LegendLength said:
Good info. It will help me crunch some numbers and get a temperature amount for electric vehicle usage rather than just a carbon output figure.
Also i'm sure the ratio of carbon to temperature is not linear so a small reduction in carbon output may have a large effect on temperature.
I'm glad this info is helping somebody, lots of people don't seem interested in understanding the science very much.
But now you've opened a whole new barrel of monkeys. While the core science I've described so far is essentially indisputable, the calculation of warming created by a given amount of carbon is where much of the uncertainty remains. First, the term to look for is 'Climate Sensitivity', which is defined as the amount of warming we'll experience given a doubling of CO2 concentrations.
At the beginning of the industrial age, concentrations were around 275ppm, so a doubling would be 550ppm. We're now at 380 or so, and growing by ~3ppm per year, so 550 could be hit before the end of this century, assuming existing growth rates. And the best estimates for the climate sensitivity number is around 3 degrees C. However, there's a pretty wide range of plausible values, anything from about 2.5 up to 5 or 6C is possible. And historically, climate scientists have always
underestimated the risk, so I'd bet on a higher number rather than a lower one.
But that number is based on 'fast' feedbacks, and ignores slow ones. What do I mean? Ok, water vapor is a fast feedback, in that a small increase in planetary temperature almost immediately results in higher levels of water vapor, which creates more warming. That 3C number includes the amplification of CO2 from water vapor. However, there are lots of additional feedback mechanisms, and they take much longer to respond to an initial warming. Recent research indicates that climate sensitivity should be doubled or even tripled if you want to account for slow feedbacks. So, if CO2 concentrations are halted this century at 550ppm, we'll probably see 3C of total warming (of which 0.8C has already happened). But that's just the temp at the end of this century. If you wait another century, there's another 3C of warming waiting to happen. And possibly yet another 3C in the century after that. We may see only 5' of ocean levels rising by the end of this century, but the slow melting of Greenland and Antarctica could end up being as much as 200' in the long term, assuming we stabilize at these higher temperatures.
So what are the slow feedbacks to be worried about? Off the top of my head, the scariest two are methane from melting permafrost and undersea deposits, as well as reduced albedo from melting ice.
In the northern part of North America, Europe, and Asia, there are vast forests and tundra on top of thick layers of permafrost. The ground is permanently frozen, year round. That means that dead organic matter, such as fallen leaves and branches, don't rot. Instead, they are frozen and accumulate year after year, century after century. This effectively traps their carbon content in the ground, keeping it from reaching the atmosphere. However, as the arctic region warms, the permafrost starts to thaw. The organic matter then decays and rots, releasing either carbon dioxide or methane into the atmosphere. But adding carbon dioxide and methane to the atmosphere increases planetary temperatures, and forces the permafrost to thaw faster. That causes additional rotting, and additional CO2 and methane. Lather, rinse, repeat. And this is not a small problem, there's more carbon trapped in the permafrost right now than there is in the entire atmosphere, a full thawing would easily take 550ppm well past 1000ppm.
On a related trend, there's vast amounts of methane trapped under the ocean, in a form of ice called methane clathrate. I think this mostly happens along the continental shelves. But as the oceans absorb heat from above, the clathrate melts, releasing the methane as a gas into the water. That then bubbles up into the atmosphere, and causes additional warming. More warming causes more clathrate to melt, forcing yet more methane into the air. Lather, rinse, repeat. Again, this isn't a small problem, between the volume of methane trapped, and the higher GWP of methane to start with, this also could end up doubling the amount of warming we'll observe.
Greenhouse gasses aren't the only way in which rising temperatures create more rising temperatures. Another important factor is the reflective nature of ice and snow. The white surface reflects sunlight far more effectively than dark ground or ocean, providing a cooling effect. But as the ice melts under higher temperatures, less heat is reflected, and more is absorbed by the ground and ocean. And once the ocean warms up, it's far harder for sea ice to form on the surface, so you get another cycle of less ice and more heating. We're already seeing rapid reductions in the amount of sea ice in the Arctic, indicating that this feedback is just becoming strongly active.
In fact, all 3 of these feedbacks are already happening, at least to a limited extent. We're definitely seeing melting permafrost in the arctic regions, there are even lakes in Siberia that have started bubbling out low levels of methane. More methane has been observed bubbling out of the oceans, released by thawing clathrates. And arctic ice is clearly starting to decline. But these feedbacks also suggest that there's absolutely no way to halt greenhouse gasses above a certain limit. If we pass 450ppm CO2, for example, then stopping at 550 might become utterly impossible, the feedbacks will guarantee that we go all the way to 1000. And even if we stop at 450ppm, if we stay there for long enough, the feedbacks will still kick in and bring us to 1000. There's a very strong argument that the highest safe concentration is around 350ppm, and we're at 380ppm today.