Showing posts with label Nick Breeze. Show all posts
Showing posts with label Nick Breeze. Show all posts

Monday, February 23, 2026

The 2026 El Nino

Arctic sea ice extent

Arctic sea ice extent was 13.53 million km² on February 28, 2026, the second lowest on record for the time of year. This is a very dangerous situation, as we're moving out of a La Niña that is suppressing temperatures into an El Niño that is elevating temperatures. 

The above image is adapted from the Japanese National Institute of Polar Research and shows Arctic sea ice extent from the start of the year through early May. 

The image below, adapted from NSIDC, shows that Arctic sea ice extent was second lowest on record for the time of year on February 27, 2026. 


As illustrated by the image below, Arctic sea ice extent was 1.36 million km² lower than 1981-2010 on February 27, 2026 (black), the second lowest anomaly on record for the time of year and a deviation from 1981-2010 of -2.96σ. 


Importantly, we're moving from a La Niña to an El Niño. The above images illustrate the impact of differences between El Niño and La Niña. The year 2016 was a strong El Niño year and Arctic sea ice extent started to decline strongly in the course of 2016 and extent remained low in 20017 and 2018. The El Niño that started to develop in 2023 contributed to the very low sea ice extent in early 2025, while sea ice extent was also lowest on record for the day during early parts of 2026. The blue line is the 2012 extent, which would turn into a record low later that year, a record that still stands today. 

What happened in 2012? Let's first look into greenhouse gas concentrations, which are high in the Arctic and causing Arctic temperatures to rise strongly.


[ CO₂ concentration on Feb 22, 2026 ]
As illustrated by the image below, methane concentrations were as high as 2498 ppb on February 19, 2026. Methane tends to be higher closer to the North Pole, while methane is particularly high at this altitude, unlike CO₂ that has its highest concentrations close to the surface.

As illustrated by the image on the right, surface concentration of carbon dioxide (CO₂) was as high as 526 ppm on February 22, 2026. The image also shows that CO₂ concentrations are high across the Arctic.

High Arctic concentrations of greenhouse gases are causing Arctic temperatures to rise strongly, contributing to decline in Arctic ice and snow cover, which causes loss of surface albedo (reflectivity).

Albedo loss is a self-amplifying feedback loop that further speeds up the temperature rise in the Arctic. 

The strong rise of Arctic temperatures narrows the temperature difference between the Equator and the Arctic, which slows down the speed at which hot air flows from the Equator to the Arctic. This slowdown can hugely distort the Jet Stream and can also contribute to a slowdown of ocean currents such as the Atlantic Meridional Overturning Circulation (AMOC), which - together with ocean stratification - can contribute to more ocean heat accumulating at the surface and to less lower clouds (albedo loss).

[ Storm over Arctic Ocean, August 2012 ]
Distortion of the Jet Stream in turn results in more extreme weather such as heatwaves, storms and fires. Fires produce soot that can settle down on the snow and ice cover and darken the surface (albedo loss). Storms can bring huge amounts of warm air into the Arctic. Furthermore, storms can churn sea ice into smaller pieces.

Early August 2012, a storm hit the Arctic Ocean, as illustrated by the image on the right. Smaller pieces of ice melt more rapidly, since more parts become exposed to ocean heat, in contrast to a large flat and solid layer of ice that is also less susceptible to wind. 

Pieces of ice that are lighter and smaller will more easily stand out above the water and capture the wind like the sails of yachts. Storms can push these smaller pieces more easily together, decreasing sea ice extent (albedo loss). 

Storms can also temporarily speed up currents that are moving pieces of sea ice, with the potential to move pieces all the way out of the Arctic Ocean, where they will melt away rapidly. 

Furthermore, storms can cause deeper vertical mixing of the sea water column, causing more heat to penetrate the seabed and resulting in destabilization of hydrates contained in sediments and eruption of huge amounts of methane from hydrates and from free gas held underneath the hydrates. 

In conclusion, a huge retreat in Arctic sea ice extent could occur in 2026, as Jet Stream distortion is getting ever stronger due to the ongoing temperature rise and this can cause storms over the Arctic Ocean to devastate sea ice extent. A Blue Ocean Event could therefore happen in the course of 2026. 

