Methane hydrates (clathrates) exist on the Arctic submarine shelf and slope where they are stabilized by the low temperatures and they have a continuous cap of frozen permafrost which normally prevents methane escape (Figure 1 below).
However, recent research has shown that millions of tons of methane are already being released in the Siberian Arctic through perforated zones in the subsea permafrost cap with the concentrations reaching up to 100 times the normal, such as in the discharge region of the Lena River and the junction of the Laptev and East Siberian Seas (Shakova et al. 2010).
Mean methane concentrations in the Arctic atmosphere showed a striking anomalous buildup between November 1-10, 2008 and November 1-10, 2011 (Figure 2 above)(Yurganov 2012 in Carana, 2012a).
Wales (2012) has outlined the Arctic climate. The climate of the Arctic is moderated by the Arctic Ocean which can never have a temperature below -2 degrees C (28 degrees F). The Arctic winters are cold and long, while the summers are short and cool. All regions are subjected to extremes of solar radiation throughout the year. Parts of the Arctic have a continuous sea ice, glacial ice or snow cover, but every Arctic zone has some snow cover during the year. In January the average temperatures range from 0 degrees C to -40 degrees C (+32 degrees F to -40 degrees F) and in winter the temperature can fall below -50 degrees C (-58 degrees F) in much of the Arctic. In July the average temperatures range from +10 degrees C to -10 degrees C (50 degrees F to 25 degrees F) but can exceed 30 degrees C (86 degrees F) in the summer in some onland regions.
(IOC et al. 2012 in King 2012).
Very extensive continental shelves surround the Eurasian and Amerasian basins. The Barents, Kara, Laptev and East Siberian shelves extend from west to east along the coasts of Europe and Siberia (Figure 6 above) (IOC et al. 2012 in King 2012). The Chukchi and Beaufort shelves extend from west to east along the coast of North America (Figure 6 above) (IOC et al. 2012 in King 2012). The Lincoln shelf lies off the north coast of Greenland which is flanked by the East and West Greenland rift basins to the E and W.
6. DEPOSIT TYPES Giant natural gas reserves underlie the Barents and Kara shelves while significant oil and natural gas potential occurs within the East and West Greenland rift basins (Figure 6 above)(IOC et al. 2012 in King 2012). Subsea (shelf and slope) methane hydrate deposits are extremely widespread throughout the Arctic (Figure 1 above and 9 above)(Max and Lowrie 1993; Kvenvolden 1998, 2001; Shakova et al. 2010; Saldo 2012; Harrison et al. 2008) while geopressured methane formed from their decomposition and also of thermogenic origin is trapped beneath the subsea permafrost and in the complex fault and shear network (Figure 8)(Kholodov et al. 1999, Saldo 2012; Harrison et al. 2008; Shakova et al. 2010). This methane is now escaping in increasing quantities from these faults/shears (taliks) now open to the surface because of destabilization of the methane hydrate by globally warmed marine waters and they have formed widespread Arctic methane eruption centres (torches)(Figures 9 and 11)(Kholodov et al. 1999; Harrison et al. 2008; Shakova et al. 2010; Saldo, 2012, Sekretov 1998).
7. ARCTIC METHANE HYDRATES
Above Figures 7, 8 and 9 show the distribution of Arctic subsea methane eruption points from AIRS data (Saldo 2012; Shakova et al. 2010; Harrison et al. 2008; Yurganov 2012 a, b; Max and Lowrie 1993; NOAA 2011a). Several important points emerge from these diagrams. - The size of the methane eruption (torch) zones increase into the Arctic and are largest well away from land exactly overlying the methane hydrates indicating that they can only be sourced from these subsea methane hydrates and the more profound thermogenic formation of methane from deeply buried oil/gas fields (Figure 9) (Saldo 2012; Harrison et al. 2008; Shakova et al. 2010; Max and Lowrie 1993; Allen and Allen, 1990). The fact that the further north you go, the more the subsea methane is erupting and that this is the region where the greatest global warming induced temperature increase is being observed indicates that the two are intimately linked. Globally warmed oceanic water currents are decomposing the subsea methane hydrates and opening the taliks above the seismically active strike slip and normal faults in the Gakkel Ridge and Beaufort Sea regions where they are releasing geopressured methane in increasing amounts up to the sea surface and into the atmosphere (Figures 9 and 11) (Saldo 2012; Harrison et al. 2008; Shakova et al. 2010; Max and Lowrie 1993, Kholodov et al. 1999; Sekretov 1998).
