The image on the right shows a NASA Worldview satellite image of a blue Beaufort Sea (with Barrow, Alaska, at the top left, on September 7, 2022).
The image shows that there is a lot of open water between the coast of Alaska and the sea ice.
Such a satellite image provides a visual way to determine how much sea ice is present. It can be hard to determine where there is open water and where the sea ice starts; the sea ice is often covered by clouds; furthermore, even when there are no clouds, the question remains what is to be regarded as sea ice and what is to be regarded as water.
The image shows that there is a lot of open water between the coast of Alaska and the sea ice.
Such a satellite image provides a visual way to determine how much sea ice is present. It can be hard to determine where there is open water and where the sea ice starts; the sea ice is often covered by clouds; furthermore, even when there are no clouds, the question remains what is to be regarded as sea ice and what is to be regarded as water.
Another way to measure how much sea ice is there is to look at sea ice concentration. Sea ice concentration in the Central Arctic region has been very low for some time.
The image on the right, from an earlier post, shows that on August 12, 2022, sea ice concentration in a large area close to the North Pole was as low as 0%. In the two images below, Nico Sun calculates the impact of albedo loss based on NSIDC sea ice concentration data. The images illustrate why sea ice loss in the Central Arctic region is so important.
Arctic sea ice has become extremely thin, so the latent heat buffer loss is also very strong. This loss of the latent heat buffer can continue to result in higher temperatures of the water for a long time, even long after insolation has passed its annual peak on the Northern Hemisphere, thus causing the combined accumulative impact to continue to be high.
The image below shows that further albedo loss in the Barents Sea, which is virtually icefree at the moment, doesn't make much difference now.
The image below shows that, by contrast, more albedo loss in the Central Arctic region makes much more difference, even in September.
Another way to measure how much sea ice is present is to look at the extent of the sea ice. According to many, a Blue Ocean Event starts once the Arctic sea ice falls below 1 million km² in extent.
Here is another example of such a scenario. Recent studies indicate that human-caused climate change will soon increase El Niño frequency and intensity. Accordingly, the upcoming El Niño may well be strong. As illustrated with above image, we're currently in the depth of a persistent La Niña, which suppresses the temperature rise, whereas the opposite occurs during El Niño, which amplifies the temperature rise, and this especially affects the Arctic, which is already heating up much faster than the rest of the world. Also, the upcoming El Niño may very well coincide with a peak in sunspots in 2025, further pushing up temperatures.
In the video below, from this page, Guy McPherson addresses the question: Has the “Methane Bomb” Been Triggered?
• NASA Worldview
• Nico Sun - CryosphereComputing
• More Frequent El Niño Events Predicted by 2040
Cutting-edge models predict that El Niño frequency will increase within 2 decades because of climate change, regardless of emissions mitigation efforts.
• Emergence of climate change in the tropical Pacific - by Yun Ying et al.
Arctic sea ice extent was 4.912 million km² on September 6, 2022, which is larger than the extent in many previous years around this time of year (see NSIDC image below). However, the sea ice has become very thin, resulting in many areas where only small pieces of ice are present.
NSIDC regard a cell to have sea ice if it has at least 15% sea ice, but when regarding a cell to have sea ice if it has at least 50% ice and if that's the case for ⅕ of the cells where there is (some) ice, then we're already in a Blue Ocean Event right now.
So let's have another look at how much of the above 4.912 million km² can be regarded as sea ice, by using the NSIDC map with sea ice concentration as a guide.
The roughly-sketched outline drawn over the NASA map below indicates that there may only have been some 991 thousand km² of concentrated sea ice left on September 6, 2022 (inset shows NSIDC sea ice concentration for the day).
The roughly-sketched outline drawn over the NASA map below indicates that there may only have been some 991 thousand km² of concentrated sea ice left on September 6, 2022 (inset shows NSIDC sea ice concentration for the day).
As said, it's a rough sketch, so some cells with a higher concentration of sea ice may have been left out. Having said that, we're currently in the depth of a persistent La Niña and the associated lower air temperatures contribute to a relatively larger sea ice extent than would otherwise be the case.
In conclusion, depending on what is counted as sea ice, we could already be experiencing a Blue Ocean Event right now.
In conclusion, depending on what is counted as sea ice, we could already be experiencing a Blue Ocean Event right now.
