end IS in the water.. CORRECT? If its already in the water, how does that raise sea level if it melts?
Because _more_ of the ass end moves off the land and into the water.
It's not a difficult concept. Why does it fluster you so?
And, it WASN'T in the water prior to this 40 km retreat.
In recent years, the grounding line, which separates the grounded ice sheet from the floating ice shelf, has retreated by tens of kilometres. At present, the grounding line is crossing a retrograde bedrock slope that lies well below sea level, raising the possibility that the glacier is susceptible to the marine ice-sheet instability mechanism.
When ice ages have warm periods, glaciers melt. It also happens when ice ages are moving toward an ending.