
What makes current conditions even more dire is that not only are concentrations of CO₂ extremely high (without match going back millions of years) and rising, but the speed at which CO₂ is currently rising is also unprecedented, while additionally there has been an increase in total solar irradiance of ∼400 Wm⁻² since the formation of the Earth. The image below shows the combined climate forcing by changing CO₂ and solar output for the past 450 million years.
Between 14 and 15 million years ago, the temperature in central Europe was 20°C higher than today, as illustrated by the image below (adapted from a 2020 study by Methner et al.).
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| [ from earlier post, click on images to enlarge ] |
Concentrations of carbon dioxide haven't been this high for millions of years, as confirmed by recent analysis led by Sarah Shackleton and Julia Marks-Peterson. Their analysis finds that, while the average temperature of the ocean has decreased by 2 to 2.5°C over the past 3 million years, average atmospheric carbon dioxide levels have likely remained below 300 parts per million over this time. Methane levels have also remained relatively stable. This makes the recent daily concentration of 433.95 ppm at Mauna Loa and the high recent methane levels (see earlier post) even more threatening and it means that, in addition to the key role of heat-trapping greenhouse gases, there were important contributions from other components of the climate system such as Earth’s reflectivity, variations in vegetation and/or ice cover and ocean circulation.
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| [ from earlier post, discussed on facebook ] |
The image below shows a worrying recent rise in concentrations of sulfur hexafluoride (SF6), which has a global warming potential (GWP) over 100 years of 24,300 and, because it has a lifetime of 1000 years, its GWP over 500 years is even higher, i.e. 29,000 (IPCC AR6).
As temperatures rise, the outgoing longwave radiation (in black) has not risen as fast as the absorbed incoming solar radiation (in orange), due to high (and rising) concentrations of greenhouse gases and loss of albedo, resulting in an increasingly larger amount of extra energy stored on Earth. The image below, from an earlier post, depicts Earth energy imbalance (in red).
Where does the extra energy go? According to the IPCC AR6 WG1, 91% of the extra energy is taken up by oceans, 5% by land, 3% by ice melting and 1% remains in the atmosphere. Oceans, land and melting ice thus act as a buffer that did take up the vast majority (99%) of the extra energy, based on IPCC data. In the image below, by Leon Simons, absorbed solar radiation is colored in black, while outgoing longwave radiation is colored red.
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| [ image by Leon Simons, discussed on facebook ] |
- Oceans
The ocean's capacity to act as an energy buffer is increasingly compromised by stratification, changes to ocean currents, changes in salinity, ocean oxygen depletion, acidification and more, as discussed in earlier posts such as this one. This is a big issue, since oceans take up 91% of the extra heat caused by greenhouse gases, so if there is even a 1% reduction in the heat taken up by oceans, the heat remaining in the atmosphere may double.
- Ice
Furthermore, the capacity for ice to act as a buffer by consuming energy in the process of melting is increasingly compromised by sea ice decline, by retreat of glaciers, and by darkening of ice due to dust, algae, black carbon and more. Arctic sea ice is facing a Blue Ocean Event with sea ice decline threatening to both dramatically lower albedo and reduce the ability for ocean heat to be consumed in the process of melting. Mountain glaciers are also in decline and permafrost is approaching the point where thawing of permafrost will speed up rapidly, as discussed in earlier posts such as this one.
- Land
The capacity for land to take up heat also faces a tipping point: The Land Evaporation Tipping Point can get crossed locally when water is no longer available locally for further evapotranspiration, i.e. from all processes by which water moves from the land surface to the atmosphere via evaporation and transpiration, including transpiration from vegetation, evaporation from the soil surface, from the capillary fringe of the groundwater table, and from water bodies on land. Once this tipping point gets crossed, the land and atmosphere will heat up strongly, due to the extra heat, i.e. heat that was previously consumed by evaporation and thawing, as described at this page.
- Atmosphere
As said, while the extra energy is increasing, as depicted by the above images, the capacity of oceans, land and ice to take up more energy is decreasing. Consequently, an increasingly large amount of extra heat threatens to accumulate in the lower atmosphere, especially in the Northern Hemisphere over land and in the Arctic, where temperatures are rising faster than anywhere in the world.
Compounding dangers in Arctic
Peatlands store approximately 30% of the global total soil carbon, with 80% of this carbon contained in Arctic peatlands. An emerging concern caused by accelerated climate change and permafrost thaw is the rapid increase in Arctic peatland fires, which have already expanded to the Siberian Arctic Ocean coast, Greenland, and Alaskan tundra peatlands. These fires occur along with record-breaking boreal forest fires raging in Canada. Peat fires may smolder for weeks and months, releasing massive amounts of, potentially ancient, carbon, which may transform them from a major carbon sink into a net carbon source into the atmosphere.
In addition to globally significant greenhouse gas emissions, peatland fires release abundant particulate matter. Smoldering peat fires may emit six times more aerosol mass per unit carbon combusted compared to flaming (grassland and forest) fires. Wildfires are a major source of Black Carbon (BC), which is the strongest light-absorbing particulate with a large positive global radiative effect. Simultaneously, wildfires release abundant Organic Carbon (OC), which can have a cooling effect either directly by scattering solar radiation or indirectly by modulating cloud properties. However, increasing evidence of substantial light-absorbing OC, i.e., Brown Carbon (BrC), being emitted in wildfires, suggests that the atmospheric net effect of biomass burning plumes is warming, as specifically shown for boreal and Indonesian peat combustion, while the properties and atmospheric lifetime of BrC vary depending on, for instance, combustion characteristics, biomass type, and moisture content. Moreover, BC and BrC decrease surface albedo when deposited on snow and ice, further accelerating Arctic climate change. Consequently, increasing high-latitude peatland fires are of great concern in the vicinity of snow- and ice-covered surfaces.
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
• Keeling Curve - by Scripps Institution of Oceanography at UC San Diego
https://keelingcurve.ucsd.edu
• NOAA - Global Monitoring Laboratory - Carbon Cycle Greenhouse Gases - Mauna Loa, Hawaii
https://gml.noaa.gov/ccgg/trends/mlo.html
• IPCC AR6, Workgroup 1, Chapter 7, Supplementary material - SF6 GWP and lifetime
• Arctic and Boreal Wildfires Impact Climate by Releasing Ancient Carbon and Light-Absorbing Particles - by Meri Ruppel et al. (2026)
https://www.facebook.com/groups/arcticnews/posts/10164246757324679
• 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





















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