dohboi wrote:much sooner than previously assumed
This seemingly technical finding has profound and troubling implications. The more stable the upper ocean, the less vertical mixing that takes place. This mixing is a primary means by which the ocean buries warming surface waters. So the surface warms up even faster. It’s what we call a “positive feedback”—a vicious cycle.
Our study suggests that key positive feedbacks (amplifying factors) related to reduced ocean heat might lead to more rapid surface warming in the decades ahead than many of the models predict.
Newfie wrote:More news, bad news, from the arctic re: methane.
https://www.theguardian.com/science/202 ... tists-find
Remember Cid Yama?
At this moment, there is unlikely to be any major impact on global warming, but the point is that this process has now been triggered. This East Siberian slope methane hydrate system has been perturbed and the process will be ongoing,” said the Swedish scientist Örjan Gustafsson, of Stockholm University, in a satellite call from the vessel.
An earth system model shows self-sustained melting of permafrost even if all man-made GHG emissions stop in 2020
Abstract
The risk of points-of-no-return, which, once surpassed lock the world into new dynamics, have been discussed for decades. Recently, there have been warnings that some of these tipping points are coming closer and are too dangerous to be disregarded. In this paper we report that in the ESCIMO climate model the world is already past a point-of-no-return for global warming. In ESCIMO we observe self-sustained melting of the permafrost for hundreds of years, even if global society stops all emissions of man-made GHGs immediately. We encourage other model builders to explore our discovery in their (bigger) models, and report on their findings. The melting (in ESCIMO) is the result of a continuing self-sustained rise in the global temperature. This warming is the combined effect of three physical processes: (1) declining surface albedo (driven by melting of the Arctic ice cover), (2) increasing amounts of water vapour in the atmosphere (driven by higher temperatures), and (3) changes in the concentrations of the GHG in the atmosphere (driven by the absorption of CO2 in biomass and oceans, and emission of carbon (CH4 and CO2) from melting permafrost). This self-sustained, in the sense of no further GHG emissions, melting process (in ESCIMO) is a causally determined, physical process that evolves over time. It starts with the man-made warming up to the 1950s, leading to a rise in the amount of water vapour in the atmosphere—further lifting the temperature, causing increasing release of carbon from melting permafrost, and simultaneously a decline in the surface albedo as the ice and snow covers melts. To stop the self-sustained warming in ESCIMO, enormous amounts of CO2 have to be extracted from the atmosphere.
A new study, published in Science Advances on Friday, aimed to see how South American forests’ carbon intake has changed in recent years. To do so, the authors analyzed greenhouse gas monitoring data from 1987 to 2020 on 32 deciduous, semi-deciduous, and evergreen forests—each of which has seen deforestation—in the lush state of Minas Gerais in southeastern Brazil. Altogether, the area they examined spanned some 81.5 acres (33 hectares).
By plugging this data into statistical models, the authors found that on average, these forests are now sucking up 2.6% less carbon per year than they were 33 years ago. At the same time, the forests’ carbon output from fires increased by 3.4% per year, meaning overall, they’re losing their ability to absorb the gas. These changes were enough to push the forests over the edge from carbon sinks to carbon sources. The authors fear their findings may be able to be extrapolated to tropical forests in the region as a whole.
The data shows that the switch happened in 2013. That year, on average, the examined forests released 0.14 U.S. tons per 2.5 acres (0.13 metric tons of carbon per hectare), or the equivalent output of driving 323 miles in a diesel car.
The authors’ findings are particularly troubling because separate research recently found that the importance of tropical forests’ carbon sequestering is nearly as important as that of the Amazon rainforest.
A recent third-party study, also referenced in the aforementioned Arctic News article d/d June 10th, concluded that at 1200 ppm atmospheric CO2 global heating cranks up by 8°C, or 14.4°F, within a decade. (Source: Arctic News d/d June 10, 2019). Truth be known, that scenario is not problematic, it’s catastrophic and too far along to be classified as a problem. After all, problems can be fixed; catastrophes are fatal.
According to Shakhova’s research, as referenced in Geosciences/ 2019: “Releases could potentially increase by 3–5 orders of magnitude, considering the sheer amount of CH4 preserved within the shallow ESAS seabed deposits and the documented thawing rates of subsea permafrost reported recently. The purpose of this paper is to introduce the ESAS permafrost–hydrates system, which is largely unfamiliar to scientists,” Ibid. (Side note: 3 orders of magnitude is equivalent to 1,000, i.e., a large methane release.)
