Arctic News: soot

Showing posts with label soot. Show all posts

Tuesday, July 30, 2019

Arctic Sea Ice Gone By September 2019?

Record low Arctic sea ice extent for the time of year

Arctic sea ice minimum extent typically occurs about half September. In 2012, minimum extent was reached on September 17, 2012, when extent was 3.387 million km².

On July 28, 2019, Arctic sea ice extent was 6.576 million km². How much extent do you think there will be by September 17, 2019? From July 28, 2019, to September 17, 2019, that's a period of 52 days during which a lot of melting can occur. Could there be a Blue Ocean Event in 2019, with virtually all sea ice disappearing in the Arctic?

Consider this. Extent was 6.926 million km² on September 17, 1989. Extent was 3.387 million km² on September 17, 2012, so 3.539 million km² had disappeared in 23 years. Over those years, more ice extent disappeared than what was left on September 17, 2012.

The question is how much sea ice extent will be left when it will reach its minimum this year, i.e. in September 2019. The red dashed line on the image at the top continues the path of the recent fall in sea ice extent, pointing at zero Arctic sea ice extent in September 2019. Progress is followed at this post.

Zero Arctic sea ice in 2019

Zero Arctic sea ice in 2019 sounds alarming, and there is good reason to be alarmed.

Above map shows temperatures on Greenland on July 31, 2019, with temperatures at one location as high as 23.2°C or 73.8°F and at another location - in the north - as high as 14.2°C or 57.6°F.

The map on the right shows sea surface temperature anomalies compared to 1961-1990 as on July 29, 2019. Note the high anomalies in the areas where the sea ice did disappear during the past few months. The reason for these high anomalies is that the buffer has disappeared that previously had kept consuming heat in the process of melting.

Where that buffer is gone, the heat has to go somewhere else, so it will be absorbed by the water and it will also speed up heating of the atmosphere over the Arctic.

Sea ice melting is accelerating for a number of reasons:

Ocean Heat - Much of the melting of the sea ice occurs from below and is caused by heat arriving in the Arctic Ocean from the Atlantic Ocean and the Pacific Ocean.
Direct Sunlight - Hot air will melt the ice from above and this kind of melting can increase strongly due to changing wind patterns.
Rivers - Heatwaves over land can extend over the Arctic Ocean and they also heat up river water flowing into the Arctic Ocean.
Fires - Changing wind patterns can also increase the intensity and duration of such heatwaves that can also come with fires resulting in huge amounts of greenhouse gas emissions, thus further speeding up the temperature rise, and also resulting in huge emissions of soot that, when settling on sea ice, speeds up melting (see images below).
Numerous feedbacks will further speed up melting. Heating is changing the texture of the sea ice at the top and is making melt pools appear, both of which cause darkening of the surface. Some further feedbacks, i.e. storms and clouds are discussed below in more detail.

Above combination image shows smoke from fires in Siberia getting pushed over the Laptev Sea on August 11, 2019, due to cyclonic winds over the Arctic Ocean. This was also discussed in an earlier post. The image below shows the situation on August 12, 2019.

The image below shows the situation on August 14, 2019.

In the video below, Paul Beckwith discusses the situation.

In the video below, Paul Beckwith discusses the heating impact of albedo loss due to Arctic sea ice loss, including the calculations in a recent paper.

As the Arctic is heating up faster than the rest of the world, it is also more strongly affected by the resulting extreme weather events, such as heatwaves, fires, strong winds, rain and hail storms, and such events can strongly speed up the melting of the sea ice.

All around Greenland, sea ice has now virtually disappeared. This is the more alarming considering that the thickest sea ice was once located north of Greenland. This indicates that the buffer is almost gone.

Why is disappearance of Arctic sea ice so important? Hand in hand with albedo loss as the sea ice disappears, there is loss of the buffer (feedbacks #1, #14 and more). As long as there is sea ice in the water, this sea ice will keep absorbing heat as it melts, so the temperature will not rise at the sea surface. The amount of energy absorbed by melting ice is as much as it takes to heat an equivalent mass of water from zero to 80°C.

Once the sea ice is gone, further heat must go elsewhere. This heat will raise the temperature of the water and will also make the atmosphere heat up faster.

Storms and Clouds

Storms: As temperatures in the Arctic are rising faster than at the Equator, the Jet Stream is changing, making it easier for warm air to enter the Arctic and for cold air to descend over continents that can thus become much colder than the oceans, and this stronger temperature difference fuels storms.

