The April 2024 temperature was 1.32°C higher than 1951-1980, as illustrated by the above image, created with NASA content. Local anomalies are as high as 6.2°C.
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The above image shows a magenta trend that points at the temperature crossing 3°C above pre-industrial later this year (2024). What could be behind such a steep rise?
Have Feedbacks taken over?
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The extremely high recent temperatures and the trends depicted in the images further above raise the question as to what the underlying driver is, given that we’re no longer in an El Niño. Indeed, the question is whether feedbacks have taken over as the main driver causing the temperature rise to further accelerate.
There is no single feedback that could cause the recent steep rise of temperatures and its acceleration, instead there are numerous non-linear, self-amplifying feedback loops that can all contribute, interact and start to kick in with greater ferocity, amplifying and further accelerating the rise.
Furthermore, developments such as rising emissions from industry, transport, land use, forest fires and waste fires, ocean acidification and reductions in sulfur emissions over the past few years all contribute to further acceleration of the temperature rise.
Two tipping points threaten to get crossed
Contributing to these high temperatures in the Arctic are high temperatures of the North Atlantic Ocean, which are now rising rapidly, in line with seasonal changes, as illustrated by the image below, created with Climate Reanalyzer content.
North Atlantic sea surface temperatures are now rising strongly, in line with seasonal changes. Ominously, a peak of 25.4°C was reached in August 2023. The question is how high the North Atlantic temperature will be in 2024 at that time of year.
The image below shows North Atlantic sea surface temperature anomalies versus 1982-2011. Data shown are from September 1, 1981, through May 31, 2024.
As discussed, one reason for the high temperatures of the North Atlantic is that sulfur emissions have been reduced over the years. Furthermore, there are many feedbacks. Importantly, there is potential for the slowing down of the Atlantic meridional overturning circulation (AMOC) to contribute to more heat accumulating at the surface of the North Atlantic Ocean, as also illustrated by the image below.
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[ Albedo change, from the Albedo page ] |
Next to the albedo loss, there is loss of the latent heat buffer constituted by the sea ice. Latent heat is energy associated with a phase change, in this case the energy consumed as solid ice turns into liquid water (i.e. melts). During a phase change, the temperature remains constant. Sea ice acts as a buffer that absorbs heat, while keeping the temperature at about zero degrees Celsius. As long as there is sea ice in the water, this sea ice will keep absorbing heat, so the temperature doesn’t rise at the sea surface.
As long as air temperatures over the Arctic are below freezing, sea ice can persist at the surface, maintaining sea ice extent, which may give the false impression that sea ice was healthy, whereas in fact sea ice has steadily been declining in thickness.
Arctic sea ice volume is at its lowest on record for the time of year, as illustrated by the image below, created with Danish Meteorological Institute content, and as also discussed in earlier posts such as this one.
The amount of energy absorbed by melting ice is as much as it takes to heat up an equivalent mass of water from zero to 80°C. Loss of sea ice thickness implies loss of the latent heat buffer and constitutes a tipping point, i.e. once crossed, the Arctic Ocean will heat up at accelerating pace.
Seafloor methane constitutes a second tipping point. When methane escapes from hydrates that get destabilized by rising temperatures, the methane will expand to 160 times its previous volume and enter the atmosphere with force. Without the buffer constituted by thicker sea ice, an influx of ocean heat could cause large-scale destabilization of hydrates contained in sediments at the seafloor of the Arctic Ocean, resulting in eruptions of huge amounts of methane.
Crossing of the latent heat tipping point and the seafloor methane tipping point results in ever more heat reaching and accumulating in the Arctic ocean, destabilizing methane hydrates contained in sediments at the seafloor of the Arctic Ocean, as discussed in many earlier posts such as this one.
Self-amplifying feedbacks and developments as discussed above, as well as crossing of these two tipping points, could all contribute to cause a temperature rise of over 10°C, in the process causing the clouds tipping point to get crossed that can push up the temperature rise by a further 8°C.
Altogether, the temperature rise may exceed 18°C from pre-industrial by as early as 2026, as illustrated by the image on the right, from the extinction page.
Climate Emergency Declaration
Links
• NASA – datasets and images
https://data.giss.nasa.gov
• Moistening Atmosphere
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