The 2026 El Niño
 
During La Niña, heat builds up underneath the sea surface, so sea surface temperatures and air temperatures get suppressed. During El Niño, ocean heat comes to the sea surface and air temperatures are elevated.

The image below shows ERA5 daily sea surface temperature anomalies (60°S-60°N) from 1 January 2023 through 25 February 2026, with an added trend, warning about the potential for a steep temperature rise in 2026.

[ the image is discussed at Arcticnews on facebook ]

El Niño outlook ]
Moving from the bottom of a La Niña to the peak of a strong El Niño alone can make a difference of more than 0.5°C, as discussed in an earlier post.

The image on the right, adapted from NOAA, shows Niño-3.4 region temperature anomalies and forecasts, indicating that El Niño will emerge in the course of 2026. 

The image below, also adapted from NOAA, shows El Niño years (red), La Niña years (blue) and neutral years (grey).

[ image from earlier post ]

[ image from earlier post, click on images to enlarge ]
The image on the right, adapted from NOAA, shows ENSO (El Niño-Southern Oscillation) probabilities for the Niño3.4 region (5°N-5°S,120°W-170°W) relative sea surface temperature index, with El Niño (red bar) emerging in the course of 2026.

The combination image below, adapted from ECMWF, shows ENSO anomalies and forecasts for developments through February 2027 in Niño3.4 (left panel) and in Niño1+2 (right panel), indicating that the next El Niño will emerge and strengthen in the course of 2026.

[ image from earlier post ]
The combination image below, also adapted from ECMWF, shows anomalies and forecasts through August 2026 in the Niño3 region (left panel) and the Niño1+2 region (right panel).

[ image from earlier post ]
The image below, adapted from tropicaltidbits.com, shows a rise since early January 2026 of more than 2.5°C in sea surface temperature anomalies (CDAS data) in the Niño1+2 region through February 28, 2026. 


Nick Breeze talks with Jennifer Francis about the upcoming El Niño in the video below, also discussed on facebook.


Latent heat buffer loss - as sea ice, permafrost and glaciers disappear

Ocean heat is another contributor to Arctic sea ice loss and ocean heat keeps melting sea ice all year long from below. 

Latent heat is energy associated with a phase change, such as the energy consumed when ice turns into water. During a phase change, the temperature remains constant. As long as there is ice, additional heat will be absorbed by the process of ice turning into water, so the temperature doesn't rise at the surface.
The amount of energy absorbed by melting ice is as much as it takes to heat an equivalent mass of water from zero to 80°C.

The image below, from an earlier post, shows monthly Arctic sea ice volume in the past 25 years. Markers show April (blue) and September (red) volume, corresponding with the year's maximum and minimum. In 2025, Arctic sea ice reached a record low maximum volume as well as a record low minimum volume.

As illustrated by the above image, Arctic sea ice volume in April 2025 was very low, so while relatively little melting took place between April 2025 and September 2025, a record low Arctic sea ice volume was still reached in September 2025. The above image shows Arctic sea ice volume through mid December 2025, with an analysis of the strength of the melting between April (annual maximum) and September (annual minimum). If the trend in annual maxima (blue circles) continues, Arctic sea ice in 2026 looks set to reach an even lower volume in April 2026. The difference between strong melting (magenta) and little melting (green) is 3000 km³, so if strong melting will take place from April 2026, this may well cause a Blue Ocean Event to occur later in 2026. A Blue Ocean Event could be said to occur when only 1000 km³ or less Arctic sea ice volume remains.

There is a huge danger that seafloor methane and methane from thawing terrestrial permafrost will add strongly and abruptly to the temperature rise, as discussed in many earlier posts such as this one and as illustrated by the screenshot below.
 
Warmer water flowing into the Arctic Ocean causes Arctic sea ice to lose thickness and thus volume, diminishing its capacity to act as a buffer that consumes ocean heat entering the Arctic Ocean from the North Atlantic. This means that - as sea ice thickness decreases - a lot of incoming ocean heat can no longer be consumed by melting the sea ice from below, and the heat will therefore contribute to higher temperatures of the water of the Arctic Ocean. The danger of this is described in the screenshot below. 
[ screenshot from earlier post ]
The image below shows that Arctic sea ice volume was at a record daily low on February 28, 2026. 


