Tuesday, December 31, 2013

The Biggest Story of 2013

While the world chose to turn a blind eye, the biggest story of 2013 is the methane over the Arctic. As the year progressed, huge quantities of methane started to be released from the seabed of the Arctic Ocean.

Biggest story of 2013: Huge methane releases from the seafloor of the Arctic Ocean
Very high concentrations of methane have been recorded over the Arctic Ocean over the year and the high releases are still continuing (a peak of 2399 ppb was reached on December 29, 2013, p.m.). The methane appears to originate particularly from areas along the Gakkel Ridge fault line that continues as the Laptev Sea Ridge, as discussed in earlier posts.

The Naval Research Laboratory animation below shows that sea ice extent is growing and that thinner sea ice is getting thicker, which is normal for this time of year. At the same time, the multi-meters thick ice is not increasing in extent nor in thickness. In fact, much multi-meters thick sea ice is being pushed out of the Arctic Ocean. Methane looks to be moving underneath the sea ice along exit currents and entering the atmosphere at the edges of the sea ice, where the sea ice is fractured or thin enough to allow methane to rise.



What is causing the release of this much methane?

To answer this question, let's first examine why the Arctic is warming up more rapidly than other places.

Emissions are causing albedo changes in the Arctic, while emissions from North America are - due to the Coriolis effect - moving over areas off the North American coast in the path of the Gulf Stream (see animation on the right).

These impacts constitute a second kind of warming that is hitting the Arctic particularly hard, on top of global warming.

In addition, there are feedbacks that are further accelerating warming of the Arctic, in particular:
  • Snow and ice decline is causing more sunlight to be absorbed in the Arctic (feedback #1).
  • As warming in the Arctic accelerates, a weaker Jet Stream lets warmer air move from lower latitudes into the Arctic (feedback #10).
  • A weaker Jet Stream further elevates the chance of heat waves warming up the Gulf Stream and warming up rivers that end in the Arctic Ocean (feedback #11). This feedback looks to have caused a lot of seabed warming and subsequent methane releases from the sea floor of the Arctic Ocean.  
  • The high methane concentrations are in turn further warming up the air over the Arctic (feedback #2). 
The above is depicted in the diagram below.


The diagram below shows thirteen feedbacks that are accelerating warming in the Arctic.

Hover over each kind of warming and feedback to view more details, click to go to page with further background 
Image Mapemissions cause global warmingArctic warming accelerated by soot, etc.additional warming of Gulf Stream by emissions methane releases escalatePolar vortex and jet stream weaken as Arctic warmssnow and ice decline causing less sunlight to be reflected back into spacemethane releases warm Arctic airas sea ice decline weakens vertical currents, seabed warmsStorms cause vertical mixing of wateraccelerated Arctic warming causes storms that push cold air of the Arcticextreme weather causing storms that push away sea iceextreme weather causing storms that create higher waves, breaking up the sea icestorms creating more wavy waters that absorb more sunlightextreme weather causing fires, etc.weaker polar vortex and jet stream let cold air move out of Arcticextreme weather causing warmer waterssnow and ice decline cause seismic activity that destabilizes hydratesmethane releases prevent sea ice from forming
The image below shows that global warming is hitting the polar regions particularly hard. In a large area of the Arctic Ocean, surface temperature anomalies of more than 2.5 degrees Celsius were recorded during the year 2013.


Importantly, on specific days anomalies did reach much higher values. The image below shows how a large area of the Arctic was exposed to 20+ degrees Celsius surface temperature anomalies recently.

[ click on image to enlarge ]
The NOAA map below shows where sea surface temperatures in August 2013 were warmer (red) or cooler (blue) than the 1982-2006 average.


By September 2013, surface waters around the Barents Sea Opening were about 5°F (3°C) warmer than they were in 2012. Southern Barents Sea temperatures reached 52°F (11°C), which is 9°F (5°C) warmer than the 1977-2006 average. Warm water from rivers flowing into the Arctic Ocean was highlighted in the earlier post Arctic Ocean is turning red.

The danger is that an ever warmer seabed will result in release of ever larger quantities of methane, escalating into runaway global warming.

What makes this story even bigger is that the media have largely chosen to ignore the threat that methane releases from the Arctic Ocean will escalate into to runaway global warming.

While one can read many stories in the media that global warming was supposed to somehow have 'halted', little attention was given to a recent study that points out that the commonly-used United Kingdom temperature record is actually biased and underestimates warming in certain regions, in particular the Arctic.

And while the IPCC points out that most of the additional heat associated with global warming goes into oceans (image right), the IPCC fails to highlight the vulnerability of the Arctic Ocean.

