Showing posts with label volume. Show all posts
Showing posts with label volume. Show all posts

Blue Ocean Event September 2017?

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Will there be a Blue Ocean Event in September 2017, during which the Arctic Ocean will be virtually ice-free? What would be the significance of such an event?

The Arctic Ocean is about to become virtually ice-free, perhaps as early as next year. At first, this Blue Ocean Event may last for one or more days in September 2017. Over the years, the ice-free period will grow longer and longer, if no action is taken.

Projections of an ice-free Arctic Ocean have been made for years. What makes the prospect of a Blue Ocean Event so dire?

Disappearance of the sea ice means that a huge amount of sunlight that was previously reflected back into space, is instead getting absorbed by the Arctic. The reason for this is that sea ice is more reflective than the water of the Arctic Ocean. The situation on land in the Arctic is similar, i.e. the snow and ice cover on land is more reflective than the darker soil and rocks that get uncovered as the snow and ice disappears. So, extra heat gets added and this is accelerating warming in the Arctic. On land, extra heat will also warm up water of rivers, and a lot of this heat will end up in the Arctic Ocean.

Another feedback is water vapor, as highlighted in the diagram below.


A warmer atmosphere carries more water vapor. Since water vapor is a potent greenhouse gas, this further accelerates warming over the Arctic.


As above image shows, temperatures have been more than 2.5°C warmer than 1981-2010 over most of the Arctic Ocean over the past 365 days (up to October 7, 2016). Accelerated Arctic warming has been taking place for a long time. So, what is it that makes a Blue Ocean Event, a virtually ice-free Arctic Ocean, such a big thing?

It is a huge event, because once the sea ice is gone, warming of the Arctic Ocean is likely to speed up even more dramatically. Why? Because having no more sea ice means that the buffer is gone. In the past, thick sea ice extended meters below the sea surface, in many parts of the Arctic Ocean. Melting of this ice into water did consume massive amounts of ocean heat. As such, thick sea ice acted as a buffer. Over the years, Arctic sea ice has become thinner and thinner, as illustrated by the image below.

[ click on image to enlarge ]
Over the past few years, trends have been pointing at zero thickness soon, i.e. in a matter of years. Added below is a trend produced by Arctische Pinguin, pointing at zero volume sea ice in the year 2021.
[ click on image to enlarge ]
Note that there is some variability from year to year. This indicates that a Blue Ocean Event may well happen earlier than the trend, e.g. in September 2017. The image further shows that there's hardly any buffer left, the buffer is virtually gone!

This buffer used to consume massive amounts of ocean heat that is carried along sea currents into the Arctic Ocean. Once the sea ice is gone, that heat must go somewhere else. A huge amount of energy used to be absorbed by this buffer, i.e. by melting ice and transforming it into water. The energy that used to be absorbed by melting ice is as much as it takes to warm up an equivalent mass of water from zero °C to 80 °C. Much of this heat will then suddenly speed up warming of the water of the Arctic Ocean, rather than going into melting the ice as it did previously. So, the water of the Arctic Ocean will suddenly warm up dramatically. Remember that the Arctic Ocean in many areas is very shallow, in many places it's less than 50 m deep, as discussed in an earlier post.

The Buffer has gone, feedback #14 on the Feedbacks page
The danger is that this extra heat will reach the seafloor and destabilize methane hydrates that are contained in sediments at the bottom of the Arctic Ocean. This could result in huge methane eruptions. It is hard for methane plumes to get broken down in the water, given the abrupt and concentrated nature of such releases and given that the Arctic Ocean is in so many places very shallow. Once that methane enters the atmosphere, it will strongly contribute to further warming of the atmosphere over the Arctic.


In conclusion, disappearance of the sea ice would mean that the buffer has gone. This further increases the danger of huge abrupt releases of methane from the seafloor of the Arctic Ocean. In many respects, the danger is such that we can just count ourselves lucky that such huge releases haven't occurred yet.

In response to this danger, comprehensive and effective action is needed, along multiple lines of action, each implemented in parallel and simultaneously. While local feebates are typically the most effective policies, local communities can each decide what works best for them, provided that agreed targets are met, and such targets will need to be a lot stronger and more comprehensive than the aspirational emission reductions that countries have submitted as part of the Paris Agreement.