The situation is dire and unacceptably dangerous

The combination image below shows images adapted from Copernicus. The image on the left shows temperature anomalies at the bottom end of the scale over parts of North America and Russia on February 27, 2026, while temperature anomalies are at the top end of the scale over much of the Arctic Ocean. The image on the right shows absolute temperatures on February 27, 2025.


The image below shows a temperature anomaly forecast for February 27, 2026, adapted from tropicaltidbits.com, with anomalies at the top end of the scale (28°C) showing up over most of the Arctic Ocean. The image also illustrates to what extent cold air has descended from the Arctic over Russia and North America, with more background as to why this is happening discussed in a recent post.


The image below shows a temperature anomaly forecast for November 2026, adapted from tropicaltidbits.com, with anomalies at the top end of the scale (13°C) showing up over most of the Arctic Ocean.


The danger is that a strong 2026 El Niño could trigger a cascade of feedbacks, kicking in with increasing ferocity, as follows:

• a strong 2026 El Niño could trigger a cascade of feedbacks, including:
• a Blue Ocean Event (minimal Arctic sea ice), resulting in huge loss of albedo,
• with crossing of the latent heat tipping point (loss of ice buffer), resulting in
• seafloor CH₄ hydrates destabilization and eruption of vast amounts of CH₄, and
• submarine and terrestrial permafrost thawing, resulting in even more emissions,
• and further Jet Stream distortion, causing even more extreme weather events,
• resulting in forest fires, initially in Siberia, Alaska and Canada, and also in
• droughts and fires in global peatlands and in tropical rainforests, causing
• rapid melting and thaw of mountaintop snow and ice, initially causing flooding,
• followed by droughts, fires, water shortages, famine, heatwaves, starvation,
• resulting in massive biodiversity loss, while infrastructure collapses, and
• the Greenland Ice Sheet and parts of the Antarctic Ice Sheet collapse, causing
• massive flooding of coastal areas, next to a huge rise in temperature,
• while more water vapor in the air causes the temperature rise to speed up further.

[ image from earlier post, also discussed on facebook ]

Climate Emergency Declaration

The situation is dire and unacceptably dangerous, and the precautionary principle necessitates rapid, comprehensive and effective action to reduce the damage and to improve the outlook, where needed in combination with a Climate Emergency Declaration, as described in posts such as in this 2022 post and this 2025 post, and as discussed in the Climate Plan group.



Links

• Japanese National Institute of Polar Research
https://ads.nipr.ac.jp/vishop

• NSIDC - Sea Ice Extent

• Danish Meteorological Institute - Arctic sea ice volume and thickness
https://ocean.dmi.dk/arctic/icethickness/thk.uk.php

• Blue Ocean  Event






Friday, February 23, 2024

Stephen Salter, a giant in combating climate change passes away

   Stephen Salter (2012)
Stephen Hugh Salter, MBE, FRSE, Emeritus Professor of Engineering Design at the University of Edinburgh, was born December 7, 1938, and passed away peacefully on February 23, 2024, at the age of 85.

Stephen Salter was a giant who persisted to dedicate his life to combating climate change, and he did so in many ways until the very end. 

Stephen's work on wave energy led to Salter's Duck (1974), a device able to both generate energy and reduce wave strength. In 1977, Stephen built a multi-directional wave tank at the University of Edinburgh. 

In 2011, Stephen looked at ways to capture methane released in the Arctic, such as by covering lakes and parts of seas by sheets to collect the methane (drawing below).

Empty and filled extruded rubber trough cases with 4 times enlarged views of end and centre

Stephen was perhaps best known for his work on marine cloud brightening, i.e. deploying vessels to spray salt particles into the air in an effort to reduce sea surface temperatures, and thus also reducing sea ice loss and reducing the strength of extreme weather events including storms and hurricanes.

In the video below, Stephen discusses marine cloud brightening in a TEDx talk in 2016. 


Marine cloud brightening | Prof. Stephen Salter | TEDx Talks Published 15 Nov 2016

The image below is from the post Hurricane Moderation at Arctic-news.blogspot.com


In the video below, by theedinburghreporter, Stephen Salter talks about marine cloud brightening.


