The moon over Baikal glittered in different way, like you are looking at sable fur
'Subsea permafrost thaws faster than previously thought, Russian scientists say.
Bubbling water of the East Siberia Sea. Picture: Tomsk Polytechnic University
Unexpectedly high level of subsea permafrost degradation was recorded by a Russian-led scientific expedition that spent more than a month in the seas of the eastern Arctic.
A record high methane gas emission in a shape of an underwater ‘fountain’ was registered at the beginning of October east of Bennett island in the East Siberian Sea.
‘It was a needle in a haystack chase, to find an exact place of a methane seep in dark sea waters, but we found it!
'Just right off the Academician Keldysh scientists noticed a spot of emerald-coloured water, with gas rushing to surface in thousands of bubble threads’, said expedition member Sergey Nikiforov, a communications experts of the Tomsk Politechnical University.
The area of the fountain covered about five metres, with water ‘so violently boiling with methane bubbles’ that scientists skipped using plastic cones for sampling and instead collected the gas in buckets.
‘This was the most powerful seep I have ever observed. No one has ever recorded anything similar’ said head of the expedition Igor Semiletov, who has participated in 45 Arctic expeditions.
Bubbling water of the East Siberia Sea. Pictures: Tomsk Polytechnic University
Unexpectedly high speed of degradation of subsea permafrost has been recorded.
'In some areas the roof of subsea permafrost thawed to the stability horizons of gas hydrates. Moreover, it has been proved that over the past 30 years speed of vertical degradation of subsea permafrost doubled compared to previous centuries and reached 18 centimetres per year which is significantly higher than in earlier estimates', said professor Semiletov.
'This result makes us reconsider the belief that subsea permafrost is stable and can only thaw by a few metres by the end of 21st century', he stressed.
First video of the largest methane seep (fountain) so far discovered in the Arctic Ocean, credit Tomsk Politechnic University
KEY FACTS
Aims of the expedition were
What they actually established
What else did researchers say?
Elena Kudryashova, rector of Northern Federal University, Arkhangelsk: 'Another important subject of our research was study of various types of microplastic in the seas of the eastern Arctic.
'It is important to compare and analyse results of all expeditions because microplastic represents a serious threat to organisms and sea ecosystems as a whole.'
Pictures of the methane gas seep credit Tomsk Polytechnic University
Archeologists discovered a new stone bracelet, two sharp pins, a marble ring and fox tooth pendants.
Comments (13)
Nothing special about this, there are 100's of thousands of "leaks" like that - perhaps millions - all over the world, on land, in the oceans, in lakes and in rivers.
Quite normal, been going on for billions of years.
The difference is, today the "Green" Rent & Grant Seekers are trying to use it to keep the climate alarm going, i.e. the funding of their dishonest alarmism.
No Excuses...your peoples demand it.
"Methane emissions from thermokarst areas of lakes that have expanded over the past 60 years were directly proportional to the mass of soil carbon inputs to the lakes from the erosion of thawing permafrost." And they have the same radiocarbon age. https://www.nature.com/articles/ngeo2795
"Radiocarbon data demonstrate that the CH4presentin the ESAS sediment is of Pleistocene age or older..."
"The14C content of CH4from the hotspot cores covers arange from 0.79 to 3.4 pmC corresponding to a radiocarbonage of 26 to 39 kyr BP (Fig. 2)." https://boris.unibe.ch/100942/1/Sapart_CH4%20sources%20in%20ESAS%20using%2014C-13C-2H%20(BG%202017).pdf
The lake methane is generated from previously frozen organic matter being released from thawing permafrost and metabolized producing methane. The seabed methane was produced ages ago and capped by the permafrost,
Thank you for reporting this very bad news.