Indeed, perhaps the biggest story of the year is the question why the IPCC has decided not to warn people about the looming Arctic methane threat, ignoring the need for comprehensive and effective action such as discussed at the Climate Plan Blog.


Related

- Ocean heat: Four Hiroshima bombs a second: how we imagine climate change

- (Three kinds of) Warming in the Arctic

Feedbacks
  1. Albedo: snow and ice decline causing less sunlight to be reflected back into space
    http://arctic-news.blogspot.com/2012/07/albedo-change-in-arctic.html
  2. Methane releases warm Arctic air
    http://arctic-news.blogspot.com/2013/11/methane-levels-going-through-the-roof.html
  3. As sea ice decline weakens vertical currents, seabed warms
    http://arctic-news.blogspot.com/2012/09/arctic-sea-ice-loss-is-effectively-doubling-mankinds-contribution-to-global-warming.html
  4. Storms cause vertical mixing of water
    http://arctic-news.blogspot.com/2012/07/arctic-waters-are-heating-up.html
  5. Accelerated Arctic warming causes storms that push cold air of the Arctic
    http://arctic-news.blogspot.com/2012/08/diagram-of-doom.html
  6. Extreme weather causing storms that push away sea ice
    http://arctic-news.blogspot.com/2012/04/supplementary-evidence-by-prof-peter.html
  7. Extreme weather causing storms that create higher waves, breaking up the sea ice
    http://arctic-news.blogspot.com/2012/08/huge-cyclone-batters-arctic-sea-ice.html
  8. Storms creating more wavy waters that absorb more sunlight
    http://arctic-news.blogspot.com/2012/08/diagram-of-doom.html
  9. Extreme weather causing fires, etc." title="extreme weather causing fires, etc.
    http://arctic-news.blogspot.com/2012/07/how-extreme-will-it-get.html
  10. Weaker polar vortex and jet stream let cold air move out of Arctic
    http://arctic-news.blogspot.com/2012/08/opening-further-doorways-to-doom.html
  11. Extreme weather causing warmer waters
    http://arctic-news.blogspot.com/2013/12/the-biggest-story-of-2013.html
  12. Snow and ice decline cause seismic activity that destabilizes hydrates
    http://arctic-news.blogspot.com/2013/09/methane-release-caused-by-earthquakes.html
  13. Methane releases prevent sea ice from forming
    http://arctic-news.blogspot.com/2013/12/methane-emerges-from-warmer-areas.html


Friday, December 27, 2013

New Year's Eve Treats: Salmon with Crispy Skin and Buckaroo Cookies

Where does time go? Last I looked, it was almost Thanksgiving. Now it's almost New Year's Eve. 2013 was a good year. Wishing everyone a great 2014.

On New Year's Eve we're having friends over for a late dinner and an evening of movie watching. We've seen most of the movies in Oscar contention and we have our favorites (HerNebraska Philomena and Fruitvale Station). But we have more to watch so we'll enjoy the evening with food and films.

Two of the treats I'll make include holiday cookies and salmon filet with crispy skin.  A few months ago for my oldest son's birthday party, we had a dinner at Napa Valley Grille in Westwood. Franklin likes farm fresh food, simply prepared, not fussy. We sampled the menu and the food was delicious. The chef stopped by to see if everyone was happy. A friendly, nice guy, chef Taylor Boudreaux sent out a pasta dish with truffles as a gift to the table. What a nice thing to do.
One of the dishes we had at the dinner was  a salmon filet with crispy skin. It's a simple dish but I've never been able to get the skin right at home. Chef Boudreaux agreed to do a video demonstration.
The interview and video are on Zester Daily. He makes it look so easy. He shared the magic. I tried it at home. It worked! So cool.

Chef's Secret To Crispy Skin For Pan-Seared Salmon Filets

Alana Vague, a friend of a friend, was baking cookies as holiday gifts. She put them in little brown paper bags, nicely tied with a ribbon.  They are delicious and Alana says they're easy to make, a recipe from her great-grandmother. They'll be perfect to snack on while we're watching movies.

Alana's Great-Grandmother's Buckaroo Cookies
Yield: a lot

Ingredients

1 1/4 cups all-purpose flour
1 tsp baking soda
1/2 tsp salt
1/2 tsp cinnamon
1 cup butter, softened
3/4 cup sugar
3/4 cup brown sugar
2 eggs
1 tsp vanilla
3 cups quick oats
1 cup butterscotch chips
2/3 cup chocolate chips

Directions

Cream butter and sugars
Add eggs and vanilla
Add dry ingredients
Stir in oats and chips
Drop by tablespoon on cookie sheet
Bake at 375 degrees for 7-9 minutes
(I bake them for 7ish then let them rest on the cookie sheet for 5 minutes or so)

Thursday, December 26, 2013

Sea Ice in decline between Svalbard and Greenland

[ click on image to enlarge ]
Above image shows that Earth's highest atmospheric methane concentrations are recorded over the Arctic Ocean. The insets show lower methane concentrations over various continents, North and South America (top left), Europe (mid right), Australia bottom left) and Antarctica (bottom right).

