Burke EJ, Chadburn SE, Huntingford C, Jones CD (2018) CO2
loss by permafrost thawing implies additional emissions reductions to limit warming to 1.5 or 2 °C.
Not exact matches
A significant release of methane due to melting of the vast deposits trapped
by permafrost and clathrate in the Arctic would result in massive
loss of oxygen, particularly in the Arctic ocean but also in the atmosphere.
Many scientists concede that without drastic emissions reductions
by 2020, we are on the path toward a 4C rise as early as mid-century, with catastrophic consequences, including the
loss of the world's coral reefs; the disappearance of major mountain glaciers; the total
loss of the Arctic summer sea - ice, most of the Greenland ice - sheet and the break - up of West Antarctica; acidification and overheating of the oceans; the collapse of the Amazon rainforest; and the
loss of Arctic
permafrost; to name just a few.
Another way of putting it: Just like H2O (outside runaway), the C gain
by the atmosphere from C
loss from
permafrost «penultimately» reaches an equilibrium value that varies as a continuous function of the imposed forcing, rather than having a discontinuous jump.
A significant release of methane due to melting of the vast deposits trapped
by permafrost and clathrate in the Arctic would result in massive
loss of oxygen, particularly in the Arctic ocean but also in the atmosphere.
The likelihood of the complete
loss of Arctic summer sea ice
by 2030, faster melting of the vast Greenland ice sheets, and the rapid and quickening thaw of
permafrost regions indicate that the window for arresting climate change before tipping points are reached is rapidly closing.
Since this effect would not depend on slow rates of thermal diffusion though frozen sediments, but instead
by a simple
loss of ice, which could occur more quickly, such hydrates might be more vulnerable to destabilization than hydrates buried under
permafrost.
The USGS model also underestimates the extent of
permafrost loss by the end of the century, he said, adding that his research shows two - thirds of the state's
permafrost could be lost
by 2100 if human carbon emissions aren't cut.
Yet in view of the entirely predictable erosion of sink capacity (
by forest
loss & combustion, soils» desiccation,
permafrost melt, and oceans» warming and acidification) that notion appears to be an outstanding example of optimism bias.
In order of seniority, the seven feedbacks that seem outstanding are: Water vapour — rising
by ~ 7 % per 1.0 C of warming; Albedo
loss — due mostly to cryosphere decline; Microbial peat - bog decay — due to rising CO2 affecting ecological dynamics; Desiccation of tropical and temperate soils — due to SAT rise and droughts;
Permafrost melt — due to SAT rise plus
loss of snow cover, etc; Forest combustion — due to SAT rise, droughts, pest responses, etc; Methyl clathrates [aka methane hydrates] now threatened
by rising sea - temperatures, increased water column mixing, etc..
In hopes that a subsequent paper may remedy this shortfall, one further seminal shift would seem worth including, being a case for
permafrost GHG contribution on top of the warming from the best case of emissions control, specifically: — present realized warming, — plus pipeline warming, — plus warming from phase - out emissions reaching near - zero
by 2050, — plus a multiplier for the consequent
loss of the fossil sulphate parasol.
A 2008 study led
by David Lawrence of the National Center for Atmospheric Research (NCAR) concluded (see «Tundra 4:
Permafrost loss linked to Arctic sea ice
loss»):
The studies were performed
by Susan M. Natali, Edward A. G. Schuur, Elizabeth E. Webb, Caitlin E. Hicks Pries and Kathryn G. Crummer of Woods Hole Research Center, Massachusetts, and the University of Florida - in ESA Ecology, as «
Permafrost degradation stimulates carbon
loss from experimentally warmed tundra».
Related Rapid sea - ice
loss may increase the rate of Arctic land warming
by 3.5 times — affecting
permafrost Is This the Compost Bomb's Smoking Gun?
«It is very likely that there will be continued
loss of sea ice extent in the Arctic, decreases of snow cover, and reductions of
permafrost at high latitudes of the Northern Hemisphere
by 2016 — 2035.
«Many scientists concede that without drastic emissions reductions
by 2020, we are on the path toward a 4C rise as early as mid-century, with catastrophic consequences, including the
loss of the world's coral reefs; the disappearance of major mountain glaciers; the total
loss of the Arctic summer sea - ice, most of the Greenland ice - sheet and the break - up of West Antarctica; acidification and overheating of the oceans; the collapse of the Amazon rainforest; and the
loss of Arctic
permafrost; to name just a few.