Further events and developments
A Blue Ocean Event constitutes the crossing of a huge tipping point and, as a strong El Niño looks set to emerge, this could trigger the unfolding of further events and developments leading to extinction of most species (including humans), as:
- a strong El Niño triggers:
- further decline of the Arctic sea ice, with loss of the latent heat buffer, combined with
- associated loss of sea ice albedo and
- destabilization of seafloor methane hydrates, causing eruption of vast amounts of methane that further speed up Arctic warming and cause
- rapid thawing of terrestrial permafrost, resulting in even more emissions,
- while the Jet Stream gets even more deformed, resulting in more extreme weather events
- causing forest fires, at first in Siberia and Canada and
- eventually also in the peat fields and tropical rain forests of the Amazon, in Africa and South-east Asia, resulting in
- decline of snow and ice on mountains, at first causing huge flooding, followed by
- drought, heatwaves and urban collapse,
- collapse of the Greenland and West-Antarctic ice sheets,
- falling away of aerosol masking as civilization grinds to a halt,
- further heating due to gases and particulates from wood and waste burning and biomass decomposition, and
- further heating due to additional gases (including water vapor), cirrus clouds, albedo changes and heat rising up from oceans.
Importantly, depicted above is only one scenario out of many. Things may eventuate in different order and occur simultaneously, i.e. instead of one domino tipping over the next one sequentially, many events may occur simultaneously and reinforce each other. Further events and developments could be added to the list, such as ocean stratification and stronger storms that can push large amounts of warm salty water into the Arctic Ocean.
Here is another example of such a scenario. Recent studies indicate that human-caused climate change will soon increase El Niño frequency and intensity. Accordingly, the upcoming El Niño may well be strong. As illustrated with above image, we're currently in the depth of a persistent La Niña, which suppresses the temperature rise, whereas the opposite occurs during El Niño, which amplifies the temperature rise, and this especially affects the Arctic, which is already heating up much faster than the rest of the world. Also, the upcoming El Niño may very well coincide with a peak in sunspots in 2025, further pushing up temperatures.
The image below shows that the rise in sea surface temperatures on the Northern Hemisphere has been suppressed during the ongoing La Niña, but as we move into the next El Niño, the seafloor methane tipping point could be crossed even earlier than the current trend indicates, say by 2025.
One reason for this is that the narrowing temperature difference between the Arctic and the Tropics will further deform the Jet Stream and in turn cause more extreme weather, leading to more loss of sea ice and thus of its capacity to reflect sunlight and act as a buffer against incoming ocean heat.
A huge amount of heat has built up in the North Atlantic off the coast of North America, as illustrated by the image on the right.
Furthermore, the temperature of the water may well be substantially higher some 50 meter below the sea surface than at the sea surface.
A huge amount of heat has built up in the North Atlantic off the coast of North America, as illustrated by the image on the right.
Furthermore, the temperature of the water may well be substantially higher some 50 meter below the sea surface than at the sea surface.
As discussed in an earlier post, rising temperatures result in stronger winds along the path of the Gulf Stream that can make huge amounts of warm, salty water travel from the Atlantic Ocean toward the Arctic and reach shallow parts of the Arctic Ocean such as the East Siberian Arctic Shelf (ESAS), where most of the sea is less than 50 m deep. The danger is illustrated by the Argo float compilation below.
Very high methane levels
The image below, from an earlier post, shows annual global mean methane with a trend added that points at a methane rise that could in 2028 represent a forcing of 780 ppm CO₂e (with a 1-year GWP of 200).
NOAA's globally averaged marine surface mean for April 2022 was 1909.9 ppb. The above image shows that, on September 4, 2022 am, the MetOp satellite recorded a mean methane concentration of 1904 ppb at 586 mb, which is close to sea level. At 293 mb, however, the MetOp satellite recorded a mean of 1977 ppb, while at 218 mb it recorded a peak of 2805 ppb.
Such high methane levels could be caused by destabilization of methane hydrates at the seafloor of the Arctic Ocean, with large amounts of methane erupting (increasing 160 x in volume) and rising up at accelerating speed through the water column (since methane is lighter than water), concentrated in the form of plumes, which makes that less methane gets broken down in the water by microbes and in the air by hydroxyl, of which there is very little in the Arctic in the first place. Such a methane eruption entering the atmosphere in the form of a plume can be hard to detect as long as it still doesn't cover enough of the 12 km in diameter footprint to give a pixel the color associated with high methane levels.