The top right inset shows sea ice thickness, illustrating that methane is escaping from the sea floor of the Arctic Ocean and is transported by currents to the thinner edges of the sea ice, where it is entering the atmosphere.

As discussed in a recent post, methane can be bubbling up in the Arctic Ocean with a force strong enough to prevent sea ice from forming in the area. This feedback is depicted in the Diagram of Doom further below as feedback #13.


Around this time of year, Arctic sea ice is typically growing rapidly, both in extent and thickness.

However, the above image shows that in the area marked by the white circle, between Svalbard and Greenland, the sea ice is actually in decline.

[ click on image to enlarge ]
This decline is caused by methane that is entering the atmosphere in the area as warmer water continues to be transported by the Gulf Stream into the Arctic Ocean, as discussed in previous posts such as this one, and as also illustrated by the image on the right.

Warmer than average waters have been entering the Arctic Ocean along the Gulf Stream since July 2013, when changes to the Jet Stream contributed to waters off the North American coast reaching record warmest temperatures, as depicted in the Diagram of Doom below as feedback #11.

In summary, the above images show that methane makes it hard for ice to form, while the warm water of the West Spitzbergen Current is pushing the ice away, breaking up even the thickest ice to the north of Greenland.

Surface temperatures in the area have been extremely high recently. This part of the Arctic Ocean was hit by an 18+°C anomaly during the week from December 16 to December 22, 2013, as illustrated by the image below.


On some days that week, anomalies of 20+°C were recorded over an even larger part of the Arctic Ocean, as described in a previous post. These anomalies show how a number of feedbacks can interact and contribute to huge warming peaks in the Arctic Ocean, such as methane releases (feedbacks #2 and #13 in the diagram below) and changes to the Jet Stream (feedbacks #10 and #11 in the diagram below).

This spells bad news for the sea ice. Some people may have hoped that the thicker sea ice north of Greenland would take decades to disappear. However, as depicted in the Diagram of Doom below, feedbacks can hugely accelerate sea ice decline. As sea ice declines further, more open water make it more likely that stronger storms and cyclones will appear that can rip the sea ice apart and move the pieces into the Atlantic Ocean in a matter of days.

The image below, by Jim Pettit, illustrates the ongoing decline of the sea ice.


Thirteen feedbacks that can accelerate warming in the Arctic are depicted in the diagram below.


Specific feedbacks are described in the following posts:
- Diagram of Doom
- Further feedbacks of sea ice decline in the Arctic
- Causes of high methane levels over Arctic Ocean
- Methane Release caused by Earthquakes
- How Do We Act in the Face of Climate Chaos?
- The astounding global warming impact on our oceans . . .
- Methane emerges from warmer areas
Feedbacks are pictured in a more general way in the image below.


Above image shows how the accumulation of the many feedbacks and their interaction leads to ever stronger albedo changes, while the resulting accelerated warming in the Arctic causes increasing quantities of methane to be released from the seafloor of the Arctic Ocean, in turn leading to runaway global warming, as also pictured in the image below.

[ click on image to enlarge ]
As above image shows, a polynomial trendline already points at global temperature anomalies of 5°C by 2060. Even worse, a polynomial trendline for the Arctic shows temperature anomalies of 4°C by 2020, 7°C by 2030 and 11°C by 2040, threatening to cause major feedbacks to kick in, including albedo changes and methane releases that will trigger runaway global warming that looks set to eventually catch up with accelerated warming in the Arctic and result in global temperature anomalies of 20°C+ by 2050.

To reduce these risks, comprehensive and effective action is needed, such as described at the Climate Plan blog.

Saturday, December 21, 2013

Act now on methane

by Malcolm Light

  This is an extract. The full paper including figures and tables is at:  
https://sites.google.com/site/runawayglobalwarming

Methane concentrations in the Arctic are higher than elsewhere in the world, as shown on figure 1. below (NASA image).


Methane is entering the atmosphere at high latitudes and spreading across the globe from there.


What is causing methane to be released in large quantities in the Arctic?

The Gulf Stream, pictured on figure 3. below, is warming up more than usual due to global warming. Specifically, pollution clouds pouring eastwards from the coast of Canada and the United States are the main culprit in heating up the Gulf Stream.