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



Above post was also read by David Petraitis as part of the podcast by Wolfgang Werminghausen



Extreme Weather Events

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Sea ice close to the North Pole looks slushy and fractured into small pieces. The image below shows the situation on July 8, 2016.

Sea ice north of the geographic North Pole. For more on the (geo)magnetic North Pole, see this page. 
For reference, the bars at the bottom right show distances of 20 km and 20 miles. By comparison, sea ice in the same area did develop large cracks in 2012, but even in September 13, 2012, it was not broken up into small pieces, as shown by this image at a recent post.


As shown by above image, by Jim Pettit, Arctic sea ice volume has been in decline for decades. While this may look like a steady decline, chances are that the sea ice will abruptly collapse over the next two months, for the reasons described below.

The animation below, from the Naval Research Laboratory, shows Arctic sea ice thickness for 30 days up through July 8, 2016, including a forecast of 7 days.

Below is a new Naval Research Laboratory image, dated July 4, 2016
and contributed by Albert Kallio with the following description.


NORTH POLE SEA ICE DISAPPEARING VERY RAPIDLY 4.7.2016

Albert Kallio: The upgraded US Navy sea ice thickness system revealed extreme rates of sea ice pulverization and melting on 4.7.2016 which justifies a continued close attention to the developments on the Arctic Ocean. Due to virtually continuous storm centering the North Pole for weeks now, warm water upswells and sea water mixing drives base melting of icefloes besides wave actions that both wash and pulverize broken sea ice. The more pulverized sea ice becomes, the greater its 3-dimensional surface area that sits in water becomes, this easing transfer of heat from ocean to sea ice. In addition, honeycombing of ice also flushes ice with water in a stormy weather. The final factor being that most of sea ice is very recent (seasonal) ice that contain residues of salts, when saline brine is expelled this creates boreholes into ice making it "rotten ice" easily.
https://www7320.nrlssc.navy.mil/GLBhycomcice-12/navo/arcticictn_nowcast_anim30d.gif
Sea ice decline reflects the extra energy added to the Arctic, as global warming and feedbacks are hitting the Arctic particularly strongly. Three of these feedbacks are depicted in the image on the right.

As the sea ice melts, sea surface temperatures will remain at around zero degree Celsius (32°F) for as long as there is ice in the water, since the extra energy will first go into melting the ice. Only after the ice has melted will the extra energy start raising the temperature of the water.

Sea ice thus acts as a buffer that absorbs heat, preventing sea surface temperature from rising. As
sea ice is busy melting, each gram of ice takes 334 Joule of heat to change into water, while the temperature remains steady at 0°C ( 32°F).

Once all ice has turned into water, all further heat goes into raising the temperature of the water. To raise the temperature of each gram of water by one degree Celsius then takes only 4.18 Joule of heat.

In other words, melting of the ice absorbs 8 times as much heat as it takes to warm up the same mass of water from zero to 10°C. As sea ice disappears, extra energy instead goes into raising the temperature of the water, as depicted in the image on the right, and as further described at the feedbacks page as feedback #14.

Sea ice can reflect as much as 90% of the sunlight back into space. Once the ice has melted away, the water of the ocean reflects only 6% of the incoming solar radiation and absorbs the rest. Albedo change is depicted in above image as feedback #1. As Professor Peter Wadhams once calculated, warming due to Arctic snow and ice loss could more than double the net warming now caused by all emissions by all people of the world.

Professor Peter Wadhams on albedo changes in the Arctic, image from Edge of Extinction
Once the sea ice has disappeared, a lot more energy will get absorbed by the Arctic Ocean, i.e. energy that was previously reflected back into space and energy that previously went into changing ice into water.

Furthermore, as the sea ice disappears, chances increase that storms will develop that come with rain and winds that can batter and push the remaining sea ice out of the Arctic Ocean, while storms can also increase the amount of water vapor in the atmosphere and the occurrence of cirrus clouds that can trap heat.

Methane is a further feedback, depicted as feedback #2 in the image further above. As the water of the Arctic Ocean gets warmer, the danger increases that heat will reach hydrates at the seafloor and that this will trigger release of huge amounts of methane, in an additional self-reinforcing feedback loop that will make warming in the Arctic accelerate further and that threatens to escalate into a third kind of warming, i.e. runaway warming. Peter Wadhams co-authored a study that calculated that methane release from the seafloor of the Arctic Ocean could yield 0.6°C warming of the planet in 5 years (see video at earlier post).


