Showing posts with label Paul Beckwith. Show all posts
Showing posts with label Paul Beckwith. Show all posts

Sunday, October 30, 2022

Transforming Society


How can the problems of war, climate collapse and famine best be addressed? 

Earlier this year, the U.N. issued a warning about famine, pointing out that war is compounding the problems of climate disruption and famine, adding that the "main costs to farmers are fertilizers and energy". The U.N. statement follows many news media reports about the rising cost of living.  

How can these problems best be addressed? For more than two decades, two sets of feebates have been recommended to help achieve agriculture reform and a rapid transition to clean, renewable energy, as depicted in the images in this post and as discussed in many earlier posts and the text below.


Agricultural Reform

Agriculture uses half of habitable land. Agriculture uses 70% to 90% of the freshwater supply. Most farmland is used to produce meat and diary. A 2019 Greenpeace analysis found over 71% of EU farmland to be dedicated to meat and dairy. Much agricultural land is used unsustainably in many ways; there is growing dependence on chemical fertilizers and weedkillers & herbicides, fungicides, insecticides, rodenticides and other pesticides; there is also a growing dependency on fossil fuel in many agricultural and food-related activities; and there is a growing demand for water. This causes huge emissions of greenhouse gases, pollution with toxic compounds, depletion of groundwater, salinification and erosion of soil and loss of soil nutrients and soil carbon content, and loss of diversity of many of the plants, the wildlife and the microorganisms that helped the world population grow to 8 billion people


Changing from food that is rich in meat and dairy to vegan-organic food can free up large areas of land that can instead be used for other purposes such as community gardens and food forests. It can bring down the cost of food and it can, in combination with biochar, restore the soil's carbon, moisture and nutrients content.

Instead of adding chemical nitrogen fertilizers - typically produced with natural gas - in annually-planted monocultures, it's better to have a diversity of vegetation including a variety of perennial plants such as legumes and trees. Furthermore, pyrolyzing biowaste should be encouraged, as this reduces fire hazards and produces biochar that can be added to soil to sequester carbon and to increase nutrients and moisture in the soil. According to Schmidt et al., 400,000 pyrolysis plants need to be built to process 3.8 billion tons of biowaste annually.

Local councils could encourage this by adding extra fees to rates for land where soil carbon falls, while using the revenue for rebates on rates for land where soil carbon rises.

That way, adding biochar effectively becomes a tool to lower rates, while it will also help improve the soil's fertility, its ability to retain water and to support more vegetation. That way, real assets are built, as illustrated by the image on the right, from the 2014 post Biochar Builds Real Assets.

Two sets of feebates can strongly reduce the greenhouse gases in the atmosphere, specifically carbon dioxide (C₂O), methane (CH₄) and nitrous oxide (N₂O).

[ from earlier post ]
The contribution of agriculture to emissions of carbon dioxide and especially methane is huge. The image on the right illustrates the difference between using a Gobal Warming Potential (GWP) for methane of 171 over a few years versus 28 over 100 years.

Nitrous oxide is also important, as a potent greenhouse gas and also as an ozone depleting substance (ODS). The impact of nitrous oxide as an ODS has grown relative to the impact of CFCs, as the abundance of nitrous oxide has kept rising in the atmosphere.

The IPCC in AR6 gives nitrous oxide a lifetime of 109 years and a GWP of 273. A 2017 study warns about increased nitrous oxide emissions from Arctic peatlands after permafrost thaw.

Furthermore, a recent study finds that nitrous oxide emissions contribute strongly to cirrus clouds, especially when ammonia, nitric acid and sulfuric acid are present together. Cirrus clouds exerts a net positive radiative forcing of about 5 W m⁻², according to IPCC AR6.

Much of current nitrous oxide emissions is caused by nitrogen fertilizers. Legumes include beans, peas, peanuts, lentils, lupins, mesquite, carob, tamarind, alfalfa, and clover. Legumes can naturally fix nitrogen to the soil, thus reducing the need for nitrogen fertilizer and in turn reducing the associated emissions, including emissions of methane and nitrous oxide.

Adding nitrogen fertilizer can also cause the formation of dead zones in lakes and oceans. Dead zones occur when the water gets too many nutrients, such as phosphorus and nitrogen from fertilizers, resulting in oxygen depletion at the top layer of oceans, which can also increase nitrous oxide releases.

In the video on the right, Jim McHenry discusses ways to improve the situation. 

All too often, chemical nitrogen fertilizers are added unnecessarily. The intent may be to help the plants grow, e.g. when leaves of plants turn yellow or when there is little growth. But it may actually be that the plants get too little water because the roots of the plants were damaged or too short, or that there was too little shade and too much sun. Excessive nitrogen fertilization and irrigation can then result in a lot of green leaves, but this growth can come at the expense of good food.

Instead, with a good mix of vegetation, there's little or no need to add chemical nitrogen fertilizer, since nitrogen-fixing plants such as legumes can help fast-growing plants get the necessary nitrogen, while the fast-growing plants provide shade for the legumes and the soil. Next to providing shade, the tall, sturdy stalks of plants such as corn can give the vines of beans something to attach themselves to. Fast-growing pants can provide a lot of shade to other plants and to the soil, thus keeping the soil moist, while also preventing the infiltration and growth of weeds and while also deterring pests with their spiny leaves.

