Above image, from the National Institute of Polar Research in Japan, shows Arctic sea ice extent at a record low for the time of year, on July 4, 2021, at 8.4 million km².
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| [ for earlier animations, see discussions ] |
Arctic sea ice is getting very thin rapidly, threatening the latent heat tipping point to get crossed soon.
The U.S. Navy animation on the right shows Arctic sea ice thickness (in m) for the 30 days up to July 31, 2021, with eight days of forecasts included.
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| [ disappearing sea ice north of Greenland ] |
An often-used threshold for a Blue Ocean Event (BOE) is that a BOE occurs when sea ice extent falls below 1 million km². Similarly, a threshold for the latent heat tipping point of Arctic sea ice could be sea ice thickness.
Disappearance of the buffer constituted by subsurface sea ice could be measured by a threshold of most sea ice becoming less than 0.5 meter thin. By that measure, the buffer is now virtually gone, implying that virtually no further heat arriving from the Atlantic Ocean and the Pacific Ocean in the Arctic Ocean can be absorbed in the process of melting of the sea ice.
The NASA Worldview image on the right shows the sea ice on July 29, 2021, north of Greenland, where once the thickest sea ice was located.
As sea ice gets thinner, ever less ocean heat gets consumed in the process of melting the subsurface ice, to the point where there is only a thin layer of ice left at the surface. While this thin layer of ice may remain at the surface for as long as air temperatures are still low enough, and this ice will still consume some heat at the bottom, at the same time it acts as a seal, preventing heat from the Arctic Ocean to enter the atmosphere.
Albedo loss, latent heat loss, storms and changes to the jet stream can add up to dramatically amplify the temperature rise of the water in the Arctic Ocean, which comes with the danger of destabilization of hydrates at its seafloor, resulting in eruption of huge amounts of methane from hydrates and opening up pathways for release of even further amounts of free gas from underneath these hydrates, as illustrated by the image below.
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And while the situation in 2021 is dire, the outlook for the years beyond 2021 is that things look set to get progressively worse.
This situation in 2021 is the more remarkable given that we’re in a La Niña period, as illustrated by the NOAA image on the right showing a forecast issued July 5, 2021, that indicates that La Niña is expected to reach a new low by the end of 2021.
Sunspots are on the rise. We were at a low point in the sunspot cycle late 2019/early 2020. As the image on the right shows, the number of sunspots is rising and can be expected to rise further as we head toward 2026, and temperatures can be expected to rise accordingly.
According to James Hansen et al., the variation of solar irradiance from solar minimum to solar maximum is of the order of 0.25 W/m⁻².
So, the outlook is grim. The right thing to do now is to help avoid the worst things from happening, through immediate, comprehensive and effective action as described in the Climate Plan.
Links
• National Institute of Polar Research (NIPR) in Japan
https://ads.nipr.ac.jp/vishop
• The National Snow and Ice Data Center (NSIDC) at the University of Colorado Boulder
https://nsidc.org/arcticseaicenews/charctic-interactive-sea-ice-graph
• NOAA ENSO Evolution
https://www.cpc.ncep.noaa.gov/products/analysis_monitoring/lanina/enso_evolution-status-fcsts-web.pdf
https://www7320.nrlssc.navy.mil/GLBhycomcice1-12/arctic.html
• Latent heat
https://arctic-news.blogspot.com/p/latent-heat.html
• University of Bremen – sea ice
https://seaice.uni-bremen.de
• Aerosols
https://arctic-news.blogspot.com/p/aerosols.html
• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html