Global sea ice area was 13.00 million km² on February 9, 2025, a deviation (1981-2000 base) of -5.75 σ and the lowest area on record, as illustrated by the image below, adapted from seaice.visuals.earth.
What is the difference between sea ice area and extent? Extent is the total region with at least 15% sea ice cover. Extent can include holes or cracks in the sea ice and melt ponds on top of the ice, all having a darker color than ice. Sea ice area is the total region covered by ice alone.
Therefore, sea ice area is a critical measure in regard to albedo. Loss of sea ice area is a self-reinforcing feedback that causes the temperature to rise, resulting in further melting of sea ice, thus accelerating the temperature rise.
A Blue Ocean Event is often defined as crossing a tipping point that is crossed when sea ice falls below 1 million km² in extent. Doesn't it make more sense to look at sea ice area, rather than at sea ice extent?
Loss of albedo as a result of loss in sea ice is only one out of many feedbacks that come with rising temperatures, as described at the Threat.
Antarctic sea ice
There are many mechanisms that are driving up, if not accelerating the temperature rise and loss of sea ice.
Sea ice thickness is another important measure. The image below shows Antarctic sea ice thickness on four different dates, including February 4, 2025, from the University of Bremen.
The image below shows Antarctic sea ice thickness on February 7, 2025.
The image below shows that the Arctic temperature, i.e. at latitudes higher than 80°N, on February 6, 2025, was much higher than the mean temperature for the period 1959-2002.
The image below shows Antarctic sea ice thickness on February 7, 2025.
For a comparison of Antarctic sea ice thickness at earlier dates, also have a look at this earlier post.
Arctic sea ice
As illustrated by the image below, there are at least seven mechanisms that can accelerate the rise in surface temperatures, and thus in turn accelerating sea ice decline and further accelerating the temperature rise.
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[ from the earlier post Double Blue Ocean Event 2025? and discussed here ] |
The image below shows Arctic sea ice extent up to February 8, 2025. During the first few months of the year, Arctic sea ice extent is growing, but this recently stopped and extent was at a record low for the time of year on February 8, 2025, despite La Niña conditions. The red line and red marker shows 2025 sea ice. Dots mark sea ice extent on February 8 for the respective year.
As said, extent is only one way the sea ice can be measured; another way is to measure sea ice area. Furthermore, 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.
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[ from earlier post ] |
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[ Arctic sea ice volume, click to enlarge ] |
The image on the right shows Arctic sea ice volume up to February 10, 2025. Arctic sea ice volume in 2024 and 2025 has been much lower than in previous years.
More incoming heat therefore threatens to reach the seafloor of the Arctic Ocean and destabilize methane hydrates contained in sediments at the seafloor, resulting in eruptions of huge amounts of methane, as illustrated by the above image.
Following the influx of ocean heat from the North Atlantic into the Arctic Ocean, methane peaks above 2400 ppb were recorded by three different satellites, as illustrated by the image below, i.e.
2413 ppb at 399.1 mb by the N20 satellite on February 2, 2025 (left),
2413 ppb at 399.1 mb by the N20 satellite on February 2, 2025 (left),
2469 ppb at 399.1 mb by the N21 satellite on February 2, 2025 (center), and
2446 ppb at 487.2 mb by the Metop-C satellite on February 3, 2025 (right).
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[ Methane peaks above 2400 ppb on Feb 2 & 3, 2025, click to enlarge ] |
Arctic temperature rise
As said before, rising temperatures come with many feedbacks, such as albedo loss and loss of the latent heat buffer. Feedbacks can contribute strongly to further acceleration of the temperature rise. Another feedback is more water vapor ending up in the atmosphere, as illustrated by the image below.
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[ from earlier post ] |
A new El Niño may emerge in the course of 2025, while Arctic sea ice extent, area thickness and volume are all at record low, while numerous self-reinforcing feedbacks are kicking in with accelerating ferocity and while further mechanisms are accelerating the temperature rise, such as high sunspots and reductions in cooling aerosols, which could lead to a huge temperature rise and an Arctic Blue Ocean Event in 2025, threatening huge amounts of methane to erupt from the seafloor — yet another feedback that comes with rising temperatures.
Ominously, very high temperature anomalies are forecast over the Arctic Ocean for November 2025.
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[ Very high temperature anomalies forecast over Arctic Ocean, click to enlarge ] |
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.
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
• Kevin Pluck - seaice.visuals.earth
https://seaice.visuals.earth
• Albedo, latent heat, insolation and more
https://arctic-news.blogspot.com/p/albedo.html
• Feedbacks
https://arctic-news.blogspot.com/p/feedbacks.html
• Heat flux forecast to enter Arctic early February 2025
https://arctic-news.blogspot.com/2025/01/heat-flux-forecast-to-enter-arctic-early-february-2025.html
• Danish Meteorological Institute - daily temperature Arctic
https://ocean.dmi.dk/arctic/meant80n.uk.php
• Danish Meteorological Institute - Arctic sea ice volume and thickness
https://ocean.dmi.dk/arctic/icethickness/thk.uk.php
• Arctic and Antarctic Data Archive System (ADS) of the National Institute of Polar Research of Japan
https://ads.nipr.ac.jp
• Climate Reanalyzer
https://climatereanalyzer.org
• University of Bremen - sea ice
https://seaice.uni-bremen.de/start
• Tropical Tidbits
https://www.tropicaltidbits.com
• Transforming Society
https://arctic-news.blogspot.com/2022/10/transforming-society.html
• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html
• Climate Emergency Declaration
https://arctic-news.blogspot.com/p/climate-emergency-declaration.html
• Danish Meteorological Institute - daily temperature Arctic
https://ocean.dmi.dk/arctic/meant80n.uk.php
• Danish Meteorological Institute - Arctic sea ice volume and thickness
https://ocean.dmi.dk/arctic/icethickness/thk.uk.php
• Arctic and Antarctic Data Archive System (ADS) of the National Institute of Polar Research of Japan
https://ads.nipr.ac.jp
• Climate Reanalyzer
https://climatereanalyzer.org
• University of Bremen - sea ice
https://seaice.uni-bremen.de/start
• Tropical Tidbits
https://www.tropicaltidbits.com
• Transforming Society
https://arctic-news.blogspot.com/2022/10/transforming-society.html
• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html
• Climate Emergency Declaration
https://arctic-news.blogspot.com/p/climate-emergency-declaration.html