- There is an exact link between the spreading Gakkel Ridge and its active seismicity, high heat flow and hot water emitted from black smokers along active fault systems bounding it and the formation of methane gas filled taliks above the fault zones formed from the destabilization of subsea hydrothermal and slope methane hydrates (Figure 9) (Saldo 2012; Harrison et al. 2008; Shakova et al. 2010; Max and Lowrie 1993). Globally warmed oceanic water is also evidently penetrating down the highly fractured margins of the Gakkel Ridge where it is coming in contact with the rising mid- ocean magmas preventing them from cooling efficiently with the result that the ridge is becoming more and more active. The hotter the magmas are, the more expanded they are, generating torsional stresses on the surrounding rocks because the Gakkel mid - ocean ridge is expanding in a wedge like fashion in a region cutting at right angles through the Laptev Sea (East Siberian Arctic Shelf) north of the Tiksi (Figures 15 and 16) (IOC et al. in King 2012; Avetisov 2008; Sekretov 1998; Yurganov 2012; Saldo 2012; Hansen 2011; Light and Carana 2011). Although the effect of globally warmed Siberian river waters causing methane decomposition and methane release is locally important in the ESAS (Shakova et al. 2007, 2008, 2010) it is clearly not the driving force for the major methane atmospheric eruptions in the Laptev Sea shelf slope region of the Gakkel Ridge where the methane eruption centers occur directly above the zone where the Gakkel Ridge intersects a huge zone of slope and hydrothermal methane hydrates which are cut by a radiating zone of shear faults in a region of active seismicity (Figures 15, 1 and 9)(Harrison et al, 2008; Max and Lowrie, 1993)
- The methane eruption (torch) zones are mostly directly linked to major strike - slip and normal fault systems indicating that the latter are charged with geopressured gas and have acted as conduits for the migration of gas from destabilized shallow methane hydrates (0 - 500 meters; Kholodov et al. 1999) and from deeper gas and oil formations that have undergone methanogenesis (Allen and Allen, 1990). In the latter case the oil/gas traps became over filled and leaked (Figures 9, 10 and 11) (Allen and Allen, 1990; Light, Posey, Kyle and Price, 1987; Max and Lowrie 1993; Shakova et al. 2010; Harrison et al. 2008; Sekretov 1998). The carbon isotopic signature of the methane can be used to determine what percentage of the surface gas is derived from these two separate sources (Borowski 2004; Whiticar, 1994; Light, Posey, Kyle and Price, 1987).
- The methane eruption zones (torches) occur widely in the East Siberian Arctic Shelf (ESAS) but the largest are confined to the region outside the ESAS where the Gakkel mid ocean ridge system intersects the methane hydrate rich shelf slope region at right angles and its wedge like opening and spreading is putting the formations and overlying methane hydrate sediments under torsional stress and in the process activating the major strike slip faults that fan/radiate from this region (Figures 9, 11 and 16)(Avetisov 2008; Sekretov 1998: Yurganov 2012; Saldo 2012; Hansen 2011; Light and Carana 2011; Max and Lowrie 1993; Shakova et al 2010; Harrison et al 2008).
- The major and minor strike slip and normal faults are clearly charged with overpressured methane and form a continuous subterranean network as methane gas is escaping from these fault lines often many hundreds of km up dip and away from the subsea methane hydrate zones through which these fault zones pass (Figures 9 and 11) (Saldo 2012; Shakova et al. 2010; Max and Lowrie 1993; Kholodov et al. 1999; Harrison et al 2008; Sekretov 1998).