As above image shows, methane on July 8, 2016, reached levels as high as 2655 ppb. Such high levels typically occur due to methane hydrates getting destabilized. As the sea ice disappears, the situation could get worse rapidly, as illustrated by the images below.

July 5, 2016, sea surface was as warm as 17.1°C / 62.7°F at green circle, i.e. 13.7°C / 24.7°F warmer than 1981-2011. 
These high sea surface temperature anomalies are the result of warmer water getting carried by the Gulf Stream below the sea surface of the Atlantic Ocean into the Arctic Ocean. The water carried into the Arctic Ocean is both warmer and saltier than the water at the surface, as the fresh cold meltwater forms a lid at the surface. At areas around Svalbard where the sea is rather shallow, the warmer water comes to the surface. These high anomalies thus indicate how much warmer the water now is that is entering the Arctic Ocean, as discussed in earlier posts such as this one.
image from previous post
The rapid recent rise in ocean heat is illustrated by above image, showing that oceans on the Northern Hemisphere in May 2015 through April 2016 were 0.93°C warmer than the 20th century average, whereas for the equivalent 2012 period the anomaly was merely 0.46°C. In other words, there now is more ocean heat, making the possibility of methane hydrates destabilization more threatening.

Meanwhile, the speed at which the Arctic is warming is changing the jet streams, as discussed by Paul Beckwith in the video below, following Paul's earlier video that's included in an earlier post.



There are many indications that changes to the climate are accelerating, causing extreme weather events to hit with increasing strength and intensity. Water vapor is a potent greenhouse gas and for each degree Celsius that temperatures rise, the atmosphere can hold 7% more water vapor, which will also lead to stronger storms such as cyclones. On the image below, typhoon Nepartak is approaching Taiwan, with wind speed as high as 103 mph or 165 km/h, and with cloud water as much as 9 kg per square m on July 7, 2016.

Nepartak approaching Taiwan on July 7, 2016, with wind speed as high as 103 mph or 165 km/h (left panel), and with cloud water as much as 9 kg per square m (right panel)
NASA image
According to NASA, very powerful storms near the center of Nepartak's circulation were found to be dropping rain at a rate of over 193 mm (7.6 inches) per hour. Tall thunderstorms called "hot towers" were found to reach heights of 17.0 km (about 10.5 miles).

The image on the right shows a thermal image of Typhoon Nepartak on July 7 at 17:45 UTC. The colder the cloud tops, the higher they are in the troposphere and the stronger the storms.

On July 7, 2016, at 1500 UTC, Nepartak's maximum sustained winds had reached 150 knots (172.6 mph/ 277.8 kph), generating waves as high as 48 feet (14.6 meters).

Strong storms can bring water vapor high up into the stratosphere, contributing to the formation of cirrus clouds that trap a lot of heat that would otherwise be radiated away, from Earth into space.

Altogether, the combined global temperature rise due to global warming and feedbacks could exceed 10°C or 18°F within a decade, as discussed in previous posts such as this one.

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


Links

- The North Geographic Pole, the North Magnetic Pole and the North Geomagnetic Pole
http://wdc.kugi.kyoto-u.ac.jp/poles/polesexp.html

- Three Kinds of Warming in the Arctic
http://arctic-news.blogspot.com/2016/02/three-kinds-of-warming-in-arctic.html

- NASA: Napartak (July 9, 2016)
https://www.nasa.gov/feature/goddard/2016/napartak-nw-pacific-ocean

- Jim Pettit Climate Graphs
http://iwantsomeproof.com/3d/siv-ds-weekly-3d.asp


Arctic Sea Ice 2015 - Update 10

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It looks like sea ice has passed its minimum extent for the year 2015, as illustrated by the image below.


There are some differences between the various websites measuring extent, such as to whether the 2015 low was the third or fourth lowest. Japanese measurements show that sea ice extent was 4.26 million square km on September 14, 2015, i.e. lower than the 2011 minimum of 4.27 million square km, as illustrated by the image below.


Meanwhile, the Polar Science Center at the University of Washington has announced that Arctic sea ice volume minimum was reached on September 12, 2015, with a total volume of 5,670 cubic km. The image below shows a polynomial trendline based on their annual Arctic sea ice volume minima, including this volume for 2015.


