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Care for the Ozone Layer

January 20, 2019 water vapor

The stratosphere normally is cold and very dry. Global warming can increase water vapor in the stratosphere in a number of ways. Global warming causes the troposphere to warm and since warmer air holds more water vapor, the amount of water vapor in the troposphere is increasing. This can cause more water vapor to end up in the stratosphere as well, as described below.

Stratospheric Water Vapor over the Arctic

Around the time of the December Solstice, very little sunlight is reaching the Arctic and temperatures over land at higher latitudes can get very low. At the same time, global warming has made oceans warmer and this keeps air temperatures over water relatively warm in Winter. This can lead to a number of phenomena including sudden stratospheric warming and moistening of the stratosphere.

Sudden stratospheric warming is illustrated by the image on the right, showing temperatures in the stratosphere over Siberia as high as 12.7°C or 54.9°F on December 24, 2018, and temperatures as low as -84.8°C or -120.6°F over Greenland.

At the same time, relative humidity was as high as 100% in the stratosphere over the North Sea, as the second image on the right shows.

Moistening of the stratosphere was even more pronounced on December 24, 2016, as illustrated by the third image on the right.

Storms over the U.S.

Jennifer Francis has long pointed out that, as temperatures at the North Pole are rising faster than at the Equator, the Jet Stream is becoming wavier and can get stuck in a 'blocking pattern' for days, increasing the duration and intensity of extreme weather events.

This can result in stronger storms moving more water vapor inland over the U.S., and such storms can cause large amounts of water vapor to rise high up in the sky.

Water vapor reaching stratospheric altitudes causes loss of ozone, as James Anderson describes in a 2017 paper and discusses in the short 2016 video below.

Methane

Stratospheric water vapor can also result from methane oxidation in the stratosphere. Methane concentrations have risen strongly at higher altitudes over the years. Noctilucent clouds indicate that methane has led to water vapor in the upper atmosphere.

The danger is that, as the Arctic Ocean keeps warming, large eruptions of methane will occur from the seafloor. Ominously, high methane levels have recently shown up on satellite images over the Arctic at lower altitudes, indicating the methane is escaping from the sea.

The images below show methane levels recorded by the NPP satellite:
Jan. 6, 2019, with peak levels of 2513 ppb at 1000 mb, 2600 ppb at 840 mb and 2618 ppb at 695 mb;
Jan. 11, 2019, with peak levels of 2577 ppb at 1000 mb, 2744 ppb at 840 mb and 2912 ppb at 695 mb;
Jan. 15, 2019, with peak levels of 2524 ppb at 1000 mb, 2697 ppb at 840 mb and 2847 ppb at 695 mb.

The images below show methane levels recorded by the MetOp satellites:
Jan. 15, 2019, with peak levels of 2177 ppb at 840 mb, 2342 ppb at 695 mb and 2541 ppb at 586 mb;
Jan. 16, 2019, with peak levels of 2219 ppb at 840 mb, 2299 ppb at 695 mb and 2475 ppb at 586 mb;
Jan. 19, 2019, with peak levels of 2201 ppb at 840 mb, 2489 ppb at 695 mb and 2813 ppb at 586 mb.

The Importance of the Ozone Layer

Increases in stratospheric water vapor are bad news, as they speed up global warming and lead to loss of stratospheric ozone, as Drew Shindell pointed out back in 2001.

It has long been known that deterioration of the ozone shield increases ultraviolet-B irradiation, in turn causing skin cancer. Recent research suggest that, millions of years ago, it could also have led to loss of fertility and consequent extinction in plants and animals (see box right).

Existential Threats

In conclusion, rising levels of emissions by people constitute existential threats in many ways. Rising temperatures cause heat stress and infertility, and there are domino effects. Furthermore, stratospheric ozone loss causes cancer and infertility. Only once the ozone layer formed on Earth some 600 million years ago could multicellular life develop and survive. Further loss of stratospheric ozone could be the fastest path to extinction for humanity, making care for the ozone layer imperative.

