350 ppm - a line we've already crossed
This entry was posted on 1/2/2008 10:53 PM and is filed under Global Warming,Action.
From an article by Bill McKibben on Truthout.org:
- "...what may turn out to be the most crucial development went largely unnoticed. It happened at an academic conclave in San Francisco. A NASA scientist named James Hansen offered a simple, straightforward and mind-blowing bottom line for the planet: 350, as in parts per million carbon dioxide in the atmosphere. It's a number that may make what happened in Washington and Bali seem quaint and nearly irrelevant. It's the number that may define our future.
- Twenty years ago, Hansen kicked off this issue by testifying before Congress that the planet was warming and that people were the cause. At the time, we could only guess how much warming it would take to put us in real danger. Since the pre-Industrial Revolution concentration of carbon in the atmosphere was roughly 275 parts per million, scientists and policymakers focused on what would happen if that number doubled - 550 was a crude and mythical red line, but politicians and economists set about trying to see if we could stop short of that point. The answer was: not easily, but it could be done.
- Consider: We're already at 383 parts per million, and it's knocking the planet off kilter in substantial ways. So, what does that mean? (my bold)
- The last time the Earth warmed two or three degrees Celsius - which is what 450 parts per million implies - sea levels rose by tens of meters, something that would shake the foundations of the human enterprise should it happen again."
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The next time anyone questions our need to take significant action to reduce our greenhouse gas emissions now, tell them about NASA scientist James Hansen, 1987, 350 ppm, and 383 ppm.
My question: once we take our foot off the global warming train's "gas pedal" and significantly reduce greenhouse gas emissions, HOW LONG until the earth actually stops warming?? How fast is the train going and how much inertia does it have?