Trees can lower surface temperatures by providing shade and by holding colder air under their canopy, thus avoiding extreme temperatures that could also cause the soil to get too dry. The roots of trees prevent erosion and guide rainwater to reach greater depth, thus avoiding that the soil gets too wet in case of heavy rain. Trees then pump water up from deep in the ground with their roots and much of the water comes out again through leaves (evapotranspiration), which stimulates rainfall. Furthermore, trees release pheromones (that attract pollinators) and other aerosols such as terpenes. Trees are typically narrower at the top and wider below, and through their shape and by standing up high they can guide the wind upward, while water vapor released from leaves also helps lift these aerosols into the air.  Raindrops forming around these aerosols will further stimulate the formation of lower cloud decks that provide shade, that reflect sunlight back into space and that produce more rainfall locally.

Furthermore, olivine sand can be used to create borders for gardens, footpaths and bicycle paths. Where needed, olivine sand could also be added on top of biochar, as the light color of olivine sand reflects more sunlight, while olivine can also soak up excess water and sequester carbon, while adding nutrients to the soil. By redesigning urban areas, more space can be used for trees, which also reduces the urban heat island effect and thus lowers temperatures.

In the video below, Paul Beckwith discusses global food shortages.


Also important is the transition to a vegan-organic diet. This can dramatically reduce the need for land and water, while additionally reducing greenhouse gas emissions. A good mix and variety of vegetation can help each of the plants through symbiotic interaction grow an abundance of vegan-organic food locally in a sustainable way.

Pyrolysis of biowaste is recommended as this can turn most carbon into biochar, resulting in high carbon sequestration rates, and increased capacity of the soil to retain carbon, nutrients and moisture, thus reducing erosion, fire hazards and greenhouse gas emissions, while increasing vegetation growth resulting in additional drawdown of carbon from the atmosphere. 

Most of the biowaste can be pyrolyzed and returned to the soil in the form of biochar. Some of the biowaste can also be used to construct buildings. Instead of cutting down the largest and most healthy trees to do so, which now all too often happens, it makes more sense to instead remove only dead trees and biowaste from the forest floor. Such use of biowaste could provide funding for the process of waste removal from the forest floor. For most biowaste (including kitchen and garden waste, and sewage), it makes sense to turn it into biochar that is added to the soil.

"The carbon content of biochar varies with feedstock and production conditions from as low as 7% (gasification of biosolids) to 79% (pyrolysis of wood at above 600 °C). Of this initial carbon, 63-82% will remain unmineralized in soil after 100 years at the global mean annual cropland-temperature of 14.9 °C", a 2021 study concludes. 

[ from earlier post ]
The above image shows how policies described in the Climate Plan can reduce the cost of energy and the cost of food, and facilitate the necessary transformation of society. The image shows examples of feebates that can help transform society in sectors such as agriculture, forestry, oceans, waste management and construction (center panel). The image also shows examples of local feebates to facilitate the transition to clean, renewable energy (top panel), as further discussed below.

Reducing the Cost of Energy and the Cost of Conflict

[ from earlier post, click on image to enlarge ]
As said, the cost of energy can best be reduced by a rapid transition to clean, renewable energy.

Much land is currently used for mining and drilling, refining and transport of fossil fuel (including roads, railways, ports and military protection to secure supply lines). 

Much land is also used to grow crops and trees that are burned for energy, such as wood used for heating, wood fed into power plants and crops grown for biofuel to power vehicles.

Mining, drilling and power plants are also large users of water. They need a lot of water, mainly for cooling, and they can pollute the water they use. 

Instead, by using electricity that is generated by wind turbines and solar panels, the total amount of water and the total area of land that is needed to produce energy can be reduced dramatically. 

Currently, much fossil fuel is transported by ship. International shipping emissions are not included in national totals of greenhouse gas emissions, despite the huge part of international shipping in global trade, carrying 70% of that trade by value and more than 80% by volume. Near the coast, batteries are increasingly powering shipping, but in international waters, shipping is almost entirely powered by fossil fuel, mainly bunker oil. Some 43% of maritime transport is busy merely moving fuel across the globe, so terminating fuel usage on land could in itself almost halve international shipping emissions.

In addition to commercial emissions caused by shipping of fuel, there are also military emissions that are excluded in national totals, such as international use by the military of bunker fuels and jet fuel, greenhouse gas emissions from energy consumption of bases abroad and the manufacture of equipment used by the military abroad. A large part of the military is busy securing and protecting global supply lines for fossil fuel, while burning huge amounts of fuel in the process. A 2019 analysis found that the US military's global supply chain and heavy reliance on carbon-based fuels make it the largest institutional consumer of oil and one of the largest greenhouse gas emitters, more than many countries worldwide.


Disputes over possession of fossil fuel are behind many international conflicts. Instead, nations can each cater for their power needs more independently and securely by transitioning to clean, renewable energy. A large part of a nation's infrastructure is used to transport fuel domestically, including trucks driving on roads and highways, while also using tunnels and bridges, parking places and stations for refuelling, while additionally fuel is transported by trains, planes and vessels that need ports, railways stations and tracks, and a lot of fossil fuel is burned in the process of transporting the fuel and constructing and maintaining these facilities.