Figure 3. The Gulf Stream
In July 2013, water off the coast of North America reached 'Record Warmest' temperatures and proceeded to travel along the Gulf Stream to the Arctic Ocean, where it is now warming up the seabed. Figure 4. below further shows that above-average temperatures were recorded in July 2013 along the entire path of the Gulf Stream into the Arctic Ocean. 
Figure 4. NOAA: part of the Atlantic Ocean off the coast of North America reached record warmest temperatures in July 2013
The mean speed of the Gulf Stream is 4 miles per hour (6.4 km/hour or 1.78 metres/second), but the water slows down as it travels north. In the much wider North Atlantic Current, which is its north eastern extension, the current flows 3.5 times slower (about 0.51 metres/second), while the West Spitzbergen Current (WSC on figure 5. below) flows at about 0.35 metres/second (5 times slower).


The West Spitzbergen Current dives under the Arctic ice pack west of Svalbard, continuing as the Yermak Branch (YB on above map) into the Nansen Basin, while the Norwegian Current runs along the southern continental shelf of the Arctic Ocean, its hottest core zone at 300 metres depth destabilizing the methane hydrates en route to where the Eurasian Basin meets the Laptev Sea, a region of extreme methane hydrate destabilization and methane emissions. Figure 6. below, from an earlier post by Malcolm Light, shows how warm water flows into the Arctic Ocean and warms up methane hydrates and free gas held in sediments under the Arctic Ocean.


Sediments underneath the Arctic Ocean hold vast amounts of methane. Just one part of the Arctic Ocean alone, the East Siberian Arctic Shelf (ESAS, see figure 7. below), holds up to 1700 Gt of methane. A sudden release of just 3% of this amount could add over 50 Gt of methane to the atmosphere, and experts consider such an amount to be ready for release at any time.

Figure 7.
As above figure 7. shows, the total methane burden in the atmosphere now is 5 Gt. The 3 Gt that has been added since the 1750s accounts for almost half of all global warming. The amount of carbon stored in hydrates globally was in 1992 estimated to be 10,000 Gt (USGS), while a more recent estimate gives a figure of 63,400 Gt (Klauda & Sandler, 2005). The ESAS alone holds up to 1700 Gt of methane in the form of methane hydrates and free gas contained in sediments, of which 50 Gt is ready for abrupt release at any time, and Whiteman et al. calculate that an extra 50 Gt of methane would cause $60 trillion in damage. By comparison, the size of the world economy in 2012 was about $70 trillion. 

Smaller releases of methane in the Arctic come with the same risk; their huge local warming impact threatens to further destabilize sediments under the Arctic Ocean and trigger further methane releases, as illustrated by figure 8. below.
Figure 8.
Figure 9. below, from an earlier post by Malcolm Light, shows that, besides the shallow methane hydrate regions in the ESAS, the Arctic Ocean slope and deep water regions contain giant volumes of methane hydrate deposits (methane frozen within the ice).
If only a few percent of this methane hydrate becomes destabilized, it will release enough methane into the atmosphere to cause a Permian Age-type massive extinction event. Recent methane emission maps show that, besides the emissions from the ESAS, huge amounts of methane are being released from other parts of the Arctic Ocean.

We now know that the subsea methane hydrate is destabilizing at a fast-increasing pace and the pattern of destabilization indicates that it is mainly caused by the increasingly hot "Gulf Stream" waters entering the Arctic west of Svalbard and through the Barents Sea. These "Gulf Stream" waters do a complete circuit in the Arctic, even under a complete floating ice cover, and will destabilize the methane hydrates they come in contact with before making an exit along the edges of Greenland. Methane is now also emerging from the waters of the Greenland coastline, where the southward-bound "Gulf Stream" waters exit the Arctic Ocean along the edges of Greenland.

Historically, methane has caused delayed temperature anomalies of some 20°C, according to ice core analysis data, i.e. much higher than anomalies caused by carbon dioxide. Methane has a very high warming potential compared to carbon dioxide. Over a decade, methane's global warming potential is more than 100 times as much as carbon dioxide, while methane's local warming potential can be more than 1000 times as much. As a result, giant zones of circulating warm air in the Arctic have temperature anomalies in excess of 20°C.

Figure 10. [ click on image to enlarge ]
These hot clouds, resulting from many feedbacks including this Arctic atmospheric methane build-up, show that methane's delayed temperature anomaly of 20°C has already caught up in the Arctic and is going to progressively spread around the world resulting in runaway global warming.