Clouds: More evaporation will occur as the sea ice disappears, thus further heating up the atmosphere (technically know as latent heat of vaporization).

In the video below, Paul Beckwith further discusses Arctic albedo change and clouds.

Disappearance of the sea ice causes more clouds to form over the Arctic. This on the one hand makes that more sunlight gets reflected back into space. On the other hand, this also make that less outward infrared radiation can escape into space. The net effect of more clouds is that they are likely cause further heating of the air over the Arctic Ocean (feedbacks #23 and #25).

More low-altitude clouds will reflect more sunlight back into space, and this occurs most during Summer when there is most sunshine over the Arctic. The image below, a forecast for August 17, 2019, shows rain over the Arctic. Indeed, more clouds in Summer can also mean rain, which can devastate sea ice, as discussed in an earlier post.

Regarding less outward radiation, the IPCC has long warned, e.g. in TAR, about a reduction in outgoing longwave radiation (OLR): "An increase in water vapour reduces the OLR only if it occurs at an altitude where the temperature is lower than the ground temperature, and the impact grows sharply as the temperature difference increases."

While reduction in OLR due to water vapor is occurring all year long, the impact is particularly felt in the Arctic in Winter when the air is much colder than the surface. In other words, less OLR makes Arctic sea ice thinner, especially in Winter.

The inflow of ocean heat into the Arctic Ocean can increase strongly as winds increase in intensity. Storms can push huge amounts of hot, salty water into the Arctic Ocean, as discussed earlier, such as in this post and this post. As also described at the extreme weather page, stronger storms in Winter will push more ocean heat from the Atlantic toward the Arctic Ocean, further contributing to Arctic sea ice thinning in Winter.

Seafloor Methane

[ The Buffer has gone, feedbacks #14 and #16 ]

As the buffer disappears that until now has consumed huge amounts of heat, the temperature of the water of the Arctic Ocean will rise even more rapidly, with the danger that further heat will reach methane hydrates at the seafloor of the Arctic Ocean, causing them to get destabilized and release huge amounts of methane (feedback #16).

Ominously, high methane levels were recorded at Barrow, Alaska, at the end of July 2019, as above image shows.

[ from an earlier post ]

And ominously, a mean global methane level as high as 1902 ppb was recorded by the MetOp-1 satellite in the afternoon of July 31, 2019, as above image shows.

As the image on the right shows, mean global levels of methane (CH₄) have risen much faster than carbon dioxide (CO₂) and nitrous oxide (N₂O), in 2017 reaching, respectively, 257%, 146% and 122% their 1750 levels.

Temperature Rise

Huge releases of seafloor methane alone could make marine stratus clouds disappear, as described in an earlier post, and this clouds feedback could cause a further 8°C global temperature rise.

Indeed, a rapid temperature rise of as much as 18°C could result by the year 2026 due to a combination of elements, including albedo changes, loss of sulfate cooling, and methane released from destabilizing hydrates contained in sediments at the seafloor of oceans.

[ from an earlier post ]

Below is Malcolm Light's updated Extinction Diagram.

[ click on images to enlarge ]

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

Link

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

• Smoke Covers Much Of Siberia
https://arctic-news.blogspot.com/2019/07/smoke-covers-much-of-siberia.html

• Extreme Weather
https://arctic-news.blogspot.com/p/extreme-weather.html

• Albedo and more
https://arctic-news.blogspot.com/p/albedo.html

• Radiative Heating of an Ice‐Free Arctic Ocean, by Kristina Pistone et al. (2019)
https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2019GL082914

• High cloud coverage over melted areas dominates the impact of clouds on the albedo feedback in the Arctic, by Min He et al. (2019)
https://www.nature.com/articles/s41598-019-44155-w

• ESD Reviews: Climate feedbacks in the Earth system and prospects for their evaluation, by Christoph Heinze et al. (2019)
https://www.earth-syst-dynam.net/10/379/2019/esd-10-379-2019-discussion.html

• Contribution of sea ice albedo and insulation effects to Arctic amplification in the EC-Earth Pliocene simulation, by Jianqiu Zheng et al. (2019)
https://www.clim-past.net/15/291/2019

• Far-infrared surface emissivity and climate, by Daniel Feldman et al. (2014)
https://www.pnas.org/content/111/46/16297.abstract

• Extreme Weather
https://arctic-news.blogspot.com/p/extreme-weather.html

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

• Rain Storms Devastate Arctic Ice And Glaciers
https://arctic-news.blogspot.com/2015/01/rain-storms-devastate-arctic-ice-and-glaciers.html

• A rise of 18°C or 32.4°F by 2026?
https://arctic-news.blogspot.com/2019/02/a-rise-of-18c-or-324f-by-2026.html

• As El Niño sets in, will global biodiversity collapse in 2019?
https://arctic-news.blogspot.com/2018/11/as-el-nino-sets-in-will-global-biodiversity-collapse-in-2019.html

• Dangerous situation in Arctic
https://arctic-news.blogspot.com/2018/11/dangerous-situation-in-arctic.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

Thursday, July 25, 2019

Smoke Covers Much Of Siberia

Smoke covers much of Siberia, as shown by the NASA Worldview image dated July 25, 2019.