Furthermore, part of the wood from forests and crops from farmland is used to supply biofuel, for use either to power vehicles, for heating or as fuel for power plants. Reducing the use of fuel will therefore also reduce nations getting into conflict with other nations, not only conflict over the possession of fossil fuel and over water to cool power plants, but also conflict over land and water that is used for agriculture and forestry to grow biofuel.

The easiest way to reduce the cost of conflict is to take away the reason for conflict, which in this case is the use of land to produce fuel.

In the video below, Robert Llewellyn interviews Mark Jacobson about The Climate Crisis.


Clean, renewable energy in the form of electricity generated by solar panels and wind turbines is already more economic than burning fuel for energy. Shifting to clean energy will thus lower the cost of energy, while people will also be less burdened by the cost of associated conflicts, which is more than the cost of the military and police taking care to avoid conflict, as the cost is even larger than that if conflicts do escalate and cause destruction of infrastructure, damage to soil and ecosystems and loss of lives, health and livelihood for all involved.

The comprehensive and effective action proposed by the Climate Plan can terminate the use of fuel and thus also reduce conflict, while additionally reducing the threat of runaway warming, and while additionally providing many environmental benefits and further benefits such as the termination of perceived needs for military forces to police global fuel supply lines and associated infrastructure.

In conclusion, reducing the use of fuel will in itself further reduce demand for fuel and the cost of energy. Replacing fuel by clean, renewable energy can additionally cut the need for energy through greater efficiencies of electric motors, appliances and devices. As said, this will also reduce the need for land and water, and - this cannot be said enough - avoid or delay climate collapse and catastrophe.

Air Taxis and Urban Redesign can further facilitate the necessary transformation



Electric vertical take-off and landing (eVTOL) air taxis can be an important component of the transformation of the way we travel, live, work and eat.

Using eVTOL air taxis can reduce the need for roads and associated infrastructure, further freeing up land, while the transition to electricity generated with solar panels and wind turbines can additionally free up land that is now used by utilities and their associated infrastructure such as power plants, power poles and towers, communication poles, etc. This land can instead be used for community gardens, (food) forests, parks, etc.

This doesn't have to be an instant shift. In existing cities, there already is a strong and growing movement to restrict the use of cars in city centers, and to instead add more walkways and bikeways. In this case, the roads will still be there, it's just their usage that changes. Another example is pipes. Many cities want to disconnect pipes that now supply natural gas to buildings, as it makes more sense to use electricity instead. The pipes will still be there, they just won't be used anymore, if at all. Digging up the pipes may make sense, but this may take some effort and time and it's therefore important that this issue is not used as an excuse to delay the rapid transition to the use of clean energy that is so urgently needed.

It's important to look at longer-term and more radical redesign. The transition toward greater use of air taxis enables space previously used for roads to instead be used for more walkways and bikeways, as well as for trees, community gardens, etc. This should be incorporated as part of wider and longer-term planning and redesign of urban areas.

In some places, this can lead to a more compact urban design, especially in city centers. After all, a lot of space becomes available as the use of roads for vehicle movements and for parking is reduced in an urban area, and this allows for more compact construction of new buildings and renovation of existing buildings that also reduces the distance between buildings, thus shortening the time it takes for trips by foot or bike in the city center, while there also will be plenty of opportunities for spaces to be created for air taxis to land and take off, e.g. in parks and on top of buildings.

At the same time, air taxis enable trips of up to a few hundred miles to be completed fast, while using little energy and causing little emissions. Furthermore, more remote places can be economically reached by air taxis without a need for roads to lead them to these places or for railway stations to be located nearby. Drone delivery of goods and air taxis can enable more people to live outside urban areas. More people will be able to have goods delivered to their home and to reach urban amenities if and when they want to, and more economically compared to using cars and roads.

The need for land and water to produce food and energy, and the need for land to transport goods and food can be reduced with the transitions to clean energy and to vegan-organic food. These transitions can also reduce the need for infrastructure such as pipes and poles for water supply, sewage, communications and power. Instead, we can have solar panels, microgrids, WiFi, rainwater tanks, biochar units, food forests and community gardens.

The image below illustrates how policies recommended in the Climate Plan can further reduce the need for infrastructure by supporting eVTOL air taxis, while transforming the space thus gained into community gardens, walkways, bikeways, etc.

[ from an earlier post ]

In conclusion, the situation can best be addressed through action as described in the Climate Plan, where needed in combination with a Climate Emergency Declaration.


Links

• Climate Plan (page)
https://arctic-news.blogspot.com/p/climateplan.html

• Climate Plan (post)
https://arctic-news.blogspot.com/2019/06/climate-plan.html

• Climate Plan (group)
https://www.facebook.com/groups/ClimatePlan

• Air Taxis (group)
https://www.facebook.com/groups/AirTaxis

• Biochar (group)
https://www.facebook.com/groups/biochar

• Vegan Organic Food (group)
https://www.facebook.com/groups/VeganOrganicFood

• Secretary-General Warns of Unprecedented Global Hunger Crisis, with 276 Million Facing Food Insecurity, Calling for Export Recovery, Debt Relief (June 24, 2022)
https://press.un.org/en/2022/sgsm21350.doc.htm

• Confirm Methane's Importance
https://arctic-news.blogspot.com/2021/03/confirm-methanes-importance.html

