KENAT, please see my post at 19 Mar 15 20:28 in this thread. I, and many others that believe mitigation is necessary, do not advocate for a cap-and-trade system. I think it’s important to not frame mitigation in such a one-dimensional fashion.
lacajun, that’s a good question. Someone asked something very similar in a previous thread. Please feel free to read my response at
23 Oct 14 17:19. You’ll note that my end conclusion is pretty much exactly the same as IRstuff’s response here (except I lack his brevity!).
rb1957,
rb1957 said:
we know there were sudden climate changes in the past
I think we need to be careful with some of the wording here. The “sudden” in your statement is on the order of thousands of years. Geologically speaking, this is indeed sudden. However, compared to the rate of change in the 20th-21st century, that’s moving at a glacial pace (…well given the rate of decline recently, this phrase may no longer be appropriate…but you catch my drift).
rb1957 said:
I understand we know there were sudden climate changes in the past, mechanism not well understood.
I disagree. The mechanism of past changes in climate is fairly well understood. It goes something like this (for deglaciation):
[ul 1][li]Orbital variations increase summer insolation at higher latitudes in the Northern Hemisphere (i.e. the North Pole points towards the sun more, see
Richard Alley (comically) explain Milankovitch cycles (
he’s a delightfully kooky guy)). This is fairly weak change in forcing but it leads to a series of climatic changes…[/li]
[li]The increase in Arctic and Northern Hemisphere summer insolation causes the rate and extent of ice sheet melt to increase[/li]
[li]North Atlantic deep water formation is inhibited by this freshwater runoff[/li]
[li]Thermohaline circulation is interrupted[/li]
[li]Northern Hemisphere actually cools as the equator to pole heat transports weakens[/li]
[li]Heat that use to transfer to the North, now works to warm Southern Hemisphere oceans[/li]
[li]Southern Hemisphere warming releases large reservoirs of CO2 from deep water[/li]
[li]Global CO2 concentrations increase which leads to global warming[/li]
[li]Global warming release CH4 feedback and positive ice albedo feedback[/li]
[li]Warming intensifies (note: this process takes thousands of years)[/li]
[li]As the initial driver (Milankovitch cycles) is not strengthening and as you run out of ice to melt (to provide a positive feedback), the climate settles momentarily before the opposite cycle kicks it[/li][/ul]
Some of this will sound familiar. The same underlying concepts explain past changes in climate as well as modern changes. The same (range of) sensitivity estimates explain past changes in climate as well as modern changes. The same cannot be said about any other theory I know of. This is why I’m very confused when people use “it’s change before” as an argument
against anthropogenic climate change. I will also note that the 20th century warming could not be due to Milankovitch cycles because (1) the rate of deglaciation caused by Milankovitch cycles occurs over thousands of years (as stated above) and (2) the timing is all wrong (it’s off by about 20,000 to 50,000 years). But I digress…
rb1957 said:
But this is, to a large extent, a red herring in the current debate.
How so? It’s the same planet. You need a theory that explains past and current changes in climate. The mechanism can’t magically change (however, you do need them to magically change to make “competing” theories fit). Furthermore, the impacts of paleoclimate on biodiversity are extremely relevant. Major extinctions correspond to past (major) changes in climate (which is another reason I’m confused why the “it won’t be bad” crowd seem to also be a part of the “it’s changed before” crowd (which are part of the “it’s not caused by CO2” crowd)).
rb1957 said:
The current debate is how much is the FF we burnt yesterday affecting today's climate
If you’re questioning how quickly CO2 emissions impact the climate, I responded to this at 13 Mar 15 19:37.
If you’re questioning the extent to which CO2 emissions will impact climate (now and into the future),
i.e. climate sensitivity, than, yes, I agree this is where the current debate lies. A great conference was just held on the subject of sensitivity. A lot of great information can be found at the
Max-Planck Institute of Meterology.
However, I’ll point out again,
that this is absolutely related to paleoclimatology. For example, if you want to say, “climate sensitivity (ECS) is likely about 1K. Therefore, future temperatures won’t be that high.”, you not only have to demonstrate how that value would be consistent with 20th century warming but, also and equally importantly, how it would explain past changes in climate. Beyond that, you’ll also need to explain how a low sensitivity planet lead to past mass extinctions. From what I’ve seen, you need an ECS of >2K to explain all this.
Perhaps I’m misinterpreting what you meant by it being a “red herring”, but paleoclimatology is absolutely relevant and extremely important to the current climate change debate. I hope we agree on that.