Figure 11. [ click on image to enlarge ]
Above figure 11. (by Sam Carana) and figure 12. below (by Malcolm Light) indicate that the critical mean atmospheric temperature anomaly of 8°C will be reached between 2035 and 2050. At this temperature we can expect total deglaciation and extinction, according IPCC AR4 (2007).


By 2012, the mean atmospheric temperature had increased by some 0.8°C by human induced global warming. This year however Australia has seen an anomalous 0.22°C temperature increase. The new Australian temperature gradient implies that in ten years the atmosphere will be 2.2°C hotter and in 30 to 40 years, 6.6 to 8.8°C hotter which is consistent with the Arctic methane emission temperature increase curves of Carana and Light.

The reason for this sudden temperature increase in Australia this year is due to the fast building pall of methane in the Northern Hemisphere caused by global warming and destabilization of the subsea Arctic methane hydrates and the Arctic surface methane hydrate permafrosts.

At the moment, the entire Arctic is covered by a widespread methane cloud, but it is very concentrated (> 1950 ppb) over the Eurasian Basin and Laptev Sea where the subsea methane hydrates are being destabilized at increasing rates by heated Atlantic (Gulf Stream) waters. The area of the Eurasian Basin is similar to that of the East Siberian Arctic Shelf (ESAS) where Shakova et al. (1999) have shown that some 50 billion tons of methane could be released at any moment during the next 50 years from destabilization of subsea ESAS methane hydrates.

Figure 13.  Methane over the Arctic Ocean on December 3, 2013        [ click on image to enlarge ]
At the moment, water saturated with methane is traveling underneath the ice carried by exit currents and emerging at locations where the sea ice is still less than one meter thick, such as in Baffin Bay and in Hudson Bay, as also shown on the animation below.

[ this animation is a 1.5MB file and may take some time to fully load ]
This massive volume of methane entering the atmosphere will produce catastrophic consequences for the global climate system. Furthermore global warming is now destabilizing methane hydrates in the Eurasian Basin even more than on the ESAS. The release of an additional 50 billion tons of methane or more from the Eurasian Basin over the next 50 years will further compound the catastrophe represented by the destabilization of methane hydrates on the ESAS. Essentially we have passed the methane hydrate tipping point and are now accelerating into extinction as the methane hydrate "Clathrate Gun" has begun firing increasingly large volleys of methane into the Arctic atmosphere.

The growth of the mean atmospheric temperature using the curves on figure 12 indicate that the mean atmospheric temperature anomaly will exceed 1.5°C in 15 years and 2°C in 20 years, at which time storm systems will be very extreme with droughts, flooding, sea level rise and the loss of Pacific islands. When the mean atmospheric temperature anomaly reaches 8°C some 39 years in the future, there will be total deglaciation and a major extinction event that will culminate in a Permian-type extinction of all life on Earth.

If we do not stop the massive increases of Arctic methane emissions into the atmosphere the oceans will begin to boil off by 2080, when the mean temperature anomaly exceeds 115 to 120°C and the temperatures will be like those on Venus by 2100 (see figure 12).

The present end of the financial crisis and recovery of the U.S. economy will take us down the same fossil fuel driven road to catastrophe that the U.S. has followed before, when they refused to sign the original Kyoto Protocols. Unless the United States and Canada reduce their extreme carbon footprints (per unit population), they will end up being found guilty of ecocide and genocide, as the number of countries destroyed by the catastrophic weather systems continues to increase.

The United States and Canada seek to expand their economies by increasingly frenetic extraction of fossil fuels, using the most environmentally destructive methods possible (fracking and shale oil), while the population's total addiction to inefficient gas transport is leading our planet into suicide. We are like maniacal lemmings leaping to their deaths over a global warming cliff. What a final and futile legacy it will be for the leader of the free world to be remembered only in the log of some passing alien ship recording the loss of the Earth’s atmosphere and hydrosphere after 2080 due to human greed and absolute energy ineptitude.

The U.S. Government and Canada must ban all environmentally destructive methods of fossil fuel extraction such as fracking, extracting shale oil and coal and widespread construction of the now found to be faulty hydrocarbon pipeline systems. All Federal Government subsidies to fossil fuel corporations, for fossil fuel discovery and extraction must be immediately eliminated and the money spent solely on renewable energy development, which will provide many jobs to the unemployed. All long and short range (high consumption) fossil fuel-powered transport must be electrified or converted to hydrogen and where the range is too large, electric vehicles (including electric trains and ships) must be used instead of fossil fuel-powered trucks or aviation means of transport. All the major work for this conversion (including railway construction) can provide a new and growing set of jobs for the unemployed. Nuclear power stations must continue to be used and should be converted to the safe thorium energy system until the transition is complete.