• Land Use - by Hannah Ritchie and Max Roser
https://ourworldindata.org/land-use

• FAO - Water for Sustainable Food and Agriculture

• Global agricultural green and blue water consumption under future climate and land use changes - by Zhongwei Huang et al. 
https://www.sciencedirect.com/science/article/abs/pii/S002216941930383X

• UN - population

• 400,000 Pyrolysis Plants to Save the Climate - by Hans-Peter Schmidt and Nikolas Hagemann (2021) 

• Greenhouse Gas Inventory Model for Biochar Additions to Soil - by Dominic Woolf et al. 
https://pubs.acs.org/doi/full/10.1021/acs.est.1c02425

• Nitrogen fertiliser use could ‘threaten global climate goals’
https://www.carbonbrief.org/nitrogen-fertiliser-use-could-threaten-global-climate-goals

• IPCC AR6 WG1 Chapter 7
https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_Chapter_07.pdf

• Synergistic HNO3 H2SO4 NH3 upper tropospheric particle formation - by Mingyi Wang et al. (2022) 
https://www.nature.com/articles/s41586-022-04605-4

• IPCC AR6 WG1 Chapter 4
https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_Chapter_04.pdf

• Low oxygen eddies in the eastern tropical North Atlantic: Implications for N2O cycling - by D. Grundle et al. (2017) 
https://www.nature.com/articles/s41598-017-04745-y

• Increased nitrous oxide emissions from Arctic peatlands after permafrost thaw - by Carolina Voigt et al. (2017) 
https://www.pnas.org/doi/10.1073/pnas.1702902114

• Low-cost solutions to global warming, air pollution, and energy insecurity for 145 countries - by Mark Jacobson et al.
• Numerous Benefits of 100% Clean, Renewable Energy

• How Much Water Do Power Plants Use? 
https://blog.ucsusa.org/john-rogers/how-much-water-do-power-plants-use-316

• Why does the Carmichael coal mine need to use so much water?

• View your government’s military emissions data
https://militaryemissions.org

• Military emissions
https://militaryemissions.org/wp-content/uploads/2022/06/military-emissions_final.pdf

• Emissions from fuels used for international aviation and maritime transport

• Decarbonizing the maritime sector: Mobilizing coordinated action in the industry using an ecosystems approach

• Assessing possible impacts on States of future shipping decarbonization

• News release: No environmental justice, no positive peace — and vice versa
https://www.hiroshima-u.ac.jp/en/news/73129

• Study: A global analysis of interactions between peace and environmental sustainability - by Dahylia Simangan et al.
https://www.sciencedirect.com/science/article/pii/S2589811622000210

• Also discussed at:

• Costs of War - Neta Crawford



Wednesday, April 27, 2022

Carbon dioxide crosses 422 ppm

Carbon dioxide (CO₂) reached an average daily concentration of 422.06 ppm on April 26, 2022, at Mauna Loa, Hawaii.


Furthermore, very high methane (CH₄) concentrations were recorded recently at Mauna Loa, Hawaii, with surface flask readings appearing to be as high as 1955 ppb.  


Clouds tipping point

A methane concentration of 1955 ppb corresponds, at a Global Warming Potential (GWP) of 200, with a carbon dioxide equivalent (CO₂e) of 391 ppm. Together with the above daily average CO₂ concentration of 422.06 ppm this adds up to a joint CO₂e of 813.06 ppm, i.e. less than 387 ppm away from the clouds tipping point (at 1200 ppm CO₂e) that on its own could raise the global temperature by 8°C.

Such a 387 ppm CO₂e could be added almost immediately by a burst of seafloor methane less than the size of the methane that is currently in the atmosphere (about 5 Gt). There is plenty of potential for such an abrupt release, given the rising ocean heat and the vast amounts of methane present in vulnerable sediments at the seafloor of the Arctic Ocean, as discussed in posts such as this one.


The 1200 ppm CO₂e clouds tipping point could also be crossed even without such an abrupt seafloor methane release. Carbon dioxide and methane levels are rising rapidly. The above image shows carbon dioxide concentration with a trend added, based on NOAA 1980-2021 mean global annual carbon dioxide data, illustrating how carbon dioxide concentration could cross 750 ppm by the end of the year 2029.

[ see also the importance of methane ]

The above image shows methane concentration with a trend added, based on NOAA 2008-2021 mean global annual methane data, illustrating how methane concentration could cross 4100 ppb by the end of the year 2029 and how methane's impact could cross 820 ppm CO₂e by the end of the year 2029.

As illustrated by the image below, 750 ppm carbon dioxide and 820 ppm CO₂e methane would together yield a joint CO₂e of 1570 ppm and thus would have already raised the global temperature by 8°C due to the clouds feedback much earlier than 2029, while the temperature rise would also have been driven up by the higher carbon dioxide and the methane concentrations. 


Furthermore, nitrous oxide is also rising and there are many further forcers, as discussed at the Extinction page. Altogether, there is the potential for a temperature rise of well over 18°C by 2026, as discussed in an earlier post.

Such high carbon dioxide concentrations could occur due to forest fires causing soils to burn (especially peat soils), which can also add vast amounts of methane to the atmosphere. 

