Dennis Tate
Banned
Depends on the plants..
Although China’s Green Great Wall tree-planting efforts—similar to sustainable forestry practices in Western Europe and tree regrowth on abandoned lands in Eastern Europe—enhance our planet’s ability to absorb atmospheric carbon, greening achieved through intensive agriculture does not have the same effect, says Victor Brovkin of the Max Planck Institute for Meteorology, another coauthor on our paper. Instead, carbon absorbed by crops is quickly released back into the atmosphere.
And it still does not address the destruction of ecosystems.
Wow!!!
Thank you for this exceptional reply!
When I first began to research all of this, (around 2006), I could not visualize any way to do this that would not involve a huge amount of desalination of ocean water.
Over these past fifteen years though I have ran into quite encouraging bits and pieces of information that indicate that perhaps..... just perhaps.... this can significantly be done largely without mega- scale desalination of ocean water.
As far as the destruction of ecosystems goes...... for one thing...... I cannot say that there are no negatives with this theory.......
I can only say that it sure seems to me that the alternatives to doing something along this line are even worse.........
I am worried about a mass extinction event that could well affect up to ninety percent of humans within this century.......
I would love to be terribly in error in that concern but.......... I still believe that the worst case scenario as climate change continues is far, far, far worse than the majority of experts are predicting........
partly because they are risking their careers to make the predictions that they do write.
I consider the predictions regarding how quickly the West Antarctic Ice Sheet could perhaps crack and slide...... (which is a very different thing from it melting)...... are so terribly "conservative" that I would use the word "naive" to consider those projections but......
again... I would so love to be wrong... and it would be great to find out that those relatively conservative scientists were correct?!
GUEST POSTS
14 February 2020 8:00
Guest post: How close is the West Antarctic ice sheet to a ‘tipping point’?
https://www.carbonbrief.org/guest-post-how-close-is-the-west-antarctic-ice-sheet-to-a-tipping-point
.....The West Antarctic ice sheet (WAIS) is a relatively small part, containing an amount of ice equivalent to 3.3m of sea level rise. Yet, most of it sits in a precarious position and is considered “theoretically unstable”.
As a result, how the WAIS will change in response to human-caused warming is generally thought to be the largest source of uncertainty for long-term sea level projections.
Marine ice sheet
According to the recent special report on the ocean and cryosphere (SROCC) by the Intergovernmental Panel on Climate Change (IPCC), there are two main controls on how much global sea levels will rise this century: future human-caused greenhouse gas emissions and how warming affects the Antarctic ice sheet. The IPCC says:
“Beyond 2050, uncertainty in climate change induced SLR [sea level rise] increases substantially due to uncertainties in emission scenarios and the associated climate changes, and the response of the Antarctic ice sheet in a warmer world.”
The concern around the vulnerability of the WAIS principally lies in something called “marine ice sheet instability” (MISI) – “marine” because the base of the ice sheet is below sea level and “instability” for the fact that, once it starts, the retreat is self-sustaining.
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Instability
This basic picture of ice sheet mass balance is all you need to understand why glaciologists are concerned about MISI.
Changes to the ice shelf on the floating side of the grounding line – such as thinning – can cause ice on the grounded side to lift off from the seafloor. As this ice floats, the grounding line will retreat. Because the ice flows more rapidly when it is floating than it does when grounded, the rate of ice flow near the grounding line will increase. Stretching caused by the faster flow becomes a new source of thinning near the grounding line.
This is illustrated in the figure below. As the newly floating ice flows and thins more quickly, it can cause more ice to lift off and float, driving the grounding line back.
In addition, the areas of the ice sheet at risk of MISI have a reverse, or “retrograde” gradient, which means it gets deeper further inland. As the grounding line retreats further into thicker parts of the ice sheet, the flow speeds up, further increasing ice loss. The reverse gradient makes this process self-sustaining as a positive feedback loop – this is what makes MISI an instability.
Illustration of Marine Ice Sheet Instability, or MISI. Thinning of the buttressing ice shelf leads to acceleration of the ice sheet flow and thinning of the marine-terminated ice margin. Because bedrock under the ice sheet is sloping towards ice sheet interior, thinning of the ice causes retreat of the grounding line followed by an increase of the seaward ice flux, further thinning of the ice margin, and further retreat of the grounding line. Credit: IPCC SROCC (2019) Fig CB8.1a
It is not clear yet if the MISI threshold has been crossed anywhere in Antarctica. We do know that grounding lines are retreating along the Amundsen Sea coastline – most spectacularly on the Thwaites Glacier. And the driver for the retreat appears to be relatively warm ocean water – about 2C warmer than the historical average – flowing toward the grounding line and causing stronger than usual melting.
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