Showing posts sorted by relevance for query methane plume. Sort by date Show all posts
Showing posts sorted by relevance for query methane plume. Sort by date Show all posts

Wednesday, November 11, 2020

Above Zero Celsius at North Pole November 2020

Above image shows that, in October 2020, the Arctic Ocean was very hot. The Copernicus image below shows temperatures averaged over the twelve-month period from November 2019 to October 2020.

Keep in mind that, in the Copernicus image, anomalies are compared to the 1981-2010 average.

Note that the shape of the recent twelve-month period is similar to the 2016 peak, when there was a strong El Niño, while in October 2020 the temperature was suppressed due to La Niña and due to low sunspots.

The image below shows how a hot Arctic Ocean distorts the Jet Stream and hot air moves all the way up to the North Pole. 

Above image shows the Northern Hemisphere at November 12, 2020, with a temperature forecast of 2.0°C or 35.5°F at the North Pole at 1000 hPa at 15:00Z. On the right, jet stream crosses the Arctic Ocean (at 250 hPa). At surface level, a temperature was forecast to be 0.6°C or 33.2°F. 


As it turned out, the highest temperature at the North Pole was 1.1°C or 34.1°F on November 12, 2020, at 1000 hPa at 18:00Z, as above image shows. At 15:00Z that day, a temperature of 1.9°C or 35.3°F was recorded at 1000 hPa just south of the North Pole, at 89.50° N, 1.50° E.

The image below shows temperature anomalies for November 12, 2020, with forecasts approaching 30°C. 


[ Click on images to enlarge ]
These high temperatures over the Arctic Ocean are caused by transfer of huge amounts of heat from the Arctic Ocean to the atmosphere, indicating severe overheating of the Arctic Ocean as a result of the ongoing movement of ocean heat at the surface of the North Atlantic to the Arctic Ocean along the Gulf Stream. 

As the image on the right shows, temperature anomalies above 20°C were recorded over a large part of the Arctic Ocean on November 16, 2020. 

As illustrated by the image below, temperature anomalies are forecast to remain high over the Arctic Ocean, with the forecast for November 26, 2020, showing anomalies approaching 30°C. 


The resulting distortion of the Jet Stream can at times speed up winds that move hot air from the North Atlantic Ocean toward to Arctic Ocean, as illustrated by the image at the top. 

[ click on images to enlarge ]
The image on the right shows that the Jet Stream was as fast as 411 km/h or 255 mph south of Greenland (at the green circle), before crossing the Arctic Ocean on November 4, 2020. 

The image below shows how, on November 20, 2020 15:00 UTC, a distorted Jet Stream reaches a speed of 327 km/h or 203 mph (at circle, globe left). At 850 hPa, wind reaches speeds as high as 161 km/h or 100 mph (circle, globe right). 

The danger is that such strong wind will speed up ocean currents in the North Atlantic that carry huge amounts of heat toward the Arctic Ocean. 


The image below shows sea surface temperature anomalies compared to 1981-2011 on the Northern Hemisphere on October 23, 2020, when anomalies off the coast of North America were as high as 10.8°C or 19.5°F (left), and on December 3, 2020, when anomalies off the coast of North America were as high as 12.7°C or 22.8°F (right). 


According to a recent news report, an atmospheric river smashed into Juneau, Alaska, dropping 5.08 inches of rain in 24 hours ending 3 a.m. Wednesday December 2, 2020.

This is not an isolated event, but a symptom of the unfolding catastrophe referred to as global warming, which threatens to remove all life from Earth.

Sea surface temperatures around North America are very high. The above image shows that sea surface temperatures were as much as 12.7°C or 22.8°F higher than 1981-2011 off the east coast of North America on December 3, 2020 (green circle). On the image below, the globe on the left shows that sea surface temperature anomalies (SSTA) were as high as 4.1°C or 7.3°F off the west coast of North America on December 4, 2020 (at the green circle).

These high sea surface temperatures speed up de Jet Stream over oceans. At this time of year, temperatures over continents are low, so there is greater ocean/land temperature difference, which further speeds up the Jet Stream where it travels over oceans toward continents. The center globe shows wind as fast as 381 km/h or 237 mph at the time (at circle). 

At the same time, the narrowing temperature difference between the Equator and the North Pole is slowing down the Jet Stream. This is making the Jet Stream more wavy at higher latitudes, even resulting in circular wind patterns, and this can make a lot of cold air leave the Arctic and move over continents, thus further widening the ocean/land temperature difference. Given that more than 90% of global warming goes into oceans, this is an important self-reinforcing feedback of global warming. 

Stronger wind results in stronger evaporation, which cools down the sea surface somewhat, as the blue areas over the Pacific Ocean indicate. Due to the strong wind, much of the moisture falls down farther on the path of the wind. The globe on the right shows 3-hour precipitation accumulation as high as 31.3 mm or 1.23 in off the west coast of North America (green circle). 