Importantly, the sea ice in many places is now less thick than it was in 2012, as illustrated by the image below, showing sea ice thickness on September 27, 2012 (panel left) and a forecast for September 27, 2015 (panel right).


The reason for the dramatic decrease in thickness of the multi-year sea ice is ocean heat, as illustrated by the image below, showing sea surface temperature anomalies in the Arctic as at September 21, 2015.


The water of the Arctic Ocean is very warm, not only at the surface, but even more so underneath the surface. What has contributed to this situation is described by the image below. From 2012, huge amounts of fresh water have run off Greenland, with the accumulated fresh water now covering a huge part of the North Atlantic.

Since it's fresh water that is now covering a large part of the surface of the North Atlantic, it will not easily sink in the very salty water that was already there. The water in the North Atlantic was very salty due to the high evaporation, which was in turn due to high temperatures and strong winds and currents. As said, fresh water tends to stay on top of more salty water, even though the temperature of the fresh water is low, which makes this water more dense. The result of this stratification is less evaporation in the North Atlantic, and less transfer of ocean heat to the atmosphere, and thus lower air temperatures than would have been the case without this colder surface water.


Meanwhile, global warming continues to heat up the oceans, while less of this ocean heat can now be transferred from the water to the atmosphere in the North Atlantic, since the fresh water is acting like a lid.

The danger is thus that warmer water will be pushed into the Arctic Ocean at lower depth, and that it will reach the seafloor of the Arctic Ocean where huge amounts of methane are contained in sediments. Ice acts like a glue, holding these sediments together and preventing destabilization of methane hydrates. Warmer water reaching these sediments can penetrate them by traveling down cracks and fractures in the sediments, and reach the hydrates.

The big melt in Greenland and the Arctic in general is causing further problems. Isostatic adjustment following melting can contribute to seismic events such as earthquakes, shockwaves and landslides that can destabilize methane hydrates contained in sediments on the Arctic Ocean seafloor.

In the video below, by Nick Breeze, Professor Peter Wadhams discusses the situation.



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


The water of the Arctic Ocean is very warm, not only at the surface, but even more so underneath the surface. What has...
Posted by Sam Carana on Tuesday, September 22, 2015

Arctic Sea Ice Collapse Threatens - Update 9

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The image below shows that Arctic sea ice had reached a level of 4.45 million square kilometers on September 16, 2015 (end of dark blue line at center of image).


NSIDC has meanwhile called the 2015 minimum, but the first sentence of their post hastens to add that on September 11, Arctic sea ice reached its likely minimum for 2015,  at 4.41 million square kilometers (1.70 million square miles), putting 2015 in the fourth lowest place since satellite records began. Arctic sea ice minimum was lower only in 2012 (dotted line), 2007 (light blue line) and 2011 (orange line). Sea ice extent was 4.413 million square kilometers both on September 9, 2015, as well as on September 10 and 11, 2015.

September 9 would be early for the sea ice to reach its minimum, as a comparison with earlier years on above image illustrates. The dark blue line on above image shows that sea ice extent fell slightly on September 16, compared to the day before, and is now below the 2011 extent (orange line) for this time of the year. Over the next few days, sea ice extent may well fall somewhat further, and reach a level below the 2011 minimum, thus reaching the third lowest minimum extent since record began. This could eventuate due to winds compacting the sea ice.

More importantly, sea ice thickness is still falling, as illustrated by the image below showing the sea ice thickness on September 9 in the left panel and a forecast for thickness on September 24 in the right panel.


The image below compares sea ice thickness between September 24, 2012 (left panel) with that forecast for September 24, 2015 (right panel).


Above image illustrates why the situation in 2015 is even more threatening than it was in 2012. Only the ice that is colored light green, yellow and red is more than 3 meters thick. In 2015, ocean heat has been melting the sea ice from underneath. So, even while the currently lower temperatures of the air may have resulted in a slight increase in extent over the past week, the added ice is very thin. Ocean heat first of all goes into melting the thickest sea ice, i.e. the parts that are meters below the surface. This because the water at surface level is colder than the water underneath the surface. This explains why much of the water surface will remain covered by (very thin) ice as air temperatures are now falling (compared to air temperatures over the past few months).

The image below shows sea surface temperatures as at September 17, 2015.