- One small methane eruption zone occurs directly over the centre of the Gakkel Ridge and probably represents thermogenic deep seated methane being released by the magmatic heating of adjacent oil/gas fields that the rising (pyroclastic) magma is heating up (Figure 9) (Edwards et al. 2001). This surface gas eruption appears to only represent a tiny percentage of the total gas released from other sources such as methane hydrates as do methane eruptions around Cenozoic volcanics offshore Tiksi on the East Siberian shelf (Figure 9) (Saldo 2012; Shakova et al 2010; Max and Lowrie 1993).
- An elongated set of methane eruption zones occur on the west submarine slope off Svalbard flanking the Gakkel Ridge and appear to be the result of methane hydrate decomposition caused by the changing pressure and temperature conditions due to submarine slides/slumps evidently set off by Gakkel Ridge seismic activity close to the widest zone of ridge opening (Figure 9) (Saldo 2012; Shakova et al 2010; Max and Lowrie 1993). This may be similar to the Storegga slide (Light and Solana, 2002).
- Shakova et al, 2010a estimate that some 50 Gt of methane could erupt at any moment on the East Siberian Arctic Shelf (ESAS) where subsea methane eruption zones are up to 1 km across and this will cause an equivalent increase in the mean carbon dioxide content of the atmosphere by 12 generating a climatic catastrophe. Such an increase in equivalent carbon dioxide would cause a worldwide atmospheric temperature anomaly up to 10 degrees Centigrade above the present atmospheric mean as it spreads around the Earth's atmosphere and lead to our certain extinction within the next 20 to 40 years (See Carana and Light, 2011; Figures 12 and 13). However it is evident from Figure 9 that most of the methane eruption zones visible from the stationary start points of atmospheric methane clouds recognised on AIRS data (Yurganov, 2012) lie outside the East Siberian Arctic Shelf (ESAS) area (Max and Lowrie, 1993; Shakova et al. 2010; Saldo 2012). Furthermore from two to three times as much methane appears to be undergoing release into the atmosphere outside the ESAS as within it (Figure 17)(Saldo 2012; Harrison et al 2008). Consequently the estimate of Shakova et al. (2010a) of some 50 Gt of unstable methane hydrates ready to release methane into the atmosphere from the ESAS at any time can be replaced roughly by some 100 Gt to 200 Gt of unstable methane hydrate ready for immediate release of methane into the Arctic atmosphere for the entire Arctic region. The release of such a vast quantity of methane into the Arctic atmosphere will cause a worldwide atmospheric temperature anomaly between 20oC to 40oC degrees above the present atmospheric mean. As this giant methane cloud rises because of its low denisty and spreads around the Earth's atmosphere, it will lead to humanities complete and absolute extinction within the next 20 to 40 years unless we can eliminate the threat that this methane poses.
8. EXPLORATION Kholodov et al. 1999 have modeled the thickness of the offshore permafrost on the Laptev Sea shelf (Figures 10 and 11 above) (Harrison et al. 2008; Sekretov 1998; Saldo 2012). Figure 10 shows the distribution of the thickness calculated permafrost and the fault system from the most recent Arctic map (Harrison et al. 2008), while Figure 11 shows the atmospheric methane eruption points in yellow and purple derived from the stationary start points of methane clouds on AIRS data (Saldo, 2012). The distribution of the methane eruption zones in the Laptev Sea is clearly linked to the fault network but also to the trend of the Gakkel Ridge as eruption zones surround Cenozoic volcanoes close to latitudes 73 and 75 degrees (Sekretov, 1999) along the shelf extension of the submarine ridge system.
The calculated thickness of the ice bonded permafrost in the Laptev Sea between latitudes 72N and 77N and at water depths of 20 meters to 100 meters varies from 80 meters to 470 meters in regions of structural uplift and 80 meters to 530 meters in regions of structural depression (Figure 11) (Kholodov et al. 1999). Although no borehole data was available from the Laptev Sea shelf to check the calculated data set, the data was calibrated on well temperature measurements from the Tiksi area (from Devyatkin in Kholodov et al. 1999).
The maximum thickness (ca 500 meters) of the offshore ice bound permafrost on the Laptev Sea shelf formed around 18,000 years ago (Sartan cryochron) but has been reduced to 150 to 200 meters due to the recent thawing of these deposits from beneath and the retreat of the shorelines due to thermoerosion (Figures 10 and 11) (Kholodov et al. 1999).