The image below shows an earlier analysis, describing the situation in September 6, 2020, when high sea surface temperatures on the Northern Hemisphere and a narrow difference between the Equator and the North Pole distorted the Jet Stream, making it cross the Arctic Ocean, form circular wind patterns and reach speeds as fast as 262 km/h or 163 mph (250 hPa, green circle) over the North Atlantic. The globe on the right shows that the Gulf Stream off the North American coast reached speeds of 8 km/h or 5 mph (at green circle). 

[ click on images to enlarge ]

More ocean heat can move into the Arctic Ocean for a number of reasons, including: 
  • At times, the Jet Stream becomes very strong and elongated over the North Atlantic, speeding up the flow of ocean heat along the path of Gulf Stream all the way to the Arctic Ocean;
  • Overall, winds are getting stronger, speeding up ocean currents running just below the sea surface;
  • Stratification of the North Atlantic results in less heat mixing down to lower parts of the ocean; and 
  • Increased evaporation and increased subsequent rainfall farther down the path of the Gulf Stream forms a colder freshwater lid stretched out at the sea surface from the North Atlantic to the Arctic Ocean, sealing off transfer of heat from ocean to atmosphere and consequently moving more heat just underneath the sea surface into the Arctic Ocean.

    [ from earlier post ]
As the image below shows, sea surface temperatures as high as 16.6°C or 61.9°F were recorded north of Svalbard on November 9, 2020. 


As the image below shows, the N2O satellite recorded a peak methane level of 2762 ppb on the morning of November 16, 2020.


As the image below shows, the MetOp-1 satellite recorded a peak methane level of 2725 ppb on the afternoon of November 18, 2020.


The video below shows a methane plume or bubble cloud spotted by a team of 69 scientists from ten countries documenting bubble clouds rising from a depth of around 300 metres (985ft) along a 150km (93 mile) undersea slope in the Laptev Sea.


The danger is that even more hot and salty water will reach the shallow parts of the Arctic Ocean that contain huge amounts of methane in the form of hydrates and free gas in sediments at the seafloor, resulting in huge eruptions of methane that, on its own, could almost instantly cause the 1200 ppm CO₂e cloud feedback tipping point to be crossed, which can cause global temperatures to rise by 8°C.

Latent heat loss, feedback #14 on the Feedbacks page

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


Links

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

• NASA GISS Surface Temperature Analysis - global maps

• Copernicus - surface air temperature for October 2020

• Climate Reanalyzer

• nullschool earth wind map

• Atmospheric River Smashes Alaskan Capital’s 24-Hour Rain Record

• Bubbling methane craters and super seeps - is this the worrying new face of the undersea Arctic? - by Valeria Sukhova, Olga Gertcyk - Siberian Post

• Why stronger winds over the North Atlantic are so dangerous

• Feedbacks in the Arctic

• September 2015 Sea Surface Warmest On Record

Thursday, February 18, 2016

Has maximum sea ice extent already been reached this year?

An earlier post wondered whether maximum extent for this year had already been reached, i.e. on February 9, 2016, when sea ice extent was 14.214 million km2.

As illustrated by the image below, extent since has been lower, including on the two most recent days on the image, i.e. on February 16 and 17, 2016, when extent was respectively 14.208 and 14.203 million km2.



Last year (2015), maximum sea ice extent was reached on February 25. That's close to the most recent date on the image of February 17, so with El Nino still going strong, it may well be that the maximum in 2016 will be reached early.

On the other hand, strong winds could spread out the sea ice and speed up its drift out of the Arctic Ocean, which may result in a larger extent, but which won't do much to strengthen the sea ice.

UPDATES: On February 18, 2016 (arrow), Arctic sea ice extent was 14.186 million square km, i.e. less than it was on February 9. In fact, sea ice extent hasn't been higher on any day since February 9, 2016. So, the question is, has this year's maximum extent already passed us by (i.e. on February 9)?

The image below shows the heat is having a huge impact on the sea ice, with some areas (black) showing sea surface temperature anomalies above 8°C (or above 14.4°F).


Ominously, sea surface off the North American east coast was as much as 11.8°C or 21.3°F warmer on February 19, 2016, than it was in 1981-2011 (at the location marked by the green circle in the image below).


Temperatures over the Arctic Ocean are forecast to remain extremely high for the next five days, with anomalies in a large part of the Arctic Ocean at the top end of the scale, i.e. 20°C or 36°F.


As the image below shows, Arctic sea ice area was at a record low for the time of year on February 18, 2016.



The image below shows that Arctic sea ice extent on February 20, 2016, was only 14.166
million km2 (arrow), adding to fears that this year's maximum was already reached on February 9.


The image below shows that Arctic sea ice extent on February 21, 2016, was only 14.160
million km2 (arrow), further fueling fears that this year's maximum was already reached on February 9.


Meanwhile, very high methane levels, as high as 3096 parts per billion, were recorded on February 20, 2016, as shown by the image below.


Further analysis indicates that these high levels likely originated from destabilizing methane hydrates in sediments, from a location about latitude 85°North and longitude +105° (East), on the Gakkel Ridge, just outside the East Siberian Arctic Shelf, at the location of the red marker on the map below.