The IPCC does contemplate high carbon dioxide scenarios (see image right), but as discussed in an earlier post, does not mention the clouds tipping point.

High carbon dioxide scenarios typically stop at the year 2100 and rarely do concentrations reach higher than 1200 ppm.

In the image on the right, from a 2020 analysis by Malte Meinshausen et al., the SSP5-8.5 scenario is extended to the year 2300 and a carbon dioxide concentration of well over 2100 ppm is reached around 2240.

In conclusion, there is plenty of scientific consideration of the potential for high concentrations of carbon dioxide and methane to eventuate, but it is typically ignored or waved away as too distant in the future to worry about. 

In other words, what's lacking is analysis of abrupt catastrophic climate change.

Climate change danger assessment

The image below expands risk assessment beyond its typical definition as the product of the severity of impact and probability, by adding a third dimension: timescale.


Water in soil and atmosphere

The image on the right, from a news release associated with a recent study, shows changes in atmospheric thirst, measured in terms of reference evapotranspiration from 1980-202 (in mm).

As temperatures rise due to people's emissions, more evaporation will take place over both land oceans, but not all water will return as precipitation, so more water vapor will stay in the air.

[ click on images to enlarge ]
The water-holding capacity of the atmosphere increases by about 7% for every 1°C (1.8°F) rise in temperature, in line with the Clausius–Clapeyron relation

In many cases, this means drier soils and vegetation, making vegetation more vulnerable to pests and diseases, and more prone to fire hazards. 

Water in the soil acts as a buffer, slowing down the temperature rise, so drier soil will heat up faster and further, causing land surface temperatures to rise even more and amplifying the impact of Urban heat island and Heat dome phenomena.

The image on the right, adapted from ESA, shows land surface temperatures as high as 65°C (149°F) in India on April 26, 2022. Note that land surface temperatures can be substantially higher than air temperatures. 

As temperatures rise, extreme weather events increase in frequency and intensity. The duration of extreme weather events can also increase, due to blocked weather patterns resulting from changes to the Jet Stream.

This contributes to shortages in food and water supplies. As long as glaciers are melting in the mountains, rivers will keep supplying some water, but the snow and ice cover is disappearing rapidly around the globe. 

The image on the right shows that food prices have risen strongly over the past few years and extreme weather events resulting from the global temperature rise have strongly contributed to the price rise. 

Further contributing to this rise is the rising demand for fertilizers that are currently all too often produced with fossil fuel, as political will to produce food in better ways remains lacking. 

Heat stress

Another issue is humidity. The more water vapor there is in the air, the harder temperature peaks are to bear.

The human body can cool itself by sweating, which has a physiological limit that is often described as a 35°C wet-bulb temperature

A 2020 study (by Raymond et al.) warned that this limit could be regularly exceeded with a temperature rise of less than 2.5°C (compared to pre-industrial).

Meanwhile, recent research found that in practice the limit will typically be lower and depending on circumstances could be as low as a wet-bulb temperature of 25°C.

In the video below, Paul Beckwith discusses the danger of combined high heat and humidity. 


In the video below, Guy McPherson also discusses the danger of combined high heat and humidity. 


Extinction

A 2018 study (by Strona & Bradshaw) indicates that most life on Earth will disappear with a 5°C rise. Humans, who depend for their survival on many other species, will likely go extinct with a 3°C rise, as illustrated by the image below, from an earlier post.


Conclusion

This further highlights the imminence of the danger and adds further urgency to the call for immediate, comprehensive and effective action, as described in the Climate Plan.


Links

• NOAA - Global Monitoring Laboratory, Recent Daily Average CO₂ at Mauna Loa, Hawaii, U.S. 
• NOAA - Global Monitoring Laboratory, Methane (surface flasks) at Mauna Loa, Hawaii, U.S. 
• The Importance of Methane
https://arctic-news.blogspot.com/p/the-importance-of-methane-in-climate.html

• Clouds feedback and tipping point
https://arctic-news.blogspot.com/p/clouds-feedback.html

• NOAA - Globally averaged marine surface annual mean carbon dioxide data
https://gml.noaa.gov/webdata/ccgg/trends/co2/co2_annmean_gl.txt

• NOAA - Globally averaged marine surface annual mean methane data
https://gml.noaa.gov/webdata/ccgg/trends/ch4/ch4_annmean_gl.txt

• NOAA - Mauna Loa CO2 weekly mean and historical comparisons
https://gml.noaa.gov/webdata/ccgg/trends/co2/co2_weekly_mlo.txt

• Methane rise is accelerating

• Runaway temperature rise by 2026?
• Extinction
https://arctic-news.blogspot.com/p/extinction.html

• Shortcomings of IPCC AR6 WGIII - Mitigation of Climate Change
https://arctic-news.blogspot.com/2022/04/shortcomings-of-ipcc-ar6-wgiii-mitigation-of-climate-change.html

• NOAA Mauna Loa CO₂ annual mean data
https://gml.noaa.gov/ccgg/trends/data.html

• NOAA globaly averaged marine surface annual mean methane data
https://gml.noaa.gov/ccgg/trends_ch4

• Is the IPCC creating false perceptions, again?
https://arctic-news.blogspot.com/2021/08/is-the-ipcc-creating-false-perceptions-again.html