The U.S. has to put itself on a war footing, but rather than fighting other military forces, it should recall its military forces from various places across the world and set them to work on the massive shift to renewable energy that the country needs to undertake if it wishes to survive the fast approaching catastrophe. The threat now comes from Mother Nature, who has infinite power at her disposal and intends to take no prisoners when she will strike back hard over a very short, absolutely brutal, 30-to-40-year period which has already begun. I cannot emphasise more, how serious humanity’s predicament is and what we should try to do to prevent our certain final destruction and extinction in 30 to 40 years if we continue down the present path we are following.

Figure 14. 
Above action plan (figure 14.) includes efforts to move to a sustainable economy (part 1.) and efforts to reflect and divert heat away from the Arctic (part 2.). Furthermore, it includes action on methane escaping from hydrates in the Arctic (part 3.), as described at the Arctic methane management page. Two types of methane management are further discussed below.

Arctic Methane Permanent Storage

In the ANGELS Proposal, subsea Arctic methane is extracted, stored and sold as LNG for distribution as fuel, to produce fertilizer, etc. Permanent storage underground, however, is more preferable.
Figure 15. 
As described by Sam Carana in an earlier post, Prof. Kenneth Yanda, at the University of California, Irvine, has shown that methane can be stored in propane - methane hydrates that are stable at temperatures of ca 15°C and low pressure (25 pounds per square inch - 1.66 atmospheres), very close to the ambient temperature and pressure conditions.

Figure 16. 
Figure 17. Methane capture in zeolite SBN. Blue represents
adsorption sites, which are optimal for methane (CH4)
uptake. Each site is connected to three other sites (yellow
arrow) at optimal interaction distance.  Credit: LLNL News
Hydrates can be produced that contain larger cages for other gases and smaller cages for methane.

Methane can be converted into propane and other gases with UV light and the final goal would be long-term storage of these gases in the form of hydrates in deep waters such as those north of Alaska, suggests Sam Carana, adding that carbon dioxide can also then be sequestered in the hydrates, after its removal from the atmosphere.

Unlike carbon dioxide, methane is completely non-polar and reacts very weakly with most materials.

Three zeolite types (SBN, ZON and FER) have been found to absorb methane at high to moderate rates (Figure 17, from Lawrence Livermore National Laboratory (LLNL) and UC Berkley, 2013).

These materials can help limit escape of fugutive gases from extraction, transport and distribution of methane.

Lucy and Alamo Projects

The Lucy project seeks to decompose methane in the atmosphere.

In a new modified version of the Lucy Project, hydroxyls can also be generated by a polarized 13.56 MHZ beam intersecting the sea surface over the region where a massive methane torch (plume) is entering the atmosphere, so that the additional hydroxyl will react with the rising methane breaking a large part of it down. The polarized 13.56 MHZ radio waves will decompose atmospheric humidity, mist, fog, ocean spray, and the surface of the waves themselves in the Arctic Ocean into nascent hydrogen and hydroxyl (figure 18).

The newly determined atmospheric temperature gradient indicates that the mean global atmospheric temperature will reach 1.5°C in 15 years and 2°C in 20 years (Figure 14). Consequently we only have 15 years to get an efficient methane destruction radio - laser system designed, tested and installed (Lucy and Alamo (HAARP) Projects, figure 18) before the accelerating methane eruptions take us into uncontrollable runaway global warming. This will give a leeway of 5 years before the critical 2°C temperature anomaly will have been exceeded and we will be looking at catastrophic storm systems, a fast rate of sea level rise and coastal zone flooding with its extremely deleterious effects on world populations and global stability.

Figure 18.

Thursday, December 19, 2013

SAVING THE GLOBAL CLIMATE FROM RUNAWAY ARCTIC METHANE RELEASE AND SEA ICE LOSS

=  =  =  STATEMENT FOR IMMEDIATE RELEASE  =  =  =  NEWS RELEASE  =  =  =  DATE: DECEMBER 18, 2013  =  =  =

SAVING THE GLOBAL CLIMATE FROM RUNAWAY ARCTIC METHANE RELEASE AND SEA ICE LOSS

The Greenhouse Gases that human civilisation has emitted have warmed the Arctic more than any other area on Earth.

The reasons for this are well known and will not be repeated here. This has resulted in a loss of sea ice especially in the late summer. More recently still Methane has started to be released from Methane Hydrates especially from the East Siberian Arctic Shelf (ESAS). Emissions of Methane from this area increased from 8 to 17 Tg (teragrams or megaton) between 2009 and 2012 according to research done by Natalia Shakhova and in 2013 appear to be about 22 Tg.
See: arctic-news.blogspot.com/2013/11/quantifying-arctic-methane.html

My understanding is that the climate research organisations broadly accept that Methane emissions from the ESAS have risen substantially in the last few years, as indicated above, and are a serious concern, but they are still small compared to total global emissions of Methane and they do not accept that they will runaway in the near future. This needs examination.



