Yeah, I’m pretty sure we’ll make a difference. The important question to me is, which difference will we make? And to that, I get to give my favorite answer to everything: It depends.
The three questions we really need to answer regarding climate change are:
[ul]What will be the eventual concentration of CO[sub]2[/sub]* in the atmosphere?[/ul]
[ul]What will the temperature change be from that greenhouse gas (GHG) concentration?[/ul]
[ul]What are the effects of such a temperature change?[/ul]
*I’m going to say CO[sub]2[/sub], but significant effects from other greenhouse gases such as methane, nitrous oxide, and tetrafluoromethane exist. Those will also have to be dealt with.
For the first question, what will be the eventual concentration of CO[sub]2[/sub] in the atmosphere? We get to choose the answer, more or less. If we could power the world with a thought, we could stop it at its present 380 ppm, but we can’t do that.
Let’s say we take CO[sub]2[/sub] concentrations up to 550 ppm by 2100 (level 2 scenario from the US Climate Change Science Program.) With that concentration, there would be a ~70% chance of temperatures reaching 2-3°C higher global average than without human GHGs and ~10% chance of 3-4°C (cite.)
Or we could say we take CO[sub]2[/sub] concentrations as high as anyone (including, to my mind, inactivists) could want – somewhere around 700-900 ppm. Then there would a ~1% chance of temperatures reaching 2-3°C higher than preindustrial global averages without GHGs, and a ~12% chance of 3-4°C higher, and ~78% chance of >4°C higher (cite.)
At the 2-3°C change level we have:
[ul]Droughts that expose 0.4 to 1.7 billion people to water scarcity.[/ul]
[ul]An additional 3 million people at risk of flooding.[/ul]
[ul]An increase in the agricultural productivity in wealthy nations such as Canada and Russia, and a decrease in agricultural productivity in poor tropical nations such as Congo (both of ‘em,) India, and Peru.[/ul]
[ul]Bleaching a majority of the world’s coral reefs with negative consequences for communities that rely on them for fishing and tourism.[/ul]
[ul]Rapid increase in frequency and breadth of heat waves with attendant crop failures and forest fires.[/ul]
[ul]Widespread deglaciation of the ice sheets on Greenland and the West Antarctic.[/ul]
[ul]High risk of extinction for 20-30% of the planet’s species.[/ul]
At the 3-4°C change level we have:
[ul]High probability of total melting of Greenland’s and West Antarctica’s ice sheets.[/ul]
[ul]Falling global food production – no longer to wealthy northern nations enjoy and increase.[/ul]
[ul]Tens of millions more exposed to increased flooding risk.[/ul]
[ul]Hundreds of millions to a billon more exposed to increased water scarcity.[/ul]
[ul]Ecosystems on land may completely switch from soaking up atmospheric carbon to a net balance of adding carbon to the atmosphere.[/ul]
[ul]Widespread complete elimination of coral reefs.[/ul]
(From Hot Topic by Walker and King, but similar information can be found in the IPCC’s 4th Assessment Report, WGII, chapters 19 & 20, especially tables 19.1 and 20.4.)
The higher the temperature gets, the worse the potential consequences, and eventually too many people will be affected to ignore. That will determine the political climate future generations operate in. For now, I hope we have enough political will to avoid the worst of the consequences. My WAG is that given political limitations we can stabilize CO[sub]2[/sub] around 500-550 ppm, but I don’t really have any way of knowing.