Open and closed linear extended taliks, representing walls of melted permafrost exist above large seismically active (strike slip and normal) fault lines with high values of geothermal flow (from 100 mW/m^2 or greater) (Figure 18) (Kholodov et al. 1999). Globally warmed Arctic Ocean sea water has melted and opened the sub - permafrost taliks to the surface where they represent the eruption points (base of the torches) for the atmospheric methane clouds that are visible on the AIRS data (Saldo, 2012). Open and closed taliks also exist in the channel parts of the paleovalleys of large rivers and in the offshore zone to depths of 15 to 20 meters (Kholodov et al. 1999).
9. MINERAL RESOURCE AND RESERVE ESTIMATESThe Arctic submarine permafrost contains abundant methane trapped as hydrates below the shelf and slope and the reserves are estimated at more than 140 times the volume of methane presently trapped in the atmosphere (Light and Solana, 2002) equivalent to 2.11*10 power 16 cubic metres of methane (STP)(Engineering Toolbox, 2011). Kvenvolden and Grantz (1990) have estimated that the total reserves of Arctic subsea methane as 540 Gt organic carbon which is equivalent to 1*10 power 15 cubic metres. McGuire et al. 2009 estimate the total reserves of the Arctic ocean methane hydrates as ranging from 30 to 170*10 power 15 grams methane equivalent to 5.03*10 power 14 to 2.85*10 power 15 cubic metres of methane (STP).
Together the Norwegian and Arctic basins have some 1,000,000 square km of slopes exposed with an average potential thickness of some 363.5 metres of gas hydrate on them from 28 modelled estimates of the ice bonded permafrost on the Laptev Sea shelf (Light and Solana, 2002; Kholodov et al. 1999). As each cubic metre of gas hydrate contains 164 cubic metres of gas (Engineering Toolbox, 2011), the total Arctic methane hydrate reserve is estimated at 5.96*10 power 16 cubic metres of methane (STP). Shakova et al (2008) estimated the total value of the ESAS carbon pool as greater than 1400 GT organic carbon equivalent to 1.4*10 power 18 grams. This gives a total ESAS methane reserve of 2.61*10 power 15 cubic metres of methane (STP). Because the ESAS represents about 1/4 of the total surface area of the Arctic shelves we can fix the total Arctic methane reserves at about 1.04*10 power 16 cubic metres of methane (STP).
Shakova et al. (2010a) have subsequently estimated the reserves of the East Siberian Arctic Shelf (ESAS) at 500 Gt of organic carbon in the permafrost, 1000 Gt of organic carbon locked in the subsea methane hydrate deposits and 700 Gt of free methane trapped beneath the methane hydrate stability zone. As one Gt is equivalent to 10 power 15 grams, the carbon locked in the subsea ESAS methane hydrate deposits is some 1*10 power 18 grams and 7*10 power 17 grams carbon as a free methane gas below the methane hydrate stability zone. This gives a total subsea methane reserve in the ESAS of 3.17*10 power 15 cubic metres of methane (STP). Because the ESAS represents about 1/4 of the total surface area of the Arctic shelves we can fix the total Arctic methane reserves at about 1.27*10 power 16 cubic metres of methane (STP).
The mean methane reserves for the subsea Arctic methane hydrate from the above seven estimates is 1.545*10 power 16 cubic metres of methane (STP) with the value ranging between 5*10 power 14 and 5.96*10 power 16 cubic metres methane (STP). The mean methane reserves of the subsea methane hydrates are equivalent to 700 million giant gas fields, where a giant gas field is defined as containing more than 3 trillion cubic feet or 85 million cubic metres of recoverable gas (Halbouty, 2001).
10. CONCLUSIONS The historical development of the offshore subsea permafrost methane hydrate layer and the subsequent degradation and thermoerosion of the permafrost with the opening of oceanic taliks by global warming effects is based on an W - E deep water profiles of the northern Laptev Sea (ca 75 to 77 Degrees N) from Kholodov et al. 1999 (see Figure 18).