• The shared socio-economic pathway (SSP) greenhouse gas concentrations and their extensions to 2500 - by Malte Meinshausen et al. 
https://gmd.copernicus.org/articles/13/3571/2020

• Clausius–Clapeyron relation

• Heat dome
https://en.wikipedia.org/wiki/Heat_dome

• ESA - Heatwave across India
https://www.esa.int/ESA_Multimedia/Images/2022/04/Heatwave_across_India

• Evaporative Demand Increase Across Lower 48 Means Less Water Supplies, Drier Vegetation, and Higher Fire Risk
https://www.drought.gov/news/evaporative-demand-increase-across-lower-48-means-less-water-supplies

• A Multidataset Assessment of Climatic Drivers and Uncertainties of Recent Trends in Evaporative Demand across the Continental United States - by Christine Albano et al.
https://journals.ametsoc.org/view/journals/hydr/23/4/JHM-D-21-0163.1.xml

• It could be unbearably hot in many places within a few years time
https://arctic-news.blogspot.com/2016/07/it-could-be-unbearably-hot-in-many-places-within-a-few-years-time.html

• The emergence of heat and humidity too severe for human tolerance - by Colin Raymond et al.
https://www.science.org/doi/10.1126/sciadv.aaw1838

• Evaluating the 35°C wet-bulb temperature adaptability threshold for young, healthy subjects (PSU HEAT Project) - by Daniel Vecellio et al.
https://pennstate.pure.elsevier.com/en/publications/evaluating-the-35c-wet-bulb-temperature-adaptability-threshold-fo

• Co-extinctions annihilate planetary life during extreme environmental change, by Giovanni Strona and Corey Bradshaw (2018)
https://www.nature.com/articles/s41598-018-35068-1

• Jet Stream
https://arctic-news.blogspot.com/p/jet-stream.html

• When Will We Die?
https://arctic-news.blogspot.com/2019/06/when-will-we-die.html

• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html






Friday, January 15, 2021

2020: Hottest Year On Record

NASA data show that 2020 was the hottest year on record.



The image below shows that high temperature in 2020 hit Siberia and the Arctic Ocean.

In above images, the temperature anomaly is compared to 1951-1980, NASA's default baseline. When using an earlier baseline, the data need to be adjusted. The image below shows a trendline pointing at an 0.31°C adjustment for a 1900 baseline. 



Additional adjustment is needed when using a 1750 baseline, while it also makes sense to add further adjustment for higher polar anomalies and for air temperatures over oceans, rather than sea surface water temperatures. In total, a 0.78°C adjustment seems appropriate, as has been applied before, such as in this analysis. For the year 2020, this translates in a temperature rise of 1.8029°C versus the year 1750.

Three trends: blue, purple and red

Will the global temperature rise to 3°C above 1750 by 2026? The blue trend below is based on 1880-2020 NASA Land+Ocean data and adjusted by 0.78°C to reflect a 1750 baseline, ocean air temperatures and higher polar anomalies, and it crosses a 3°C rise in 2026.



The trend shows a temperature for 2020 that is slightly higher than indicated by the data. This is in line with the fact that we're currently in a La Niña period and that we're also at a low point in the sunspot cycle, as discussed in an earlier post. The blue trend also shows that the 1.5°C treshold was already crossed even before the Paris Agreement was accepted. 



The second (purple) trend is based on a shorter period, i.e. 2006-2020 NASA land+ocean (LOTI) data, again adjusted by 0.78°C to reflect a 1750 baseline, ocean air temperatures and higher polar anomalies. The trend approaches 10°C above 1750 by 2026. The trend is based on 15 years of data, making it span a 30-year period centered around end 2020 when extended into the future for a similar 15 year period. The trend approaches 10°C above 1750 in 2026.

The trend is displayed on the backdrop of an image from an earlier post, showing how a 10°C rise could eventuate by 2026 when adding up the impact of warming elements and their interaction.



The stacked bars are somewhat higher than the trend. Keep in mind that the stacked bars are for the month February, when anomalies can be significantly higher than the annual average.

Temperature rise for February 2016 versus 1900.
In the NASA image on the right, the February 2016 temperature was 1.70°C above 1900 (i.e. 1885-1914). In the stacked-bar analysis, the February 2016 rise from 1900 was conservately given a value of 1.62°C, which was extended into the future, while an additional 0.3°C was added for temperature rise from pre-industrial to 1900.

Later analyses such as this one also added a further 0.2°C to the temperature rise, to reflect ocean air temperatures (rather than water temperatures) and higher polar anomalies (note the grey areas on the image in the right).

Anyway, the image shows two types of analysis on top of each other, one analysis based on trend analysis and another analysis based on a model using high values for the various warming elements. The stacked-bar analysis actually doesn't reflect the worst-case scenario, an even faster rise is illustrated by the next trend, the red line.

The third (red) trend suggests that we may have crossed the 2°C treshold in the year 2020. The trend is based on a recent period (2009-2020) of the NASA land+ocean data, again adjusted by 0.78°C to reflect a 1750 baseline, ocean air temperatures and higher polar anomalies.




Where do we go from here? 

It's important to acknowledge the danger of acceleration of the temperature rise over the next few years. The threat is illustrated by the image below and shows up most prominently in the red trend. 


