Well, I'm a bit worried about the temperatures up there too. See, a
warmer radiator (-2.7 C) is
more (-6.5 C) effective (-11.7 C) at
losing (-20.6 C) heat (-27.2 C), and since we know where it went (space) you start to wonder where it came from. Since it
isn't there now (-28.1 C), and the Sun set a while back that far north, it has to be transported from somewhere further south.
Things aren't looking too unusual compared to
last year (-20.1 C) or
the year before (-31.8 C), but nearly
a megasec ago (-2.7 C) it was around 28 C warmer than the same time
last year (-31.3 C), though the nullschool site doesn't go back before 11/24/2014 sadly.
Still the main idea here is that this wasn't a gradual process of the Arctic being warmed by +20 C, it was a freakishly warm spike this year, so we don't have a lot of precedent to go by on there.
its a tipping point issue. once temperatures rise enough to begin destablizing deposits, the contributions of the added gasses make destablization of deeper deposits happen, in a runaway reaction. that is exactly what is happening.
Tipping points are the worst fad science buzzword ever.
The planet remains within a certain temperature range over megayears, the hottest periods and the coldest periods didn't turn into permanent runaway scenarios, outside of the snowball earth periods, and the current geological period has been defined by an ice age cycle. Brief spikes to warm periods like our civilization arose within, then long slides into glaciation.
One might say the global climate exhibits a damping behavior and a tendency to return to, and oscillate around certain states. These are properties usually associated with systems involving significant negative feedbacks. This is a problem for any hypothesis proposing it is controlled by positive feedback effects, especially high gain ones.
yess... if there wasnt already epic fucktons of the stuff wrapping the planet like a blanket, which there is.
on the ocean floor, its fine. when the heat cant escape the planet, because of the amount already in the atmosphere, then any source of heat will drive more forcing.
You're talking about 44 Terawatts from the ground vs 173 Petawatts (or 173,000 Terawatts) from the Sun.
Hadn't heard about the seaweed thing for cows.
I wonder what the state of the clathrate was during the late Paleozoic (Carboniferous, Permian) and most of the Mesozoic (Triassic, Jurassic periods. The Cretaceous got cooler on average), those were pretty warm periods. Warmer than now that's for sure.
i would have to research it more carefully, but my armchair opinion is the driving greegouse gasses were co2 and water, and that clathrate ices were not being produced/stored up like we have now, as the carbon was inside organisms, or being deposited in what are now our oil fields.
methane is 36 times more powerful than co2. different atmosphere, different equilibrium.
Clathrates have formed as long as there was methane and suitably cool boundaries between oceans and rocks, so basically as long as bacteria have been farting and burping, or the entire span of life on the planet, possibly excluding the anoxic period during the Permian-Triassic extinction, and bits in the snowball periods where the behavior of methane released subsurface may not have been the same as it is today with a broad ocean/atmosphere interface.