Below is a comparison map, from grida.no
for large-size image, go to grida.no
Below is a map with sea surface temperature anomalies on February 20, 2016. The green circle marks the likely location of sediment destabilization and subsequent methane plume, at about latitude 85°North and longitude +105° (East), on the Gakkel Ridge, just outside the East Siberian Arctic Shelf.

zoom in and out at nullschool.net
If you like, you can discuss this further at the Arctic News group or below.


On February 18, 2016 (arrow), Arctic sea ice extent was 14.186 million square km, i.e. less than it was on February 9....
Posted by Sam Carana on Friday, February 19, 2016

Thursday, July 13, 2017

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.



Links

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

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

• Abrupt Warming - How Much And How Fast?
https://arctic-news.blogspot.com/2017/05/abrupt-warming-how-much-and-how-fast.html

• Accelerating growth in CO₂ levels in the atmosphere
https://arctic-news.blogspot.com/2017/02/accelerating-growth-in-co2-levels-in-the-atmosphere.html

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

• Turning forest waste into biochar
https://arctic-news.blogspot.com/2013/01/turning-forest-waste-into-biochar.html


Earlier posts on Wildfires

• Wildfires in Russia's Far East
https://arctic-news.blogspot.com/2016/08/wildfires-in-russias-far-east.html

• Wildfire Danger Increasing
https://arctic-news.blogspot.com/2016/05/wildfire-danger-increasing.html

• Smoke Blankets North America
https://arctic-news.blogspot.com/2014/07/smoke-blankets-north-america.html

• More on Wildfires
https://arctic-news.blogspot.com/2013/08/more-on-wildfires.html

• Wildfires even more damaging
https://arctic-news.blogspot.com/2013/07/wildfires-even-more-damaging.html

• Wildfires in Canada affect the Arctic
https://arctic-news.blogspot.com/2013/07/wildfires-in-canada-affect-the-arctic.html

• The Threat of Wildfires in the North
https://arctic-news.blogspot.com/2013/06/the-threat-of-wildfires-in-the-north.html

• Russia: 74 million acres burned through August 2012
https://arctic-news.blogspot.com/2012/09/russia-74-million-acres-burned-through-august-2012.html

• Earth on Fire
https://arctic-news.blogspot.com/2012/06/earth-on-fire.html

• Fires are raging again across Russia
https://arctic-news.blogspot.com/2012/06/fires-are-raging-again-across-russia.html


Further reading on wildfires and aerosols

• NASA: Grassland Fires Tear Through Montana
https://earthobservatory.nasa.gov/NaturalHazards/view.php?id=90622

• 2016 fire risk for South America
http://www.ess.uci.edu/~amazonfirerisk/ForecastWeb/SAMFSS2016.html

• Global Fire Data - 2015 Indonesian fires
http://www.globalfiredata.org/updates.html#2015_indonesia

• Indonesia’s Fire Outbreaks Producing More Daily Emissions than Entire US Economy (2015)
http://www.wri.org/blog/2015/10/indonesia%E2%80%99s-fire-outbreaks-producing-more-daily-emissions-entire-us-economy

• Indonesia’s 2015 fires killed 100,000 people, study finds
http://www.climatechangenews.com/2016/09/19/indonesias-2015-fires-killed-100000-people-study-finds

• Smoke from 2015 Indonesian fires may have caused 100,000 premature deaths
https://www.seas.harvard.edu/news/2016/09/smoke-from-2015-indonesian-fires-may-have-caused-100000-premature-deaths

• Impact of anthropogenic climate change on wildfire across western US forests, by Abatzoglou et al.
http://www.pnas.org/content/113/42/11770.abstract

• The Mean and Turbulent Properties of A Wildfire Convective Plume, by Lareau et al.
http://journals.ametsoc.org/doi/10.1175/JAMC-D-16-0384.1

• Airborne measurements of western U.S. wildfire emissions: Comparison with prescribed burning and air quality implications, by Liu et al.
http://onlinelibrary.wiley.com/doi/10.1002/2016JD026315/abstract

• Hemispheric climate shifts driven byanthropogenic aerosol–cloud interactions, by Chung et al.
http://www.nature.com/ngeo/journal/vaop/ncurrent/full/ngeo2988.html

• Effects of biomass burning on climate, accounting for heat and moisture fluxes, black and brown carbon, and cloud absorption effects, by Mark Z. Jacobson
http://onlinelibrary.wiley.com/doi/10.1002/2014JD021861/abstract

• Amplification of global warming through pH-dependence of DMS-production simulated with a fully coupled Earth system model, by Jörg Schwinger et al.
https://www.biogeosciences-discuss.net/bg-2017-33

• Role of volcanic and anthropogenic aerosols in the recent global surface warming slowdown, by Doug M. Smith et al.
http://www.nature.com/nclimate/journal/v6/n10/full/nclimate3058.html

• Slow climate mode reconciles historical and model-based estimates of climate sensitivity, by Proistosescu et al.
http://advances.sciencemag.org/content/3/7/e1602821.full

• Young People’s Burden: Requirement of Negative CO2 Emissions, by James Hansen
http://csas.ei.columbia.edu/2017/07/18/young-peoples-burden-requirement-of-negative-co2-emissions