As described in an earlier post, Earth is on the edge of runaway warming and a moist-greenhouse scenario means oceans are evaporating into the stratosphere with loss of the ozone layer.

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

Links

• Climate and ozone response to increased stratospheric water vapor, by Drew Shindell (2001)
https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/1999GL011197

• Stratospheric ozone over the United States in summer linked to observations of convection and temperature via chlorine and bromine catalysis, by James Anderson et al. (2017)
https://www.pnas.org/content/114/25/E4905

• Harvard Speaks on Climate Change: James Anderson (2016)
https://vimeo.com/185794598

• Climate Week: Climate Science Breakfast with James Anderson (April 9, 2015)
http://environment.harvard.edu/climate-week-climate-science-breakfast-james-anderson

• 10°C or 18°F warmer by 2021?
https://arctic-news.blogspot.com/2017/04/10c-or-18f-warmer-by-2021.html

• Noctilucent clouds indicate more methane in upper atmosphere
https://arctic-news.blogspot.com/2012/09/noctilucent-clouds-indicate-more-methane-in-upper-atmosphere.html

• Noctilucent clouds: further confirmation of large methane releases
https://methane-hydrates.blogspot.com/2013/12/noctilucent-clouds-further-confirmation-of-large-methane-releases.html

• 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

• Climate change: effect on sperm could hold key to species extinction, by Kris Sales
https://theconversation.com/climate-change-effect-on-sperm-could-hold-key-to-species-extinction-107375

• Climate change: effect on sperm could hold key to species extinction
https://theconversation.com/climate-change-effect-on-sperm-could-hold-key-to-species-extinction-107375

• UV-B–induced forest sterility: Implications of ozone shield failure in Earth’s largest extinction, by Jeffrey Benca et al. (2018)
http://advances.sciencemag.org/content/4/2/e1700618

• 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

• Earth is on the edge of runaway warming
https://arctic-news.blogspot.com/2013/04/earth-is-on-the-edge-of-runaway-warming.html

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

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Dangerous situation in Arctic

November 26, 2018 water

In the North Pacific, the flow of warmer water is clearly visible (see images right, green circle left).

In the North Atlantic, huge amounts of heat are moving into the Arctic Ocean (green circle right).

At some spots, heat that is traveling underneath the sea surface comes to the surface (green circle at the top).

Most warming caused by people's emissions goes into oceans, especially into the top layer of oceans.

Furthermore, warmer air and warmer sea surfaces can cause winds to grow dramatically stronger. As the Arctic is warming much faster than the rest of the world, the narrowing difference between the temperatures at the North Pole and the Equator is decreasing the speed at which winds circumnavigate Earth; at the same time, the amount of heat that is moving north can grow dramatically, both due to winds and sea currents, and cyclones can further accelerate this.

The danger is that an influx of warm salty water will reach the seafloor and trigger methane eruptions.

The situation is especially critical in many parts of the Arctic Ocean where the water is very shallow. Some 75% of the East Siberian Arctic Shelf (ESAS) is shallower than 50 m (see maps on the right).

[ warm water from the Atlantic Ocean is
increasingly invading the Arctic Ocean ]

The danger here is huge, for numerous reasons, incl.:

• shallow waters can warm up very rapidly in case of an influx of warm water;

• these shallow seas are now covered by ice, so the heat cannot escape to the atmosphere;

• sea ice is very thin, so the sea ice won't act as a buffer to absorb the heat;

• methane rising through shallow waters will pass through the water column and enter the atmosphere more quickly;

• in shallow waters, large abrupt releases will more quickly deplete the oxygen in the water, making it harder for microbes to break down the methane;

• hydroxyl levels over the Arctic are very low, which means that it takes much longer for methane over the Arctic to get broken down.

The four videos below provide a good introduction into the various issues and illustrate how dangerous the situation is in the Arctic.