18,000 years ago a major ice advance occured in the Northern Hemisphere and the ocean water depth was some 200 meters lower than at the present moment (Calder, 1983). At the same time (18,000 years ago) a series of closed vertical taliks (sheared melted vertical wall like zones in the subsea permafrost - methane hydrates) were filled with free methane and developed above seismically active strike - slip fault zones that were regions of increased geothermal gradient (> 100 mW/square meters) in the region the slowly spreading Arctic Gakkel Ridge (Figure 18) (Kholodov et al. 1999).
The Arctic methane hydrate gas reserves represent a massive "Green Gas" energy source which is available to mankind over a number of centuries if the methane is extracted in a controlled manner. The Arctic methane hydrate gas reserves also represent a catastrophic threat which will lead to our certain extinction if they are allowed to erupt out of control into the atmosphere over a short period of time. The mean methane reserves for the subsea Arctic methane hydrates (1.545*10 power 16 cubic metres of methane (STP)) is equivalent to more than 100 times the volume of methane presently trapped in the atmosphere and if it was all released would cause a mean atmospheric temperature increase of more than 190 degrees C at a methane global warming potential of 100 active over the relatively short time that methane is stable (15 years)(Dessus et al. 2008). Under these extreme conditions the oceans would begin to boil off and the Earth's atmosphere start to resemble that of Venus.
11. RECOMMENDATIONS Proposed Subsea Methane Extraction Method to Prevent Arctic Methane EruptionsThis proposed subsea methane extraction system to prevent Arctic methane eruptions on the Siberian Shelf, Canada Basin/Canada Arctic Archipelago and Bering Sea is based on an W - E deep water profile of the northern Laptev Sea (ca 75 to 77 Degrees N) from Kholodov et al. 1999 (Figure 18).
After 2015, when the Arctic Ocean becomes navigable (Figure 5 Carana 2012b) it will be possible to set up a whole series of drilling platforms adjacent to but at least 1 km away from the high volume methane eruption zones and to directionally drill inclined wells down to intersect the free methane below the sealing methane hydrate permafrost cap within the underlying fault network. The methane is likely to be highly overpressured beneath the sealing permafrost and this is the drive that has made the methane gas find its way out from beneath the permafrost layer by following multiple pathways represented by the fault system network often many hundreds of km up dip from the methane hydrates and also via open taliks to the sea surface and atmosphere in a relatively short period of time. This overpressure can result in "blowouts" where drillers penetrate the sealing shale - permafrost making overpressure detection and correct density muds a very important facet of drilling in the subsea Arctic permafrost. The actual origin of the methane gas is not important, whether it formed from methane hydrate destabilization or from thermogenic breakdown of oil in deeper reservoirs (Shakova et al. 2010). In either case it has strongly charged the network of faults underlying the subsea Arctic permafrost where it is now overpressured and erupting.
High volume methane extraction from below the subsea methane hydrates using directional drilling from platforms situated in the stable areas between the talik/fault zones should reverse the methane and seawater flow in the taliks and shut down the uncontrolled methane sea water eruptions. Methane extraction from below the subsea permafrost will pull down the rising methane and seawater erupting in the taliks and enable an equilibrium position to be reached in which no methane freely enters the atmosphere and is all being drawn up inclined wells to the drilling platform where it is separated from the seawater and stored in LNG tankers for sale. The controlled access of globally warmed sea water drawn down through the taliks to the base of the methane hydrate - permafrost cap will gradually destabilize the underlying methane hydrate and will allow complete extraction of all of the gas from the methane hydrate reserve over an extended period of time. The methane extraction boreholes can be progressively opened at shallower and shallower levels as the subterranean methane hydrate decomposes allowing the complete extraction of the sub permafrost methane reserve.
Methane derived from the submarine hydrates in the shallow Laptev Sea could also be piped ashore to run electric power generating stations. Some of this electric energy could be used for powering radio interference transmission stations (Lucy Project) designed to destroy the already erupted Arctic atmosphere methane clouds (Light 2011a). These stations could be situated on the Siberian coast, on the New Siberian Islands and on Novaya Zemlya. A similar system could also be used in Canadian and Alaskan territory.