In the video below, Stephen Salter is interviewed by Nick Breeze (2022). 


Below is a screenshot from the above video by Nick Breeze. 

Stephen Salter discusses sending solar energy back out to space by means of Marine Cloud Brightening.
Screenshot by Sam Carana from video by Nick Breeze.

Stephen Salter (2022): "A jolly small change in reflectivity of the clouds will be sending solar energy back out to space enough to balance what the excess is that's being retained here by greenhouse gases (4:26-4:41). Maybe 10 cubic meters of water a second as sub micron drops sprayed in the right place would offset all the damage we've done since pre-industrial times (5:15-5:24)." 

Our hearts are saddened by this huge loss, and our thoughts are with Stephen's family and his many friends. Stephen's work will not be forgotten.

Added below is a video featuring Stephen Salter, Peter Wadhams, Paul Beckwith, Robert Tulip, Herb Simmens, Alaxandra Price and Win Rampen. 



Links

• Futuristic fleet of 'cloudseeders' - by John Latham (2007)
https://news.bbc.co.uk/2/hi/programmes/6354759.stm

• Sea-going hardware for the cloud albedo method of reversing global warming - by Stephen Salter, Graham Sortino and John Latham (2008)
https://royalsocietypublishing.org/doi/10.1098/rsta.2008.0136

• Can we capture methane from the Arctic seabed? (2011)

• Professor Stephen Salter receives top Academy Award (2012)

• Leading wave energy pioneer Prof Stephen Salter (2012) 
https://www.theengineer.co.uk/content/in-depth/leading-wave-energy-pioneer-prof-stephen-salter

• Coded modulation of computer climate models for the prediction of precipitation and other side-effects of marine cloud brightening (2013)

• Marine cloud brightening | Prof. Stephen Salter | TEDxHeriotWattUniversity |  TEDx talk (2016)
• Hurricane Moderation (2018)
https://arctic-news.blogspot.com/2018/09/hurricane-moderation.html

• Talking to Professor Stephen Salter - TheEdinburghReporter (May 23, 2019)

• Speaking with Professor Stephen Salter - The Edinburgh Report (June 1, 2019)

• Professor Stephen Salter at Holyrood speaking about project to arrest climate change

• John Latham obituary (2021)
https://www.theguardian.com/science/2021/may/30/john-latham-obituay

• Stephen Salter - Whole interview by Nick Breeze ClimateGenn (2022)



Sunday, January 7, 2024

2024 looks to be worse than 2023


The year 2024 looks to be worse than the year 2023. The above chart shows sea surface temperatures that were extremely high in 2023 followed by a steep rise in 2024, crossing 21°C in early January 2024.

The chart below illustrates this further, showing the daily sea surface temperature anomaly using 1 Sep. 1981 to 31 Dec. 2023 data versus the 1982-2011 mean for latitudes between 60°S and 60°N.

The importance of sea surface temperatures

Slowing down of the Atlantic meridional overturning circulation (AMOC) results in less ocean heat reaching the Arctic Ocean and, instead, a huge amount of ocean heat has been accumulating in the North Atlantic in 2023.

Much of the heat in the North Atlantic could soon be pushed abruptly into the Arctic Ocean, as storms can temporarily speed up currents strongly, carrying huge amounts of ocean heat with them into the Arctic Ocean.


The mechanism behind this has been described often in earlier posts and this page. Meltwater and rain can cause a freshwater lid to form and grow at the surface of the North Atlantic and this, in combination with greater stratification as ocean temperatures rise (above image), can enable more ocean heat to increasingly travel underneath this lid from the North Atlantic into the Arctic Ocean, and especially so at times when Jet Stream changes are causing storms that speed up ocean currents along this path.


The danger is illustrated by the above image, showing a forecast for January 11, 2024, with the Jet Stream moving almost vertically over the North Atlantic to the north. The image below shows heat over the North Atlantic, with temperatures reaching as high as 10.5°C or 50.8°F over Greenland (at the green circle) at 1000 hPa on January 10, 2024, 07:00 UTC.


The image below shows 2 meter temperature anomalies on January 11, 2024. 


