This is a revised version of my
#sciencecommunication article about the effect of
#greenhousegas #outgassing from
#thawing #permafrost. I have updated aspects of the
#illustrations created using
#AI and my manual storyboards. I have also added further information to the text.
Several factors can help prevent further increases in greenhouse gases during
#globalwarming, in addition to
#humancaused #emissions. For example, ocean floors can generally bind carbon dioxide. Permafrost can also play a significant role, as large parts of our
#NorthernHemisphere are (still) covered by permafrost, along with smaller parts of the Southern Hemisphere and portions of the
#oceanfloor.
Our
#polarregions are particularly vulnerable to global warming, which is primarily caused by humans. The poles, in particular, are largely responsible for the concrete
#climaticimpacts worldwide, as they influence both climate-forming
#aircurrents and climate-influencing
#oceancurrents. Detailed and technologically up-to-date studies on the stability of greenhouse gases bound in the soil are therefore crucial for the
#future.
It is known that
#frozen permafrost acts as a
#barrier that prevents the release of greenhouse gases such as
#methane and
#carbondioxide, and it can also reduce the formation of these gases. However, it has not yet been thoroughly investigated how this barrier changes with increasing
#permeability as a result of melting due to the global
#climatechange.
Using a specially developed
#pycnopermeameter, the authors PWJ Glover et al. (2026) addressed the question of the
#magnitude of changes in the permeability of this previously reliable protective barrier during thawing and
#refreezing.
According to the researchers, the permeability increases by several orders of magnitude during thawing, specifically from 4.94 mD to 112.54 mD and from 0.26 mD to 21.43 mD, respectively, in the samples studied. The study data indicate that the
#highestpermeability occurs in the
#temperaturerange of -5 °C to -1 °C. Upon refreezing, the permafrost fully returns to its original state as a barrier, except for a time lag (
#hysteresis). The authors believe their findings can contribute to the integration of permafrost data into general
#climatemodels.
Precise scientific climate models, which illuminate the causes and effects of global climate change from many different perspectives, help us to take measures to mitigate future deterioration of our living conditions as much as possible. Naturally, any general effort to reduce our own greenhouse gas emissions is the most important foundation. But we also need to know what we can do to best protect important binding sites for CO2 and methane, such as our green biospheres, the sediments of marine and freshwater grounds, and also permafrost soils.
#Basicresearch must also develop technological innovations that make greater climate neutrality possible in the first place. Furthermore, we need concrete action models to secure food and water supplies for future generations. This includes knowledge on optimizing agricultural soils, developing new food resources, efficient alternative energy production, and ultimately, even knowledge about which
#resources we can additionally obtain from space will be important.
©
#StefanFWirth, Berlin, April 2026
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Reference:
PWJ Glover et al. (2026):
doi.org/10.1029/2025EF007232
Pictures:
© Stefan F. Wirth, AI assisted illustrations based in my handmade storyboard sketches, manually edited, April 2026, Berlin
1) permafrost landscape with hypothetical section through the ground
2) permafrost
#landscape with hypothetical section through the ground, emphasizing the ground composition and indicating melting
#icelayers due to global warming with outgassing greenhouse gases