More from Shakhova: “Here we present results of the first comprehensive scientific re-drilling to show that subsea permafrost in the near-shore zone of the ESAS has a downward movement of the ice-bonded permafrost table of ~14 cm (6 inches) year over the past 31–32 years… However, recent studies show that in some areas very recently submerged permafrost is close to or has already reached the thaw point,” Ibid.
The ESAS is the most extensive (2.1 × 106 km2) continental shelf in the World Ocean (WO); the ESAS is composed of the Laptev Sea, the East Siberian Sea, and the Russian part of the Chukchi Sea. Because of its shallowness (mean depth is ~50 m, Figure 1a) and location, the ESAS has a unique climatological history; due to sea level variations caused by glaciation in cold climate epochs or by glacier melt during warm epochs, the entire area of the ESAS is periodically subjected to dry (terrestrial) or to submerged (marine) conditions [23].
The ESAS near-shore zone is highly affected by riverine runoff, which causes significant warming of the shelf water: the mean annual temperature of bottom water is documented to be ˃0 °C and has shown a tendency to increase during the last few decades [20,25]. Heat flux from river bodies can cause formation of thawed sediments deep beneath riverbeds, which could occur below both existing rivers and paleo rivers [26]. Sedimentation on the ESAS is determined by combined input of Arctic river (Lena, Yana, Indigirka, Kolyma) fluvial sediment discharge, coastal sediment input (coastal erosion), and subsea permafrost ‘bottom thermo-abrasion’ [27,28]. Sedimentation flow varies significantly, and sedimentation rates vary by orders of spatial and temporal magnitude throughout the year; it was suggested that ˃20 Tg of terrigenous organic carbon (Corg) is delivered to the ESAS each year [29]. Sedimentary basins on the ESAS, which result from these high levels of sedimentation, are predicted to reach up to 15 km in thickness (Figure 2), providing favorable conditions for CH4 production in the seabed [30]. As a result, large amounts of CH4 accumulate in the ESAS seabed [5].
Permafrost (frozen ground with a two-year mean subzero temperature) and associated permafrost-related Arctic hydrates in the ESAS first originated during cold climate periods, when sea level dropped more than 100 m lower than it is today; consequently, the coastline extended as much as 1000 km further north, exposing the entire shelf area above the sea surface and, thus, increasing the area of the Siberian coastal accumulative plain by a factor of five [11]. Exposed to the low Arctic surface temperatures, marine sediments were subjected to a drastic change in their thermal regime—cooling by as much as −28 °C [28]. This led to freezing of the uppermost few hundred meters of sediments; as a result permafrost formed, covering the upper few hundred meters of the sedimentary drape with an impermeable cap (Figure 4b). Additionally, freezing of marine sediments and formation of permafrost caused a change in the P/T conditions of previously originated hydrates; shelf hydrates had existed in marine conditions before the shelf was exposed above the sea. As a result of this drastic change in thermal regime shelf hydrates and gaseous CH4 pre-formed in marine sediments gradually turned into permafrost-related hydrates (or Arctic hydrates), which might exist within the HSZ (conventional Arctic hydrates, Figure 4b) and/or outside the HSZ (inter-pore, porous, and/or relic hydrates, Figure 4b), and which may partially survive freeze–thaw cycles during the alternating glacial–interglacial climate periods [63].
After a sea level rise during the inter-glacial climate epochs by up to 120 m, the entire area of the ESAS was submerged (Figure 4c); the last replacement of the cold epoch by the current warm epoch (Holocene) led to permafrost inundation about 12 kyr ago [66]. Inundated together with permafrost, which became subsea permafrost after inundation, the Arctic hydrates (of terrestrial origin) became the unique shallow Arctic shelf hydrates—that is, hydrates existing where the water depth in the Arctic shelf is <200 m. Since the time of inundation, the permafrost–hydrate system has been forced to undergo transformations determined by drastic changes in the thermal regime of the surrounding environment. Indeed, due to inundation, permafrost, with a mean annual temperature upon origination of around −17 °C, achieved a new mean annual temperature under seawater of ≥−1.8 °C [10,11], reaching a new quasi-stationary temperature equilibrium with the surrounding environment [5,6].
Some gaseous CH4 converted from inter-pore hydrates started its upward movement but the major fraction was converted back to so-called metastable relic hydrates, which accumulate at depths <100 m due to the self-preservation phenomenon. This preservation allowed hydrates to survive during the short thaw cycles until inter-glacial epochs were replaced by glacial epochs. However, in places where geothermal heat flux was greater than on the rest of the shelf area and where permafrost was affected by thermokarst before inundation, partial destabilization of these hydrates was possible, allowing CH4 release to the overlying strata (Figure 4d).