Of the three trends, the red trend is based on the shortest period, and it does indicate that we have aready crossed the 2°C treshold and we could be facing an even steeper temperature rise over the next few years.

We're in a La Niña period and we're also at a low point in the sunspot cycle. This suppresses the temperature somewhat, so the 2020 temperature should actually be adjusted upward to compensate for such variables. Importantly, while such variables do show up more when basing trends on shorter periods, the data have not be adjusted for this in this case, so the situation could actually be even worse. 

At a 3°C rise, humans will likely go extinct, while most life on Earth will disappear with a 5°C rise, and as the temperature keeps rising, oceans will evaporate and Earth will go the same way as Venus, a 2019 analysis warned. 

Dangerous acceleration of the temperature rise 

There are many potential causes behind the acceleration of the temperature rise, such as the fact that the strongest impact of carbon dioxide is felt ten years after emission, so we are yet to experience the full wrath of the carbon dioxide emitted over the past decade. However, this doesn't explain why 2020 turned out to be the hottest year on record, as opposed to - say - 2019, given that in 2020 carbon dioxide emissions were 7% lower than in 2019.

James Hansen confirms that the temperature rise is accelerating, and he points at aerosols as the cause. However, most cooling aerosols come from industries such as smelters and coal-fired power plants that have hardly reduced their operations in 2020, as illustrated by the image below, from the aerosols page


Above image shows that on December 17, 2020, at 10:00 UTC, sulfate aerosols (SO₄) were as high as 6.396 τ at the green circle. Wind on the image is measured at 850 hPa.

Could the land sink be decreasing? A recent study shows that the mean temperature of the warmest quarter (3-month period) passed the thermal maximum for photosynthesis during the past decade. At higher temperatures, respiration rates continue to rise in contrast to sharply declining rates of photosynthesis. Under business-as-usual emissions, this divergence elicits a near halving of the land sink strength by as early as 2040. While this is a frightening prospect, it still doesn't explain why 2020 turned out to be the hottest year on record. 

Oceans are taking up less heat, thus leaving more heat in the atmosphere. The danger is illustrated by the image below. 


The white band around -60° (South) indicates that the Southern Ocean has not yet caught up with global warming, featuring low-level clouds that reflect sunlight back into space. Over time, the low clouds will decrease, which will allow more sunlight to be absorbed by Earth and give the world additional warming. A recent study finds that, after this 'pattern effect' is accounted for, committed global warming at present-day forcing rises by 0.7°C. While this is very worrying, it still doesn't explain why 2020 turned out to be the hottest year on record. 

Ocean stratification contributes to further surface warming, concludes another recent study
"The stronger ocean warming within upper layers versus deep water has caused an increase of ocean stratification in the past half century. With increased stratification, heat from climate warming less effectively penetrates into the deep ocean, which contributes to further surface warming. It also reduces the capability of the ocean to store carbon, exacerbating global surface warming. Furthermore, climate warming prevents the vertical exchanges of nutrients and oxygen, thus impacting the food supply of whole marine ecosystems."
"By uptaking ~90% of anthropogenic heat and ~30% of the carbon emissions, the ocean buffers global warming. [The] ocean has already absorbed an immense amount of heat, and will continue to absorb excess energy in the Earth’s system until atmospheric carbon levels are significantly lowered. In other words, the excess heat already in the ocean, and heat likely to enter the ocean in the coming years, will continue to affect weather patterns, sea level, and ocean biota for some time, even under zero carbon emission conditions."
Many feedbacks are starting to kick in with greater ferocity, with tipping points threatening to get crossed or already crossed, such as the latent heat tipping point, i.e. loss of the ocean heat buffer, as Arctic sea ice keeps getting thinner. As the above map also shows, the temperature rise is hitting the Arctic Ocean particularly hard. At least ten tipping points are affecting the Arctic, including the latent heat tipping point and the methane hydrates tipping point, as illustrated by the image below.
 
[ from an earlier post ]

A combination of higher temperatures and the resulting feedbacks such as stronger ocean stratification, stronger wind, decline of Arctic snow and ice and a distorted Jet Stream is threatening to cause formation of a lid at the surface of the North Atlantic Ocean that enables more heat to move to the Arctic Ocean. This could cause huge amounts of methane to erupt from the seafloor, thus contributing to cause the 1,200 ppm CO₂e cloud tipping point to get crossed, resulting in an extra 8°C rise, as an earlier post and a recent post warned.

Dangerous acceleration of the temperature rise

The danger is that methane is erupting in the Arctic from the seafloor and that this increasingly contributes to methane reaching the stratosphere. 

While methane initially is very potent in heating up the atmosphere, it is generally broken down relatively quickly, but in the atmosphere over the Arctic, there is very little hydroxyl to break down the methane. 

Methane also persists much longer in the stratosphere, which contributes to its accumulation there. 


Large amounts of methane may already be erupting from the seafloor of the Arctic Ocean, rising rapidly and even reaching the stratosphere

This danger is getting little public attention. The NOAA image on the right shows the globally-averaged, monthly mean atmospheric methane abundance derived from measurements from marine surface sites. Measurements that are taken at sea level do not reflect methane very well that is rising up from the seafloor of the Arctic Ocean, especially where the methane rises up high in plumes. 

