An atmosphere that sucks up more water vapor increases the atmospheric vapor pressure deficit (VPD). A 2019 study warns that increased VPD reduces global vegetation growth: “VPD greatly limits land evapotranspiration in many biomes by altering the behavior of plant stomata. Increased VPD may trigger stomatal closure to avoid excess water loss due to the high evaporative demand of the air. In addition, reduced soil water supply coupled with high evaporative demand causes xylem conduits and the rhizosphere to cavitate (become air-filled), stopping the flow of water, desiccating plant tissues, and leading to plant death. Previous studies reported that increased VPD explained 82% of the warm season drought stress in the southwestern United States, which correlated to changes of forest productivity and mortality. In addition, enhanced VPD limits tree growth even before soil moisture begins to be limiting.”
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Similarly, about a quarter of the 4% heat consumed by the cryosphere goes into melting Arctic sea ice. Loss of Arctic sea ice also constitute a tipping point, since incoming heat will from that point on instead go into the Arctic.
So, will there be Arctic sea ice left in September 2023? Current conditions make that the outlook is grim.
Ominously, November 2023 temperature anomalies are forecast to be at the top end of the scale for a large part of the Arctic Ocean, as illustrated by the tropicaltidbits.com image below.
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The image on the right, adapted from NOAA, shows ocean heat moving toward the Arctic along the path of the Gulf Stream.
Vast amounts of ocean heat are moving toward the Arctic, especially in the North Atlantic, threatening to cause rapid and massive melting of Arctic sea ice and thawing of permafrost.
As discussed in a recent post, the world sea surface temperature (between 60°South and 60°North) has been at 21°C or higher for as many as 38 days. Such temperatures are unprecedented in the NOAA record that goes back to 1981.
Rising temperatures of the water in the Arctic Ocean threaten to trigger massive loss of sea ice.
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The satellite image on the right also shows many cracks in the sea ice just north of the northern tip of Greenland.
On top of that, there are developments that could make things even worse. Loss of Arctic sea kice comes with loss of the latent heat buffer and loss of albedo that threaten to trigger subsequent eruptions of methane from the seafloor of the Arctic Ocean, as has been described many times before, such as in this post, in this post and in this post.
An earlier post discussed the Terrestrial Biosphere Temperature Tipping Point, coined in a recent study finding that at higher temperatures, respiration rates continue to rise in contrast to sharply declining rates of photosynthesis, which under business-as-usual emissions would nearly halve the land sink strength by as early as 2040.
A 2021 study on oceans finds that, with increased stratification, heat from climate warming less effectively penetrates into the deep ocean, which contributes to further surface warming, while it also reduces the capability of the ocean to store carbon, exacerbating global surface warming. An earlier analysis warns about growth of a layer of fresh water at the surface of the North Atlantic resulting in more ocean heat reaching the Arctic Ocean and the atmosphere over the Arctic, while a 2023 study finds that growth of a layer of fresh water decreases its alkalinity and thus its ability to take up CO₂, a feedback referred to as the Ocean Surface Tipping Point.
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[ from Blue Ocean Event 2022? – click on images to enlarge ] |
The above image depicts only one sequence of events, or one scenario out of many. Things may eventuate in different orders and occur simultaneously, i.e. instead of one domino tipping over the next one sequentially, many events may occur simultaneously and reinforce each other. Further events and developments could be added to the list, such as ocean stratification and stronger storms that can push large amounts of warm salty water into the Arctic Ocean.
Loss of Arctic sea ice is often recognized as a tipping point that accelerates heating up of the Arctic through albedo loss and loss of the latent heat buffer. Loss of Permafrost in Siberia and North America is often regarded as a tipping point that could trigger huge emissions of greenhouse gases. Similarly, loss of Antarctic sea ice, loss of the snow and ice cover on Greenland, on Antarctica and on mountaintops such as the Tibetan Plateau could each also be seen as tipping points, since further melting could trigger destabilization of local hydrates resulting in eruption of vast amounts of methane.
– The Clouds Tipping Point (at 1200 ppm carbon dioxide equivalent)
– The Terrestrial Biosphere Temperature Tipping Point (discussed above)
– The Ocean Surface Tipping Point (discussed above)
Links
• Heat stored in the Earth system 1960–2020: where does the energy go? – by Karina von schuckmann et al.
Discussion at:
https://www.facebook.com/groups/arcticnews/posts/10160713282559679
https://wedocs.unep.org/bitstream/handle/20.500.11822/36619/FB025.pdf
• Increased atmospheric vapor pressure deficit reducesglobal vegetation growth – by Wenping Yuan et al.
https://www.science.org/doi/epdf/10.1126/sciadv.aax1396
Discussion at:
https://www.facebook.com/groups/arcticnews/posts/10157565091229679
• Extinction
https://arctic-news.blogspot.com/p/extinction.html
• Tropicaltidbits.com
https://www.tropicaltidbits.com
• NOAA SST
https://www.ospo.noaa.gov/Products/ocean/sst/contour/index.html
• Uni of Bremen – sea ice concentration and thickness
https://seaice.uni-bremen.de/start
• Climate Reanalyzer – Daily sea surface temperatures
https://climatereanalyzer.org/clim/sst_daily
• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html