Very high sea surface temperature anomalies can occur in the path of the Gulf Stream, as illustrated by the image below showing high sea surface temperatures on January 3, 2024, as high as 11.7°C (21°F) at the green circle, over the counterpart of the Gulf Stream in the Pacific, off the coast of Japan. 


Earlier posts have warned about this, such as this post and this video, almost seven years ago. This could cause events during which much ocean heat moves abruptly into the Arctic Ocean, resulting in seafloor methane releases, overwhelming of the latent heat buffer and causing sea ice loss (and thus albedo loss), as well as loss of lower clouds (thus causing further albedo loss), while open oceans are also less efficient than sea ice when it comes to emitting in the far-infrared region of the spectrum and while an ice-free Arctic Ocean will also release more ocean heat into the atmosphere.


Arctic sea ice volume is very low for the time of year, as illustrated by the above image.

A large part of the thicker sea ice is located off Greenland's East Coast, as illustrated by the above image. Much of the sea ice will therefore rapidly disappear as the water heats up in 2024.


The above image, adapted from tropicaltidbits.com, shows a forecast for October 2024 of the 2-meter temperature anomaly in degrees Celsius, based on 1984-2009 model climatology. The anomalies are forecast to be very high for the Arctic Ocean.

In the video below, Jennifer Francis is interviewed by Nick Breeze. 



The importance of daily air temperatures, Northern Hemisphere


[ from the Extinction page ]
The situation is dire. The Northern Hemisphere is getting hit hardest by high temperatures, as illustrated by the above image. 

The Northern Hemisphere is home to some 90% of the world population of more than 8 billion people, with much of them living in South-East Asia.

As more people become aware of the dire situation, widespread panic may set in.

People may stop showing up for work, resulting in a rapid loss of the aerosol masking effect, as industries that now co-emit cooling aerosols (such as sulfates) grind to a halt.

Many people may start to collect and burn more wood, resulting in an increase in emissions that speed up the temperature rise.

As temperatures rise, more fires could also break out in forests, peatlands and urban areas including landfills and waste dumps, further contributing to emissions that speed up the temperature rise.

The image on the right illustrates how fast a huge temperature could unfold.

As a somewhat sobering footnote, humans will likely go extinct with a 3°C rise and most life on Earth will disappear with a 5°C rise, as discussed in an earlier post.


Climate Emergency Declaration

The situation is dire and the precautionary principle calls for rapid, comprehensive and effective action to reduce the damage and to improve the situation, as described in this 2022 post, where needed in combination with a Climate Emergency Declaration, as discussed at this group.



Links
• Climate Reanalyzer 
https://climatereanalyzer.org

• Nullschool

• Danish Meteorological Institute - Arctic sea ice volume and thickness
https://ocean.dmi.dk/arctic/icethickness/thk.uk.php

• New Record Ocean Temperatures and Related Climate Indicators in 2023 - by Lijing Checg et al. (2024)

• Cold freshwater lid on North Atlantic
https://arctic-news.blogspot.com/p/cold-freshwater-lid-on-north-atlantic.html

• Extinction







Saturday, May 22, 2021

Arctic Ocean invaded by hot, salty water


Sea surface temperatures on the Northern Hemisphere have been rising dramatically over the years, as illustrated by above image, indicating that the latent heat tipping point is getting crossed, while the methane hydrates tipping point could get crossed soon, depending on developments.

At the moment, the surface temperature of most of the Arctic ocean's is still below 0°C.

Heat is entering the Arctic Ocean from the south, as illustrated by the image on the right. Hot, salty water is entering the Arctic Ocean from the Atlantic Ocean as currents dive underneath the ice, causing the ice to melt from below. 
[ click on images to enlarge ]

The image on the right, from the NSIDC article A step in our Spring, compares sea ice age between March 12 to 18 for the years 1985 (a) and 2021 (b).

The bottom graph (c) shows a time series from 1985 to 2021 of percent ice coverage of the Arctic Ocean domain. The Arctic Ocean domain is depicted in the inset map with purple shading.

At the end of the ice growth season in mid-March, 73.3% of the Arctic Ocean domain was covered by first-year ice, while 3.5% was covered by ice 4+ years old. 

This compares to 70.6% and 4.4% respectively in March 2020.