Each video is part of a talk between Dave Borlace and Peter Wadhams.

Part 1 discusses albedo change in the Arctic and associated changes such as jet stream changes.

Part 2 discusses the threat of huge methane releases in the Arctic.

Part 3 discusses the thermohaline circulation and methods that could improve the situation such as carbon removal and Ocean Mechanical thermal Energy Conversion (OMTEC).

Part 4 discusses sea level rise and fires.

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As El Niño sets in, will global biodiversity collapse in 2019?

November 16, 2018 warming

Global biodiversity collapse

[ Will global biodiversity collapse in 2019? ]

A recent study created a dataset of plant temperature tolerances with a median upper tolerance limit of 23.7°C.

This temperature is about 10°C higher than the temperature in the year 1750.
Only during times of mass extinctions were temperatures that high, such as during the PETM, 55.5 million years ago, and the Permian–Triassic extinction event, 252 million years ago, also know as the Great Dying when some 95% of species known from fossils went extinct.

[ image from: How much warmer is it now? ]

The study concludes that extinction will already occur far earlier than when upper tolerance levels are reached, as "loss of one species can make more species disappear (a process known as ‘co-extinction’), and possibly bring entire systems to an unexpected, sudden regime shift, or even total collapse."

There was a small group of species with large tolerance limits and remarkable resistance to environmental change, but even they could not survive co-extinctions. In fact, their extinction was abrupt and happened far from their tolerance limits and close to global biodiversity collapse at around 5°C of heating.

[ El Niño sets in ]

In the top image on the right, monthly NASA Land+Ocean temperature data 2017-October 2018 are adjusted, and a polynomial trend is added, showing how a 5°C rise in temperature could occur very rapidly, i.e. by September 2019.

The second image on the right is from an earlier post that contains more background on the adjustment of NASA data and the need for a polynomial trend.

A strong abrupt rise in temperature could be caused by an influx of warm salty water into the Arctic Ocean, as this can trigger large eruptions of methane from its seafloor, as discussed in earlier posts such as this one and as further discussed below.

As El Niño sets in, the odds that such rapid warming will threaten to cause global biodiversity collapse are rising.

Earthquakes triggering methane releases

An additional danger is that large methane releases from the seafloor of the Arctic Ocean will be triggered by earthquakes.

The danger is that isostatic rebound will trigger earthquakes in the Arctic Ocean that this in turn will destabilize methane hydrates, as discussed in more detail at this page.

Seismic shocks can travel over long distances along fault lines and destabilize methane hydrates in other locations.

Above image shows that on November 9, 2018, an earthquake with a magnitude of 6.8 on the Richter scale occurred on the fault line between Greenland and Norway.

This area is not used to be hit by large earthquakes. No larger earthquake has occurred in this area for more than 100 years.

Subsequent earthquakes did occur nearby, on November 12, 13 and 15, respectively measuring M4.3, M4.6 and M5.2 on the Richter scale, which also are very large earthquakes to hit this area.

Ominously, high levels of methane showed up on November 21, 2018, over the Greenland Sea (top image on the right).

Earlier, high levels of methane had been recorded over the Arctic Ocean. Note that this fault line runs across the Arctic Ocean toward the Laptev Sea.

Methane levels as high as 2787 ppb were recorded on November 15, 2018 (second image on the right).

On November 17, 2018, methane levels as high as 2847 ppb were recorded (third image on the right).

On November 20, 2018, methane levels as high as 2827 ppb were recorded (fourth image on the right).

The images show large methane levels over the East Siberian Arctic Shelf, the submarine permafrost north of Eastern Siberia.

In a 2008 paper, Dr. Natalia Shakhova et al. concluded that release of up to 50 Gt of methane from hydrates storage could occur at any time, an amount many times the methane that is now present in the atmosphere.

Additional emissions

Such a temperature rise would trigger many forest fires, releasing huge amounts of additional emissions, including carbon dioxide, methane and black carbon.