The enormous intensity of the fires is illustrated by the image below, showing carbon monoxide (CO) levels as high as 80,665 ppb on July 25, 2019.

The image below shows that, at that same spot on July 25, 2019, carbon dioxide (CO₂) levels were as high as 1205 ppm.

The image below shows that aerosols from biomass burning were at the top end of the scale.

When soot from fires settles on snow and ice, it darkens the surface, resulting in more sunlight getting absorbed (instead of reflected back into space, as was previously the case), thus further speeding up the melting.

The loss of sea ice north of Greenland is particularly worrying, since this is the area where once the thickest sea ice was present. The image below shows the situation on July 24, 2019.

The image below shows the sea ice disappearing north of Greenland and Ellesmere Island on July 25, 2019.

The huge recent fall in sea ice volume is illustrated by the graph below, by Wipneus.

The naval.mil animation below illustrates the rapid fall in sea ice thickness, showing 30-day period including seven forecasts up to August 1, 2019.

The combination image below shows sea ice thickness forecasts for July 25, 2019, and for August 1, 2019.

The video below, by Robin Westenra, further illustrates our predicament.

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

Links

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

Monday, August 14, 2017

Arctic Sea Ice Break Up August 2017

Sun at 8:00 am, captured by Jim Reeve on August 7, 2017 near Sechelt AirPort, B.C., Canada

Arctic sea ice is under attack from all sides. At this time of year, the sun doesn't set at the higher latitudes.

As the image below shows, it was as hot as 94°F or 34.5°C in North Canada on August 13, 2017 (at the green circle, at 1000 hPa, at 00:00 UTC). Temperatures at surface level were as high as 33.1°C or 91.5°F at that location, where wind was coming from the south and blowing toward the north at a speed of 28 km/h or 17 mph at that time.

Above image shows cyclonic winds over the Arctic Ocean pulling warm air from North Canada over the Arctic Ocean, while pushing cold air out. Winds and rain have been battering the sea ice for some time now, as discussed in an earlier post.

Fires are becoming more devastating, as discussed in an earlier post. The August 2, 2017, satellite image below shows smoke from fires in British Columbia blanketing Vancouver and Seattle. Carbon dioxide (CO₂) levels were as high as 527 ppm, carbon monoxide (CO) levels as high as 12.59 ppm and sulfur dioxide (SO₂) levels as high as 490.77 µg/m³, as these images show.

The combination image below shows forecasts for August 8, 2017, 13:30 UTC. CO levels were forecast to be as high as 29.05 ppm, CO₂ levels as high as 625 ppm and SO₂ levels as high as 1089.65 µg/m³ (each time at the green circle). Also note the emissions from forest fires in Siberia.

Actual levels were even higher at that spot on August 11, 2017, when CO was as high as 30.97 ppm, CO₂ was as high as 633 ppm and SO₂ was as high as 1150.19 µg/m³, as illustrated by the image below.

[ click on images to enlarge ]

The image below, by Harold Hensel, shows smoke over British Columbia, Washington, and Montana on August 9, 2017.

Winds can carry smoke from forest fires over long distances, all the way to the Arctic sea ice, where the soot can settle and darken the ice, thus speeding up its decline. The image below, also by Harold Hensel, shows smoke from fires in Russia entering the Arctic Ocean near the Laptev Sea on August 9, 2017.

The image below shows the situation on August 14, 2017.

Canadian wildfires caused PM10 to reach levels as high as 11,599 μg/m³ on August 16, 2017, at the location marked by the green circle. The image below shows PM10 getting blown over the Arctic Ocean.

The thickest sea ice in the Arctic Ocean is located close to the north of Greenland and the Canadian Archipelago. This ice is now breaking up, due to high temperatures and strong cyclonic winds that cause warm rain, high waves and strong sea currents.

Watch the thickest sea ice break up on the animation below. This is a 17 MB file, so it may take some time to fully load. Click here if you do not see the file appear below.