In March 1985, near the beginning of the ice age record, the Arctic Ocean region was comprised of nearly equal amounts of first-year ice (39.3%) and 4+ year-old ice (30.6%).

Sea ice that hasn't yet survived a summer melt season is referred to as first-year ice. This thin, new ice is vulnerable to melt and disintegration in stormy conditions. Ice that survives a summer melt season can grow thicker and less salty, since snow that thickens the ice contains little salt. Thickness and salt content determine the resistance of the ice to melt. Multiyear ice is more likely to survive temperatures that would melt first-year ice, and to survive waves and winds that would break up first-year ice.

The image on the right shows a forecast of the thickness of the sea ice, run on May 20, 2021 and valid for May 21, 2021. 

An area is visible north of Severnaya Zemlya toward the North Pole where thickness is getting very thin, while there is one spot where the ice has virtually disappeared. 

The spot is likely a melting iceberg, the animation on the right shows that the spot has been there for quite a few days, while the freshwater in this spot appears to result from melting amid salty water. 

Overall, sea ice is getting very thin, indicating that the buffer constituted by the sea ice underneath the surface is almost gone, meaning that further heat entering the Arctic Ocean will strongly heat up the water. 

As the animation underneath on the right shows, freshwater is entering the Arctic Ocean due to runoff from land, i.e. rainwater from rivers, meltwater from glaciers and groundwater runoff from thawing permafrost. 

At the same time, very salty water is entering the Arctic Ocean from the Atlantic Ocean. 

The map below shows how salty and hot water from the Atlantic Ocean enters the Arctic Ocean along two currents, flowing on each side of Svalbard, and meeting at this area north of Severnaya Zemlya where thickness is getting very low. 

The blue color on the map indicates depth (see scale underneath). 

The image below, by Malcolm Light and based on Max & Lowrie (1993), from a recent post, shows vulnerable Arctic Ocean slope and deep water methane hydrates zones below 300 m depth. 

Malcolm Light indicates three areas: 
Area 1. Methane hydrates on the slope;
Area 2. Methane hydrates on the abyssal plane; 
Area 3. Methane hydrates associated with the spreading Gakkel Ridge hydro-thermal activity (the Gakkel Riidge runs in between the northern tip of Greenland and the Laptev Sea). 


The freezing point of freshwater is 0°C or 32°F. For salty water, the freezing point is -2°C or 28.4°F.

During April 2021, sea ice was about 160 cm thick.

In June and July 2021, thickness will fall rapidly, as illustrated by the image on the right by Nico Sun. 

Sea ice acts as a buffer, by consuming energy in the process of melting, thus avoiding that this energy causes a temperature rise of the water. 

As long as there is sea ice in the water, this sea ice will keep absorbing heat as it melts, so the temperature will not rise at the sea surface and remain at zero°C. The amount of energy that is consumed in the process of melting the ice is as much as it takes to heat an equivalent mass of water from zero°C to 80°C.

The accumulated ice melt energy until now is the highest on record, as illustrated by the image on the right, by Nico Sun.

The image below further illustrate the danger. As the temperature of the water keeps rising, more heat will reach sediments at the seafloor of the Arctic Ocean that contain vast amounts of methane, as discussed at this page and in this post.

Ominously, methane levels reached a peak of 2901 ppb at 469 mb on May 13, 2021. 

Research

In the extract of a 2008 paper, Natalia Shakhova et al. conclude: ". . we consider release of up to 50 Gt of predicted amount of hydrate storage as highly possible for abrupt release at any time."


The video below contains excerpts from Nick Breeze's interview with Natalia Shakhova at the European Geophysical Union in Vienna, 2012, on the likelihood and timeframe of a large methane release from the seafloor of the Arctic Ocean. 

Natalia Shakhova: "The total amount of methane in the atmosphere is about 5Gt. The amount of carbon in the form of methane in this Arctic shelf is - approximately - from hundreds to thousands Gt and, of course, only 1% of [such an] amount is required to double the atmospheric burden of methane."

"But to destabilize 1% of this carbon pool, I think, not much effort is needed, considering the state of the permafrost and the amount of methane involved, because what divides the methane from the atmosphere is a very shallow water column and the weakening permafrost, which is losing its ability to seal, to serve as a seal, and this is, I think, not a matter of thousands of years, it's a matter of decades, at most hundred years." 