The image on the right shows carbon dioxide levels in California as high as 809 ppm on November 10, 2018 (at the green circle).

The next image on the right illustrates the jump in carbon dioxide levels in Mauna Loa, Hawaii, following the the fires in California.

“Levels of heat-trapping greenhouse gases in the atmosphere have reached another new record high,” the World Meteorological Organization (WMO) said in a recent news release. “There is no sign of a reversal in this trend, which is driving long-term climate change, sea level rise, ocean acidification and more extreme weather.”

“The science is clear. Without rapid cuts in CO₂ and other greenhouse gases, climate change will have increasingly destructive and irreversible impacts on life on Earth. The window of opportunity for action is almost closed,” said WMO Secretary-General Petteri Taalas.

“The last time the Earth experienced a comparable concentration of CO₂ was 3-5 million years ago, when the temperature was 2-3°C warmer and sea level was 10-20 meters higher than now,” said Mr Taalas.

“CO₂ remains in the atmosphere for hundreds of years and in the oceans for even longer. There is currently no magic wand to remove all the excess CO₂ from the atmosphere,” said WMO Deputy Secretary-General Elena Manaenkova.

In the associated video, Dr Oksana Tarasova added that “changes in carbon dioxide levels that we are observing now do not happen naturally. Such changes never ever happened in the history of this Planet.”

As the image on the right shows, CH₄, CO₂ and N₂O levels in the atmosphere are, respectively, 257%, 146% and 122% their 1750 levels.

How fast could 5°C warming happen?

The U.S. Global Change Research Program has just released its Fourth National Climate Assessment. One of its key messages is that temperatures could rise by 5°C or more. The report adds that this could occur by the end of the century, but the report doesn't deny this could also occur much earlier. Indeed, one of its key findings is that some feedbacks and potential state shifts cannot be quantified; and some are probably still unknown.

What the report doesn't mention is that global biodiversity will have collapsed at 5°C of warming. Such a rise kills all plants on land and thus virtually all mammals (including humans), since they either directly or indirectly feed on plants.

A rapid 5°C rise could occur if an influx of warm salty water triggered methane eruptions from the seafloor of the Arctic Ocean. Combined with snow and ice loss, it could rapidly raise temperatures by 1.5°C, which increases water vapor. If cloud feedback is strongly positive, water vapor feedback can lead to 3.5 times as much warming, so these warming elements alone could cause 5°C warming within years. And then, of course, there are further warming elements.

The situation is dire and calls for comprehensive and effective action, as described at the Climate Plan, i.e. multiple lines of action implemented in parallel and locally where possible. Of course, as long as politicians remain reluctant to even consider pursuing efforts to reduce emissions, the world can be expected to remain in the Danger Zone for a long time to come.

Links

• 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

• Greenhouse gas levels in atmosphere reach new record, World Meteorological Organization (WMO)
https://public.wmo.int/en/media/press-release/greenhouse-gas-levels-atmosphere-reach-new-record

• WMO video - Press Conference: Greenhouse Gas Bulletin (Geneva, 22 November 2018)
http://webtv.un.org/watch/wmo-press-conference-greenhouse-gas-bulletin-geneva-22-november-2018/5970414543001/

• Fourth National Climate Assessment - U.S. Global Change Research Program
https://nca2018.globalchange.gov/

• Doomsday by 2021?
https://arctic-news.blogspot.com/2018/11/doomsday-by-2021.html

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

• Feedbacks
https://arctic-news.blogspot.com/p/feedbacks.html

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

• Seismic Events
https://arctic-news.blogspot.com/p/seismic-events.html

• Can we weather the Danger Zone?
https://arctic-news.blogspot.com/2018/07/can-we-weather-the-danger-zone.html

• How much warmer is it now?
https://arctic-news.blogspot.com/2018/04/how-much-warmer-is-it-now.html

• What Does Runaway Warming Look Like?
https://arctic-news.blogspot.com/2018/10/what-does-runaway-warming-look-like.html

• Peaks Matter
https://arctic-news.blogspot.com/2018/08/peaks-matter.html

• Warning of mass extinction of species, including humans, within one decade
https://arctic-news.blogspot.com/2017/02/warning-of-mass-extinction-of-species-including-humans-within-one-decade.html

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What Does Runaway Warming Look Like?