Satellite measurements better reflect the danger. The image on the right shows that the MetOp-1 satellite recorded peak methane levels as high as 2715 ppb at 469 mb on the morning of January 6, 2021. 

Most of the high (magenta-colored) levels of methane are located over oceans and a lot of them over the Arctic Ocean. 

The next image on the right shows the situation closer to sea level, at 586 mb, where even less of the high levels of methane show up over land, indicating that the methane originated from the seafloor. 

The third image on the righ shows the situation even closer to sea level, at 742 mb, and almost all high levels of methane show up over the Arctic Ocean and over areas where the Atlantic Ocean and the Pacific Ocean border on the Arctic. 

Because methane is lighter than air and much lighter than water, methane erupting from the seafloor will quickly rise up vertically. While much of the methane that is released from the seabed can get broken down in the water by microbes, methane that is rising rapidly and highly concentrated in the form of plumes will leave little opportunity for microbes to break it down in the water column, especially where waters are shallow,
as is the case in much of the Arctic Ocean.

As methane hydrates destabilize, methane will erupt with an explosive force, since methane is highly compressed inside the hydrate (1 m³ of methane hydrate can release 160 m³ of gas). Such eruptions can destabilize further hydrates located nearby. Because of this explosive force, plumes of methane can rise at high speed through the water column. 

Because methane is so much lighter than water, large methane releases from the seafloor will form larger bubbles that merge and stick together, developing more thrust as they rise through the water.

Because of this thrust, methane plumes will keep rising rapidly after entering the atmosphere, and the plumes will more easily push away aerosols and gases that slow down the rise in the air of methane elsewhere, such as where methane is emitted by cows. 

A further image of another satellite is added on the right. The N2O satellite recorded methane levels as high as 2817 ppb at 487 mb on the morning of January 10, 2021. 

Such sudden and very high peaks can hardly be caused by agriculture or wetlands, but instead they are likely caused by destabilization of methane hydrates in sediments at the seafloor. 

Further contributing to the danger is the fact that little hydroxyl is present in the atmosphere over the Arctic, so it is much harder for this methane to get broken down in the air over the Arctic, compared to methane emissions elsewhere. 

Finally, the edge of the stratosphere is much lower over the Arctic, as discussed in an earlier post.

All this makes that methane that is erupting from the seafloor of the Arctic Ocean is more prone to accumulate in the stratosphere. Once methane is in the stratosphere, it's unlikely that it will come back into the troposphere.

The IPCC AR5 (2013) gave methane a lifetime of 12.4 years. The IPCC TAR (2001) gave stratospheric methane a lifetime of 120 years, adding that less than 7% of methane did reach the stratosphere at the time. According to IPCC AR5, of the methane that gets broken down by hydroxyl in the atmosphere, some 8.5% got broken down in the stratosphere.

Conclusions

The situation is dire and calls for immediate, comprehensive and effective action as described in the Climate Plan.

In the video below, Paul Beckwith discusses the situation: 


For another perspective, Guy McPherson discusses the situation in the video below, Edge of Extinction: Maybe I’m Wrong





Links

• Climate Plan
https://arctic-news.blogspot.com/p/climateplan.html

• NASA Global Land-Ocean Temperature Index
https://data.giss.nasa.gov/gistemp

• What are El Niño and La Niña?
https://oceanservice.noaa.gov/facts/ninonina.html

• Multivariate El Niño/Southern Oscillation (ENSO) Index Version 2 (MEI.v2)
https://psl.noaa.gov/enso/mei 
 
• Temperatures keep rising
https://arctic-news.blogspot.com/2020/12/temperatures-keep-rising.html

• There is no time to lose
https://arctic-news.blogspot.com/2020/11/there-is-no-time-to-lose.html

• Possible climate transitions from breakup of stratocumulus decks under greenhouse warming, by Tapio Schneider et al. (2019)
https://www.nature.com/articles/s41561-019-0310-1

• A rise of 18°C or 32.4°F by 2026?

• Greater committed warming after accounting for the pattern effect - by Chen Zhou et al. 

• Upper Ocean Temperatures Hit Record High in 2020 - by Lijing Cheng et al. 
https://link.springer.com/article/10.1007/s00376-021-0447-x

• How close are we to the temperature tipping point of the terrestrial biosphere? - by Katharyn Duffy et al.
https://advances.sciencemag.org/content/7/3/eaay1052

• Methane hydrates tipping point threatens to get crossed

• Temperatures threaten to become unbearable

• Cold freshwater lid on North Atlantic

• Aerosols

• NOAA - Trends in Atmospheric Methane
https://www.esrl.noaa.gov/gmd/ccgg/trends_ch4

•  COVID-19 lockdown causes unprecedented drop in global CO2 emissions in 2020 - Gobal Carbon Project
https://www.globalcarbonproject.org/carbonbudget/20/files/International_FutureEarth_GCB2020.pdf

• Global Average Temperatures in 2020 Reached a RECORD HIGH of 1.55 C above PreIndustrial in 1750 - by Paul Beckwith 
https://www.youtube.com/watch?v=O0lgTAEUYyA

• Edge of Extinction: Maybe I’m Wrong - by Guy McPherson
https://guymcpherson.com/2021/01/edge-of-extinction-maybe-im-wrong

• Extinction
https://arctic-news.blogspot.com/p/extinction.html