(Natalia talks with Igor Semiletov)
Natalia Shakhova: "Just because this area is seismically and tectonically active, and there was some investigation that the tectonic activity was increasing, and the seismic activity, the destabiliation of the ground, just mechanical forcing destabiliation [may suffice to act as] additional pathway for this methane to escape. There are many factors that are very convincing for us [to conclude] that it might happen."

Elaborating on the timeframe.
Natalia Shakhova: "Not any time, any time sounds like it might happen today, it might happen tomorrow, the day after tomorrow . . " 
Igor Simelitov: "It might!"


The image below was created with content from a 2019 paper by Natalia Shakhova et al. It concludes that methane releases could potentially increase by 3-5 orders of magnitude, considering the sheer amount of methane preserved within the shallow East Siberian Arctic Shelf seabed deposits and the documented thawing rates of subsea permafrost reported recently.

In a 2021 paper by researchers from Europe, Russia and the U.S., results from field research are published showing that methane is getting released from locations deep below the submarine permafrost. Lead author, Julia Steinbach, from Stockholm University, says: “The permafrost is a closed lid over the seafloor that’s keeping everything in place. And now we have holes in this lid.” 

In the video below, Nick Breeze interviews Igor Semiletov on methane plumes detected during this 2020 field research over the East Siberian Arctic Shelf (ESAS).


In the video below, Nick Breeze interviews Örjan Gustafsson on field research on methane in the East Siberian Arctic Shelf (ESAS)


In the video below, Peter Wadhams analyses the threat of Arctic methane releases.


In the video below, Guy McPherson discusses the situation.


In conclusion, temperatures could rise dramatically soon. A 3°C will likely suffice for humans to go extinct, making it in many respects rather futile to speculate about what will happen in the longer term. On the other hand, the right thing to do is to help avoid the worst things from happening, through comprehensive and effective action as described in the Climate Plan.

Links

• NOAA Climate at a Glance

• Danish Meteorological Institute - Arctic temperature
http://ocean.dmi.dk/arctic/meant80n.uk.php

• Freezing point of water - Climate Change: Arctic sea ice

• Arctic surface temperature

• NSIDC: A step in our Spring, image credit: T. Tschudi, University of Colorado, and W. Meier and J.S. Stewart, National Snow and Ice Data Center/Image by W. Meier

• Arctic sea ice - thickness and salinity - navy.mil
https://www7320.nrlssc.navy.mil/GLBhycomcice1-12/arctic.html

• CryosphereComputing - by Nico Sun
https://cryospherecomputing.tk

• A 4.5 km resolution Arctic Ocean simulation with the global multi-resolution model FESOM 1.4 - by Qiang Wang et al. 

• Max, M.D. & Lowrie, A. 1993. Natural gas hydrates: Arctic and Nordic Sea potential. In: Vorren, T.O., Bergsager, E., Dahl-Stamnes, A., Holter, E., Johansen, B., Lie, E. & Lund, T.B. Arctic Geology and Petroleum Potential, Proceedings of the Norwegian Petroleum Society Conference, 15-17 August 1990, Tromso, Norway. Norwegian Petroleum Society (NPF), Special Publication 2 Elsevier, Amsterdam, 27-53.
https://www.elsevier.com/books/arctic-geology-and-petroleum-potential/vorren/978-0-444-88943-0

• Extinction by 2027- by Malcolm Light
https://arctic-news.blogspot.com/2021/05/extinction-by-2027.html


• Anomalies of methane in the atmosphere over the East Siberian shelf: Is there any sign of methane leakage from shallow shelf hydrates? - by Shakhova, Semiletov, Salyuk and Kosmach (2008)
https://www.cosis.net/abstracts/EGU2008/01526/EGU2008-A-01526.pdf

• Understanding the Permafrost–Hydrate System and Associated Methane Releases in the East Siberian Arctic Shelf - by Natalia Shakhova, Igor Semiletov and Evgeny Chuvilin 
https://www.mdpi.com/2076-3263/9/6/251

• A Massive Methane Reservoir Is Lurking Beneath the Sea