October 08, 2018 warming

The forcing caused by the rapid rise in the levels of greenhouse gases is far out of line with current temperatures. A 10°C higher temperature is more in line with these levels, as illustrated by the image below.

Carbon dioxide levels have been above 400 ppm for years. Methane levels above 1900 ppb were recorded in September 2018. Such high levels are more in line with a 10°C higher temperature, as illustrated by the above graph based on 420,000 years of ice core data from Vostok, Antarctica, research station.

How fast could such a 10°C temperature rise eventuate? The image below gives an idea.

Such runaway warming would first of all and most prominently become manifest in the Arctic. In many ways, such a rise is already underway, as the remainder of this post will show.

High Arctic Temperatures

Why are Arctic temperatures currently so high for the time of year?

As warmer water enters the Arctic Ocean from the Atlantic and Pacific Oceans, there is no thick sea ice left to consume this heat. Some of this heat will escape from the Arctic Ocean to the atmosphere, as illustrated by above dmi.dk image showing very high temperatures for the time of the year over the Arctic (higher than 80°C latitude).

Above dmi.dk image shows that Arctic temperatures are increasingly getting higher during Winter in the Northern Hemisphere.

Similarly, above NASA image shows that Arctic temperatures are increasingly getting higher during Winter in the Northern Hemisphere.

As the Arctic warms up faster than the rest of the world, the Jet Stream is becoming more wavy, allowing more hot air to move into the Arctic, while at the same time allowing more cold air to move south.

Above image shows that the air over the Beaufort Sea was as warm as 12.8°C or 55°F (circle, at 850 mb) on October 2, 2018. The image also illustrates that a warmer world comes with increasingly stronger cyclonic winds.

The images above and below shows that on October 2 and 7, 2018, the sea surface in the Bering Strait was as much as 6°C or 10.7°F, respectively 6.4°C or 11.6°F warmer than 1981-2011 (at the green circle).

As temperatures on the continent are coming down in line with the change in seasons, the air temperature difference is increasing between - on the one hand - the air over continents on the Northern Hemisphere and - on the one hand - air over oceans on the Northern Hemisphere. This growing difference is speeding up winds accordingly, which in turn can also speed up the influx of water into the Arctic Ocean.

[ The Buffer has gone, feedback #14 on the Feedbacks page ]

Start of freezing period

Here's the danger. In October, Arctic sea ice is widening its extent, in line with the change of seasons. This means that less heat can escape from the Arctic Ocean to the atmosphere. Sealed off from the atmosphere by sea ice, greater mixing of heat in the water will occur down to the seafloor of the Arctic Ocean, while there is little or no ice buffer left to consume an influx of heat from the Atlantic and Pacific Oceans, increasing the danger that warm water will reach the seafloor of the Arctic Ocean and destabilize methane hydrates.

Rising salt content of Arctic Ocean

It's not just the influx of heat that is the problem. There's also the salt. Ice will stay frozen and will not melt in freshwater until the temperature reaches 0°C (or 32°F). Ice in saltwater on the other hand will already have melted away at -2°C (or 28.4°F).

The animation of the right shows salty water rapidly flowing through the Bering Strait.

With the change of seasons, there is less rain over the Arctic Ocean. The sea ice also seals the water of the Arctic Ocean off from precipitation, so no more fresh water will be added to the Arctic Ocean due to rain falling or snow melting on the water.

In October, temperatures on land around the Arctic Ocean will have fallen below freezing point, so less fresh water will flow from glaciers and rivers into the Arctic Ocean. At that time of year, melting of sea ice has also stopped, so fresh water from melting sea ice is no longer added to the Arctic Ocean either.