The warming of the Arctic seems likely to lead to the total melting of the Arctic Sea Ice in late summer no later than the summer of 2018 and to massive release of Methane from the melting of Methane Hydrates beneath the ESAS by the same date leading to runaway Global Warming and the end of most life on earth. In 2018, and probably before, the Arctic will be much warmer and the rate of Methane emissions by 2016 will cause alarm worldwide. In 2016 it will probably no longer be possible to prevent a runaway greenhouse event. The problem is that until after a runaway event has started, drastic climate impacts will not occur, so most people will not be alarmed by the situation. Nonetheless, immediate action is essential to cool the arctic.

The reason for this is that the ice is melting earlier in summer than has been the case for several millennia, because of Arctic Warming caused by the increased concentration of Greenhouse Gases in the atmosphere. Methane is still being released in relatively small quantities from Methane Hydrates beneath the ESAS now, but this will accelerate rapidly as Methane concentrations increase in the arctic atmosphere, since they will absorb more sunlight and warm the Arctic, causing further Methane releases.

Arctic Methane Impact
Humanity may be able to prevent this from occurring, if drastic action is taken almost immediately, but if we don’t react then this will very rapidly become a runaway Greenhouse Event and out of our control. We must drastically reduce Greenhouse Gas emissions and take action to cool the arctic.

It is essential that your government responds to this emergency by publicising this worldwide and by trying to obtain a global agreement to drastically reduce global Greenhouse Gas emissions and to cool the Arctic.

John B Davies (personal)

This statement is supported by:
Prof. Peter Wadhams, Sam Carana, Paul Beckwith, Malcolm Light, John Nissen, Albert Kallio
Annie Mond, Carl Vilbrandt,


N.B. The truth of this prognosis should rapidly become apparent by measuring Methane emissions and concentration in the Arctic atmosphere in 2014. Thus very closely measuring arctic Methane emissions and atmospheric concentration is essential in 2014 and thereafter.

If you like to have your name added in support, please comment at the facebook post below.



Sunday, December 15, 2013

Methane emerges from warmer areas

As the year draws to a close, it's time to review where warming has occured most strongly in 2013. Surface temperature anomalies in November 2013 were 0.77°C, the highest global November anomalies on record. In November 2013, high temperature anomalies occurred in the Arctic, well over 9°C north and south of Novaya Zemlya.

Indeed, global warming is hitting the Arctic particularly hard, and some models have underestimated the pace at which this is occuring. Most heat goes into the oceans, which - due to the Gulf Stream - contributes to accelerated warming in the Arctic, where also less monitoring takes place than over land. Stefan Rahmstorf, Co-Chair of Earth System Analysis at the Potsdam Institute for Climate Impact Research, says at RealClimate:
new study by British and Canadian researchers shows that the global temperature rise of the past 15 years has been greatly underestimated. The reason is the data gaps in the weather station network, especially in the Arctic. If you fill these data gaps using satellite measurements, the warming trend is more than doubled in the widely used HadCRUT4 data.
Where did warming occur most strongly in 2013? The red/orange areas on the image below shows surface temperature anomalies of more than 2°C for the year from December 13, 2012, to December 12, 2012.


As the image shows, temperature anomalies have hit Earth most strongly in the cryosphere, i.e.
- in Antarctica, as discussed at this post;
- on the Qinghai-Tibetan Plateau, as earlier discussed at this post;
- in the Arctic, as discussed below.

Over the past 90 days, the Arctic Ocean has shown surface temperature anomalies of over 5°C and in some spots over 8°C.


Looking at anomalies over longer periods can mask the occurrence of much higher anomalies on individual days. As an example, temperature anomalies of over 20°C were recorded over a large part of the Arctic Ocean on November 17, 2013. 


Baffin Bay, west of Greenland, has until now received little attention. High temperature anomalies over the past year show up on the top image. These high temperatures are the more striking given that a cold sea current runs through Baffin Bay, as shown on the image below. 
Methane has emerged strongly from areas that have warmed most in 2013. In August 2013, high concentrations of methane showed up over Siberia. High methane releases have further occurred in all three parts of the cryosphere mentioned above, i.e. from the heights of Antarctica, as discussed at this post, on the Qinghai-Tibetan Plateau, as earlier discussed at this post, and in the Arctic, as discussed in many posts at the Arctic-news blog.