Alternating glacial–interglacial epochs led to repetitive changes in the thermal regime of the permafrost–hydrate system, with corresponding changes in system stability and integrity; such alternations are known to exist within at least four of the last climate cycles, or for ~400 kyrs [1]. During a normal climate cycle, like the Eemian which began about 130,000 years ago and ended about 115,000 years ago, the interglacial thermal maximum and associated high sea level stand usually lasted 1–2 kyrs, not long enough for permafrost to reach thermal equilibrium with the surrounding environment and start losing its integrity. This enabled the permafrost–hydrate system in the ESAS to return from state (c) to state (b) (Figure 4). The current inter-glacial epoch (Holocene) exhibits continuing warming associated with a long-lasting sea level high stand (˃5 kyrs) [1,71]. Because approaching the phase-transition point (thawing) can only be possible after permafrost reaches an equilibrium state with the surrounding environment, which requires ˃˃1–2 kyrs, the additional duration of the warming effect of seawater makes a critical contribution to the process of permafrost–hydrate system destabilization [5].
As a result, continuing warming causes not only advanced deepening of the IBPT but also thaw-through disintegration of the permafrost body at places such as fault zones, paleo-rivers, areas affected by thaw lakes, freshwater seepages into shelf sediments, and so-called pingo-like features, which provide subsea permafrost with heat and create migration pathways for CH4 that is released from destabilizing hydrates
A return from the state described in panel 4(d) to the state described in panel 4(c) is only possible if warming is replaced by cooling. Returning to the state shown in 4(a) is impossible, because the state shown in 4(a) remains hypothetical—this implies returning to the state when the ESAS was never exposed above sea level and, thus, was never subjected to conditions that allow the existence of specific types of hydrates that exist exclusively in the Arctic shallow shelf region
Newfie wrote:More validation of the awful mess we have created.
https://theconversation.com/worried-abo ... asp-153091
Plantagenet wrote:Newfie wrote:More validation of the awful mess we have created.
https://theconversation.com/worried-abo ... asp-153091
Thats a really good article, Newfie. Recommended to all.....
The scientists made multiple recommendations of what must be done immediately to save the planet.
The top 3 were:
1. abolishing the goal of perpetual economic growth
2. revealing the true cost of products and activities by forcing those who damage the environment to pay for its restoration, such as through carbon pricing
3. rapidly eliminating fossil fuels
And, of course, none of that is going to happen anytime soon. Obama did nothing and Trump did nothing and now Joe Biden will do nothing. Joe Biden is all about keeping economic growth going, he opposes a carbon tax, and he says he wants to eliminate fossil fuel.... by 2050......30 years from now, in other words it ain't gonna happen on Joe Biden's watch.
So enjoy every beautiful day.
Enjoy our beautiful planet.
It will be sad when everything collapses, but we can still have a lot of fun watching the whole system go down, thanks to the lies and incompetence of our putative leaders.
Cheers!
mmasters wrote:I agree GW is another upcoming crisis. But this one the looney left has raved enough about that sadly they will probably get the ball in their court when it manifests and, well... good luck with that LOL. Best start working now on a good setup to bug out and insulate yourself from the soon to be raving hordes.
Joe Biden will do nothing... Joe Biden opposes a carbon tax. --Plantagenet--
Biden: I Would Support a Carbon Tax .... Sep 02, 2019 · During Wednesday’s CNN Climate Town Hall, Vice President Joe Biden stated that he would support a carbon tax.
Incoming Biden Administration officials support putting a price on carbon.
As President-elect Joe Biden gears up to take office in January, he’s promised to take swift action on the climate crisis and push a bold climate agenda. In recent weeks, he has announced several of his initial nominations for positions within his cabinet. Here at CCL, we’re excited to see that Mr. Biden's picks strongly support putting a price on carbon.
suxs wrote:First a quote from President-elect Biden himself on 09/02:Biden: I Would Support a Carbon Tax .... Sep 02, 2019 · During Wednesday’s CNN Climate Town Hall, Vice President Joe Biden stated that he would support a carbon tax.
Per RedGREENandBlue 12/21/2020:Incoming Biden Administration officials support putting a price on carbon.
As President-elect Joe Biden gears up to take office in January, he’s promised to take swift action on the climate crisis and push a bold climate agenda. In recent weeks, he has announced several of his initial nominations for positions within his cabinet. Here at CCL, we’re excited to see that Mr. Biden's picks strongly support putting a price on carbon.
The real question here is what Joe Biden will actually do when he becomes President.
Why ... do you make definitive statements of fact....
an opinion piece published by a highly partisan web site does not pass the smell test for evidence.
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