Pingos and conduits. Hovland et al. (2006)

So, the Arctic Ocean is receiving less freshwater, while the influx of water from the Atlantic and Pacific Oceans is very salty. This higher salt content of the water makes it easier for ice to melt at the seafloor of the Arctic Ocean. Saltier warm water is causing ice in cracks and passages in sediments at the seafloor of the Arctic Ocean to melt, allowing methane contained in the sediment to escape.

[ click on images to enlarge ]

The image on the right, from a study by Hovland et al., shows that hydrates can exist at the end of conduits in the sediment, formed when methane did escape from such hydrates in the past. Heat can travel down such conduits relatively fast, warming up the hydrates and destabilizing them in the process, which can result in huge abrupt releases of methane.

Heat can penetrate cracks and conduits in the seafloor, destabilizing methane held in hydrates and in the form of free gas in the sediments.

Methane

peak methane levels as high as 2859 ppb

On October 2 and 7, 2018, peak methane levels were as high as 2838 ppb, respectively 2859 ppb, as the images on the right shows. Methane levels over the Beaufort Sea have been high for some time, and have remained high at very high altitudes.

The threat is that a number of tipping points are going to be crossed, including the buffer of latent heat, loss of albedo as Arctic sea ice disappears, methane releases from the seafloor and rapid melting of permafrost on land and associated decomposition of soils, resulting in additional greenhouse gases (CO₂, CH₄, N₂O and water vapor) entering the Arctic atmosphere, in a vicious self-reinforcing cycle of runaway warming.

A 10°C rise in temperature by 2026?

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Peaks Matter

August 03, 2018 warming

Heat stress

When calculating how much warmer we can expect it to get, climate models typically use linear projections based on temperature averages, such as annual global average temperatures, daily temperatures that are averages between day and night, etc. Sadly, this downplays the danger, as average temperatures are unlikely to kill people. When lives are at stake, peaks matter!

Where are temperatures rising most?

Temperatures are rising most strongly in the Arctic. Above map shows a rise of as much as 5.7°C or 10.26°F in Arctic.

Ocean heat on the move toward Arctic Ocean

The image below shows that the sea surface was 22°C or 71.6°F on August 13, 2018, at 77.958°N, 5.545°E (near Svalbard), i.e. 6.9°C or 12.4°F warmer than 47 days earlier and 16.4°C or 29.5°F warmer than it was during 1981-2011.

Local maximum temperatures can be good indicators for the maximum heat stress that can be expected in the area.

As illustrated by above image, the sea surface near Svalbard was 22°C or 69.2°F at the green circle, near Svalbard, on August 13, 2018, 16.4°C or 29.5°F warmer than 1981-2011.

This high sea surface temperature is an indicator of the temperature of the water below the surface, which in turn is an indicator of the amount of ocean heat that is entering the Arctic Ocean from the Atlantic Ocean.

Ocean heat is carried by the Gulf Stream from the North American coast toward the Arctic Ocean, as illustrated by the images below and on the right.

Warming of the Arctic Ocean comes with a number of feedbacks that accelerate this warming, such as albedo changes that take place as the Arctic snow and ice cover declines, and methane that is released from sediments containing methane in the form of hydrates and free gas.

The situation could get worse rapidly. As an example, with a decrease in cooling aerosols, which are concentrated in the Northern Hemisphere, the North Atlantic looks set to absorb more heat. A recent study calculated that the North Atlantic’s share of the uptake could increase from 6% to about 27%.

As another example, a recent study concludes: Existing models currently attribute about 20% of the permafrost carbon feedback this century to methane, with the rest due to carbon dioxide from terrestrial soils. By including thermokarst lakes, methane becomes the dominant driver, responsible for 70% to 80% of permafrost carbon-caused warming this century. Adding thermokarst methane to the models makes the feedback’s effect similar to that of land-use change, which is the second-largest source of manmade warming.