In conclusion, while the sea ice appears to have survived the 2015 melting season without collapsing, the threat that this will occur in the coming years is ominous. Lack of multi-year sea ice makes that sea ice is in a very vulnerable situation. Total collapse of sea ice is therefore more likely to happen in the coming years. Every time ocean heat will arrive in the Arctic Ocean at its fullest strength in future, this heat will no longer be able to be fully absorbed by the process of melting thick sea ice, so what's left of the sea ice will melt very quickly.

There is a strengthening El Niño, while more open water increases the chance that storms will develop that will push the last remnants of the sea ice out of the Arctic Ocean, as discussed in earlier posts such as this one. Storms can also mix warm surface waters all the way down to the seafloor, as discussed in this earlier post. Cyclones that emerge with greater force due to high sea surface temperatures further increase this danger.

The big danger is that ocean heat will cause methane contained in sediments on the Arctic Ocean seafloor to be released abruptly in large quantities, triggering further methane releases spiraling into runaway warming.

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


Below is a text-only version of this post for radio.




Sea ice thickness on September 24, 2012 (left panel) compared to a forecast for September 24, 2015 (right panel). This...
Posted by Sam Carana on Friday, September 18, 2015

Arctic Sea Ice Collapse Threatens - Update 2

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The image below shows sea surface temperature anomalies in the Arctic on July 30, 2015.


Due to warm ocean waters and to heatwaves on land that extended over the Arctic Ocean, while warming up rivers ending into the Arctic Ocean, the sea ice has taken a battering over the past few weeks, as illustrated by the images below.


Above image shows the last bit of thick (5 m) sea ice in the Canadian Archipelago, which became dislodged on July 8, 2015. It looks set to be virtually gone by August 7, 2015, according to the 30-day Naval Research Laboratory animation below, and as also discussed in greater detail in a recent post.


The situation at the north-eastern tip of Greenland doesn't look much better, as illustrated by the image below.


The comparison image below also shows the north-eastern tip of Greenland on July 5, 2015 (top), and on July 31, 2015 (bottom). The bottom image shows water in many places, pushing the last pieces of thick ice into the Wandel Sea and Fram Strait .

[ click on images to enlarge ]
Until now, the thicker multi-year sea ice used to survive the melting season, giving the sea ice strength for the next year, by acting as a buffer to absorb heat that would otherwise melt away the thinner ice. Without multi-year sea ice, the Arctic will be in a bad shape in coming years. 

[ click on images to enlarge ]
What caused the dramatic melting of this thick ice? The left panel of above image shows temperatures. On July 29, 2015, temperatures as high as 23.1°C (or 73,7°F) were recorded on the north coast of Victoria Island, in the Canadian Archipelago (green circle where the arrow points at). The satellite image on the right, captured that same day, shows that hardly any ice was left in the waters surrounding the area.


So, will the sea ice collapse this year? Consider the following four points:

Volume - The image on the top right shows sea ice volume as calculated by PIOMAS at the University of Washington. It shows that in June, volume was less than 2015 in only four years, i.e. 2010 through to 2013. The situation has deteriorated much in July 2015, and looks set to deteriorate even further.

Thickness - Volume is calculated by looking at both thickness and extent. Thickness is looking much worse than it did in the years 2012 through to 2014, as illustrated by above image.

In my experience, sea ice thickness hasn't looked this bad for this time of the year since records began, especially when taking the loss of multi-year ice into account, as also illustrated by the full-width above image.


Extent - Sea ice extent on July 31 was only outside the 2 standard deviations (shaded area) in the years 2007, 2011 and 2012, as illustrated by the image mid right. The dark blue line marks the 2015 extent, with the dot indicating extent on July 31, 2015.

Area - Similarly, Arctic sea ice area is illustrated by the image on the right. For a description of the difference between extent and area, view this NSIDC FAQ page. The bottom right image marks Arctic sea ice area as on July 30, 2015. The yellow marker indicates the situation for the year 2015 on this date. The only years with less sea ice area at this time of the year were 2007, 2011 and 2012.

Also consider that 2015 features very high sea surface temperatures and an El Niño that is still gaining in strength. Thick sea ice appears to be shattered, as illustrated by the satellite images. In conclusion, sea ice looks set to take a further battering over the next few weeks and could end
up at a record low thickness, extent, area and volume around half September 2015.

With that in mind, let's take a look at the image below.