Wildfires

Levels of carbon dioxide (CO2) in the atmosphere are accelerating, even though emissions from fossil fuel burning have remained virtually the same over the past few years.

One of the reason behind this is accelerating emissions from wildfires as temperatures are rising.

Wildfires in Nevada caused CO2 to reach levels as high as 742 ppm on July 12, 2017 (green circle image on the right).

Global warming is greatly increasing the chance for what was previously seen as an extreme weather event to occur, such as a combination of droughts and storms. Heat waves and droughts can cause much vegetation to be in a bad condition, while high temperatures can come with strong winds, storms and lightning.

Wildfires cause a range of emissions, including CO2, soot, methane and carbon monoxide (CO). In Nevada, CO levels were as high as 30.43 ppm (green circle image right).

Above satellite image below shows the smoke plumes and the charred area. The google maps image below further shows where the fires were burning.

At the moment, wildfires are hitting many places around the world.

Wildfires caused carbon dioxide to reach levels as high as 746 ppm in Kazakhstan on July 11, 2017 (green circle on image on the right).

Carbon monoxide levels in the area were as high as 20.96 ppm on July 10, 2017.

The satellite image shows wildfires in Kazakhstan on July 9, 2017.

The satellite images show wildfires in Kazakhstan on July 11, 2017.

On July 16, 2017, CO₂ reached levels as high as 830 ppm in North America at the location marked by the green circle on the image below. Note that fires are burning at multiple locations.

The image below shows the location (red marker) where the fires burned in Canada.

That same day, July 16, 2017, CO₂ reached levels as high as 873 ppm in Mongolia, as shown by the image on the right.

The image also shows further fires burning in Siberia.

Carbon monoxide levels were as high as 37.19 ppm where the fires burned in Mongolia on July 16, 2017, as shown by the image below.

The image below shows the location (red marker) where the fires burned in Mongolia. The image also shows Lake Baikal across the border with Russia.

On July 22, 2017, CO₂ reached levels as high as 1229 ppm in Montana, while CO levels at the time were as high as 56.38 ppm at that location (green circle on image below).

The satellite image below shows the situation in Montana on the next day, July 23, 2017. See also the
NASA post Grassland Fires Tear Through Montana.

Furthermore, on July 23, 2017, CO₂ reached levels as high as 884 ppm at another (nearby) location in Montana (green circle on image below).

Meanwhile, temperatures keep rising. Surface temperature as high as 53.1°C or 127.5°F were forecast in Iran for July 11, 2017, at the location marked by the green circle on the image below.

At 1000 mb (image below), temperatures in Iran were forecast to be slightly lower, i.e. as high as 51.9°C or 125.3°F at the location marked by the at green circle, but note the difference in color, especially over Greenland, the Himalayas and the Tibetan Plateau.

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

Aerosols

Some aerosols, particularly sulfur dioxide, have a cooling effect, making that they partly mask the warming effect of other emissions by people. The IPCC AR4 image below shows that the direct and cloud albedo effect of aerosols equals a radiative forcing of as much as -2.7 W/m². In other words, if this masking effect were to fall away, warming would increase by as much as 2.7 W/m², according to IPCC AR4 figures.

Anthropogenic aerosols are also suppressing the Pacific Decadal Oscillation, making that less heat gets transferred from oceans to the atmosphere. Recent research concludes that future reduction of anthropogenic aerosol emissions, particularly from China, would promote positive Pacific Decadal Oscillation, thus further speeding up warming over the coming years.

Dimethyl sulphide emissions from oceans constitute the largest natural source of atmospheric sulphur, and such emissions can decrease with ongoing ocean acidification and climate change. This could particularly impact specific regions such as Antarctica, speeding up warming and loss of sea ice there, as discussed at this paper.

The net warming effect of open biomass burning was estimated in a 2014 study by Mark Jacobson to amount to 0.4 W/m² of radiative forcing. Imagine a scenario in which many people stopped burning fossil fuels for heating, cooking and energy. That would be great, but if many of them instead switched to burning biomass in woodburners and open fires, while wildfires increased strongly, the net warming from associated aerosols would increase dramatically.

A recent paper by James Hansen uses equilibrium fast-feedback climate sensitivity of ¾°C per W/m², while another recent paper suggest that the temperature rise per W/m² could be even stronger.

A high-end increase in net radiative forcing combined with a strong temperature rise per W/m² could cause a temperature rise as a result of changes in aerosols of as much as 2.5°C in a matter of years, as suggested in earlier posts such as this one.