High methane levels warn about seafloor methane releases

The image on the right illustrates the danger, showing high methane levels at Barrow, Alaska, in July 2018.

When making projections of heat stress, it is important to look at all potential warming elements, including albedo changes, changes to jet streams and sea currents, higher levels of methane, high levels of water vapor, etc.

Methane is a potent greenhouse gas, causing huge warming immediately after entering the atmosphere, while this warming will be felt most strongly where the methane was released. Methane can therefore contribute strongly to local temperature peaks.

On August 6, 2018, mean global methane levels were as high as 1896 ppb. On August 8, 2018, they were as high as 1898 ppb.

Importantly, peak levels on the afternoon of August 6, 2018, were as high as 3046 ppb, as illustrated by the image on the right. The likely origin of those high levels is the Arctic Ocean, which should act as a stark warning of things to come.

Further contributors to heat stress

Next to temperature, humidity is of vital importance. A combination of high temperatures and high humidity is devastating.

A recent study shows that the risk of deadly heat waves is significantly increased because of intensive irrigation in specific regions. The study points at a relatively dry but highly fertile region, known as the North China Plain — a region whose role in that country is comparable to that of the Midwest in the U.S. That increased vulnerability to heat arises because the irrigation exposes more water to evaporation, leading to higher humidity in the air than would otherwise be present and exacerbating the physiological stresses of the temperature.

The image below shows a forecast of perceived temperatures in China on August 7, 2018.

The green circle highlights an area that is forecast to score high on the 'Misery Index' and that is centered around a location on the coast of Poyang Lake, which is connected to the Yangtze River. Temperatures there are forecast to be as high as 36.4°C or 97.4°F. At first glance, this may not look very high, but a relative humidity 68% is forecast to make it feel like 54.1°C or 129.3°F. This translates into a wet-bulb temperature of 31.03°C or 87.86°F.

The image on the right shows relative humidity. Also note the cyclones lined up on the Pacific Ocean. Cyclones can increase humidity, making conditions worse.

The high sea surface temperature anomalies that are common in the West Pacific (image right) contribute to warmer air and stronger cyclones carrying more moisture toward Asia, as discussed in this facebook thread which also features the next image on the right, showing that cyclone Soulik is forecast to cause waves as high as 18.54 m or 60.8 ft near Japan on August 20, 2018.

If humidity kept rising, a temperature of 36.4°C at a relative humidity of 91% would result in a wet-bulb temperature of 35°C. No amount of sweating, even in the shade and in front of strong winds or a fan, can cool the body under such conditions, and it would be lethal in a matter of hours in the absence of air conditioning or cold water.

There are further factors that can contribute to make specific areas virtually uninhabitable. The urban heat effect is such a factor. El Niño is another one. Land-only temperature anomalies are higher than anomalies that are averaged for land and oceans. As temperatures keep rising, heat waves can be expected to intensify, while their duration can be extended due to jet stream blocking.

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

Below, Paul Beckwith warns that parts of the world 'will soon be rendered uninhabitable'.

Regions to Soon Be Uninhabitable, From Unrelenting Heat and Humidity

Video: Unrelenting Heat, Humidity Will Soon Make Regions UNINHABITABLE

Paul Beckwith: "How hot can it actually get? What is in store for us? When you combine the heat domes sitting over many countries with high humidity, many areas around the planet will soon reach the deadly 35°C (95°F) 100% humidity (wet bulb temperature) or equivalent situation whereby a perfectly healthy person outside, in a well ventilated area, in the shade will die from the heat in 6 hours."

Video: Most Mammals Endure Heat Waves Better Than Humans

"Most people, like the very young, the elderly, and the rest of us won’t last anywhere as long, at even lower temperatures. I discuss the latest peer-reviewed science on how parts of high-risk regions in the North China Plains, Middle East, and South Asia will soon be rendered uninhabitable by combined heat and humidity."