Above image shows a trendline (shaded area) based on satellite data from 1979-2014, with annual minimum volume figures calculated by PIOMAS. The shaded area points at a total disappearance of the sea ice as early as September 2018. The width of the shaded area reflects natural variability, but natural variability could be wider than that, as illustrated by the fact that minimum volume in the years 2007, 2010, 2011 and 2012 was lower than the shaded area. In other words, disappearance of the sea ice could occur even earlier than September 2018 and if things get really bad, collapse could even occur as early as September this year.

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



Will the sea ice collapse this year? Firstly, consider that sea ice volume now hasn't been this bad for any day in July...
Posted by Sam Carana on Friday, July 31, 2015

Arctic Sea Ice Collapse Threatens - Update 1

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The image below compares the Arctic sea ice thickness (in m) on July 15, for the years from 2012 (left panel) to 2015 (right panel), using Naval Research Laboratory images.

Click on image to enlarge
The image below compares the Arctic sea ice concentration (in %) on July 18, for the years from 2012 (left panel) to 2015 (right panel), using Naval Research Laboratory images.


Above images show the dramatic decline of the sea ice in 2015, both in thickness and in concentration.

In terms of thickness, sea ice has been reduced by more than one meter in many places, such as north of Greenland and the Canadian Archipelago, all in the time span of just one month.

The dramatic fall in sea ice concentration also becomes apparent when comparing recent sea ice concentration (July 18, 2015, above right) with sea ice concentration back in May 2015 (image right, May 1, 2015).

This dramatic decline of the sea ice in 2015 is the result of a combination of factors, including:

  1. High levels of greenhouse gases over the Arctic Ocean, as illustrated by the image below, showing that on July 17, 2015 (pm), levels as high as 2512 parts per billion were recorded at 6,041 m (19,820 ft) altitude, while mean methane levels were 1830 parts per billion at this altitude.
  2. High levels of ocean heat, as illustrated by the image below showing high sea surface temperatures off the east coast of North America; much of this ocean heat will be carried by the Gulf Stream into the Arctic Ocean over the next few months.
  3. High air temperatures over North America and Siberia extending over the Arctic Ocean, as illustrated by the image below showing a temperature of 23.1°C (73.7°F), recorded on July 19, 2015, at Banks Island, in the Canadian Archipelago (green circle).
  4. Wildfires triggered by these heatwaves resulting in darkening compounds settling on snow and ice, as illustrated by the image below showing smoke covering a wide area on July 19, 2015, from the east Siberia over North America to the southern tip of Greenland.
  5. Very warm river water running into the Arctic Ocean, as illustrated by the image below, showing sea surface temperatures as high as 19°C (66.2°F) off the coast of Alaska on July 12-15, 2015.
The image below shows the already very high sea surface temperature anomalies as at July 18, 2015.

The Climate Reanalyzer image below shows the high sea surface temperature anomalies in the Pacific Ocean, and where water enter the Arctic Ocean through the Bering Strait, on July 19, 2015.



With still two months of melting to go before the sea ice can be expected to reach its minimum for 2015, the threat of sea ice collapse is ominous. The Arctic-News Blog has been warning for years about the growing chance of a collapse of the sea ice, in which case huge amounts of sunlight that previously were reflected back into space, as well as heat that previously went into melting the ice, will then instead have to be absorbed by the water, resulting in a dramatic rise of sea surface temperatures.

More open water will then come with an increased chance of storms that can cause high sea surface temperatures to be mixed down all the way to seafloor of the Arctic Ocean, which in many cases is less than 50 m (164 ft) deep. This is the case for the East Siberian Arctic Shelf, where experts estimate that huge amounts of methane are contained in subsea sediments. Already now, sea surface temperatures as high as 10°C (~50°F) are recorded there, as illustrated by the image below.


Massive amounts of ocean heat will be carried by the Gulf Stream into the Arctic Ocean over the next few months. The combined result of high sea surface temperatures being mixed down to the seafloor and the ocean heat entering the Arctic Ocean from the Atlantic and Pacific Oceans can be expected to result in dramatic methane eruptions from the Arctic Ocean seafloor by October 2015.

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



Arctic sea ice thickness on July 15, compared over the years 2012 through to 2015. Already virtually all the thick sea...

Posted by Sam Carana on Thursday, July 16, 2015