In other words, the clouds tipping point at 1200 ppm CO₂e could be crossed in 2028 due to the forcing of methane and CO₂ alone, assuming that CO₂ concentration in 2028 will exceed 420 ppm. Moreover, this could happen even earlier, since there are further forcers, while further events and developments could additionally push up the temperature further, as discussed above. Furthermore, the NOAA data used in the above image are for marine surface measurements. More methane tends to accumulate at higher altitudes, as illustrated by the compilation image below.
NOAA's globally averaged marine surface mean for April 2022 was 1909.9 ppb. The above image shows that, on September 4, 2022 am, the MetOp satellite recorded a mean methane concentration of 1904 ppb at 586 mb, which is close to sea level. At 293 mb, however, the MetOp satellite recorded a mean of 1977 ppb, while at 218 mb it recorded a peak of 2805 ppb.
Such high methane levels could be caused by destabilization of methane hydrates at the seafloor of the Arctic Ocean, with large amounts of methane erupting (increasing 160 x in volume) and rising up at accelerating speed through the water column (since methane is lighter than water), concentrated in the form of plumes, which makes that less methane gets broken down in the water by microbes and in the air by hydroxyl, of which there is very little in the Arctic in the first place. Such a methane eruption entering the atmosphere in the form of a plume can be hard to detect as long as it still doesn't cover enough of the 12 km in diameter footprint to give a pixel the color associated with high methane levels.
The above Copernicus image shows a forecast for September 9, 2022 18 UTC, of methane at 500 hPa.
Conclusion
The situation is dire and the right thing to do now is to help avoid or delay the worst from happening, through action as described in the Climate Plan.
Links
• NSIDC - Frequently asked questions
• NSIDC - sea ice concentration
• NSIDC - sea ice extent
Cutting-edge models predict that El Niño frequency will increase within 2 decades because of climate change, regardless of emissions mitigation efforts.
https://www.nature.com/articles/s41558-022-01301-z
• Monitoring of atmospheric composition using the thermal infrared IASI/MetOp sounder - by C. Clerbaux et al.
• NOAA - ENSO: Recent Evolution, Current Status and Predictions
https://www.cpc.ncep.noaa.gov/products/analysis_monitoring/lanina/enso_evolution-status-fcsts-web.pdf
• WMO predicts first “triple-dip” La Niña of the century
• Albedo
https://arctic-news.blogspot.com/p/albedo.html
• Latent Heat
https://arctic-news.blogspot.com/p/latent-heat.html
• Albedo, latent heat, insolation and more
https://arctic-news.blogspot.com/p/albedo.html
• Jet Stream
https://arctic-news.blogspot.com/p/jet-stream.html
• Feedbacks
https://arctic-news.blogspot.com/p/feedbacks.html
• Blue Ocean Event
https://arctic-news.blogspot.com/p/blue-ocean-event.html
• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html
• Climate Reanalyzer
• Argo Float
• NOAA - MetOp satellite methane data
• Copernicus methane forecasts
• Clouds feedback and tipping point
• NOAA - global methane
• NOAA - Sea surface temperature anomalies on the Northern Hemisphere
• NOAA - Monthly Temperature Anomalies Versus El Niño
• NOAA - ENSO: Recent Evolution, Current Status and Predictions
https://www.cpc.ncep.noaa.gov/products/analysis_monitoring/lanina/enso_evolution-status-fcsts-web.pdf
• WMO predicts first “triple-dip” La Niña of the century
https://public.wmo.int/en/media/press-release/wmo-predicts-first-%E2%80%9Ctriple-dip%E2%80%9D-la-ni%C3%B1a-of-century
• Arctic sea ice August 2022
• Arctic sea ice August 2022
• Albedo
https://arctic-news.blogspot.com/p/albedo.html
• Latent Heat
https://arctic-news.blogspot.com/p/latent-heat.html
• Albedo, latent heat, insolation and more
https://arctic-news.blogspot.com/p/albedo.html
• Jet Stream
https://arctic-news.blogspot.com/p/jet-stream.html
• Feedbacks
https://arctic-news.blogspot.com/p/feedbacks.html
• Blue Ocean Event
https://arctic-news.blogspot.com/p/blue-ocean-event.html
• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html