Huge methane concentrations have featured over Baffin Bay recently. The animation below shows huge methane emissions emerging from Baffin Bay on December 2nd, 2013. The power behind these methane releases is strong enough to make it difficult for thicker ice to form in Baffin Bay. The animation below shows an area marked by a red rectangle where it looks like the water would have been covered with thicker ice, had there not been so much methane bubbling up in the area.



This area with very thin ice in Baffin Bay is further illustrated in the Naval Research Laboratory 30-day Arctic sea ice thickness animation below.



This constitues yet another feedback, i.e. methane bubbling up from the seafloor of the Arctic Ocean with a force strong enough to prevent sea ice from forming in the area. 



Wednesday, December 11, 2013

Coconut Macarons w/Ganache

My intention was not to stop blogging for months...  how did it get to be December already?!?  I'm going forgo the excuses reasons and jump right back in with a cookie recipe I hope you'll enjoy.  As with most things, coconut is better with chocolate, and these macarons did not disappoint.



While you may not think of macarons as a traditional holiday cookie, I can't think of a day when I wouldn't want to eat one :)  And while they do require some time (they take me ~2hrs start to finish), one of the great things about macarons is that they are best made a day or two before you actually need them!



Coconut Macarons with Dark Chocolate Ganache
adapted from Annie's Eats & Chez Us
yield:  think I got about 70 using this template

There's no need to age egg whites when using this method, so once you have all your ingredients you can get to baking.

For the macaron shells:
106g almond flour
106g unsweetened coconut, finely shredded
212g powdered sugar
82 and 135g egg whites, divided
354g and a pinch of granulated sugar, divided
237g water

For the ganache:
200ml heavy cream
200g dark chocolate, chopped
1/2t cinnamon

Preheat the oven to 350deg and make sure the rack is in the middle of the oven.

Combine the almond meal, coconut and powdered sugar in a large bowl and whisk together to blend well and break up any clumps.  Make a well in the center of the dry ingredients. Pour in the 82g of egg whites and blend into the dry ingredients until evenly mixed, forming a thick paste.

Combine the 354g granulated sugar with the water in a small saucepan over medium-high heat.  Keep a candy thermometer attached to the side and be watchful! We're heating up the syrup to 248deg, but when it hits 200deg, begin whipping the 135g egg whites with a pinch of granulated sugar in a mixer on medium low speed.  Continue whipping the egg whites on medium speed until soft peaks form.  If soft peaks form before the syrup reaches 248deg, reduce the mixer speed to low to keep the egg whites moving.

Immediately remove the syrup from the heat when it hits 248deg.  Increase the mixer speed to medium and pour the syrup down the side of the bowl in a slow drizzle until fully incorporated.  Increase the mixer speed to medium-high and whip the meringue until stiff, glossy peaks form.

Add the meringue to the almond mixture in thirds, folding in each addition gently until smooth.  You may not use all of the meringue, so add it gradually.  The desired end-point is a smooth batter that runs in thick ribbons off your spatula. [Note: I made extra this time as the last time I tried a coconut batch they could've used a little extra meringue.]

Add the batter to a pastry bag fitted with a plain round tip with a 1/2" opening (or a ziploc bag with a corner cut off to a 1/2" opening).  Holding the bag perpendicular to the baking sheet, pipe rounds onto a parchment-lined baking sheet.  I find a template slipped under the parchment works well for even piping, just be sure to remove the paper before putting it in the oven!  Small peaks that you may see immediately after piping should smooth out if the texture of the batter is correct.

Transfer the baking sheet to the oven and immediately reduce the temperature to 325deg.  Bake for 9-12min, until the tops are smooth and set and feet have formed around the bottom.  Let the shells cool briefly on the baking sheet (~5min), and then peel them away from the parchment and place on a cooling rack.  They should come away easily and fully intact.  Repeat as needed with the remaining batter, replacing the parchment paper with each batch (I was feeling thrifty and used both sides) and bringing the oven temperature back up to 350deg before each batch.

While the macaron shells are cooling, prepare the dark chocolate ganache.  Add chopped chocolate into a bowl and set aside.  Pour cream into a small saucepan and heat over medium heat.  Once the cream comes to a boil, pour over the top of the chocolate.  Let sit for a couple of minutes, then stir until the chocolate has fully melted.  Add cinnamon and stir well.  Let sit in the refrigerator ~1hr before using to fill macarons.

Once the shells are baked and cooled, match them up in pairs by size.  To one macaron shell, add a layer of ganache, then top with the paired shell.  Store in an airtight container in the refrigerator.  These get better with a little time in the fridge, so don't hesitate to make them a ahead of time.




What are you baking up this holiday season?  Or perhaps what treats are you looking forward to receiving?