The methane and seawater will be produced to the surface where the separated methane will stored in specially designed LNG (Liquefied Natural Gas) tankers for transport and sale to customers as a subsidized "Green Energy" alternative to coal and oil for power generation and for air and ground transport (Figure 18). Standby LNG tankers must remain linked to the pipeline network in case there are problems such as the volume of gas being recovered or blowouts causing part of the pipeline network to be shut down. Other LNG tankers will be transferring the methane for sale to markets in Japan, China, India, US, Canada and Europe. The methane energy source will be of vital importance to Japan, who needs to replace its nuclear generating capacity with a safer "Green" alternative.
Liquid natural gas (LNG) is the most efficient method of transporting large volumes of gas over long distances. Methane can be liquefied at liquefaction plants and transported in LNG carriers across oceans and in tank trucks as liquefied or compressed natural gas (CNG) over land after it has been regasefied at the terminal. Floating liquefied natural gas (FLNG) facilities are being developed by Shell to be completed by 2017 which will allow all gas processing to be done at an offshore gas field (FT.com, 2011). Similar systems must be developed immediately for use in the Arctic Ocean on the methane hydrate eruption fields.
Because of the massive size of the methane hydrate "Green Gas" reserves in the Arctic (equivalent to more than 700 million giant gas fields; Halbouty 2001) the process of methane extraction could last over hundreds of years and supply fuel for a safe "Green Gas" electricity generation future during the long transition of the Earth to a complete green powered economy. New technologies will come in designing and mass producing drilling platforms for the Arctic shallow shelf and slope regions, in mass producing specific LNG tankers for methane, in designing and developing the gas pipeline infrastructure to transport the gas and converting all existing coal and oil electric power stations to natural gas.
Gazprom is constructing large drilling platforms for working in the Arctic in shallow water where the methane hydrate threat is large (Gazprom, 2011). Where possible jack-up rigs may be preferable as they can sit on the sea floor in case there is a blow - out, but the use of rigs with both a floating and jack up capability is to be preferred. Where undersea pipelines are laid down they must be run parallel to the trend of and some distance away from the major strike - slip faults cutting the Gakkel Ridge because these faults are active and could cause severe damage to undersea structures.
Co-production of Overpressured Methane and Seawater Where the trapped methane is sufficiently geopressured within the fault system network underlying the Arctic subsea permafrost and is partially dissolved in the water (Light, 1985; Tyler, Light and Ewing, 1984; Ewing, Light and Tyler, 1984) it may be possible to coproduce it with the seawater which would then be disposed of after the methane had be separated from it for storage (Jackson, Light and Ayers, 1987; Anderson et al., 1984; Randolph and Rogers, 1984; Chesney et al., 1982).
Canadian Arctic Many methane eruption zones occur along the narrow fault bound channels separating the complex island archipelago of Arctic Canada (Figure 6 and 9)(IOC et al 2012 in King 2012; Shakova et al. 2010; Max and Lowrie 1993; Saldo 2012; Harrison et al. 2008). In these regions drilling rigs could be located on shore or offshore and drill inclined wells to intersect the free methane zones at depth beneath the methane hydrates, while the atmospheric methane clouds could be partly eliminated by using a beamed interfering radio transmission system (Lucy Project)(Light 2011a). A similar set of onshore drilling rigs could tap sub permafrost methane along the east coast of Novaya Zemlya (Figure 6 and 9)(IOC et al 2012 in King 2012; Shakova et al. 2010; Max and Lowrie 1993; Saldo 2012; Harrison et al. 2008).
Methane as a Subsidised "Green Energy" Fuel Wales (2012) has outlined the importance of methane as a "Green Energy" fuel. 84 percent of the world's natural methane gas production is from 15 countries and it has now become a major international point of friction. This is because compressed methane is a vital necessity for electrical generation and domestic heating and cooking in many countries. Methane as liquid natural gas can be used for aircraft and road transport and produces little pollution compared to coal, gasoline and other hydrocarbon fuels. Methane is also used in the manufacture of hydrogen, fertilizers, fabrics, glass, steel, plastics, paint and other products.
Methane is a major fuel for highly efficient gas - steam, combined cycle, electrical generators in power stations. Fuel cells have also been developed that turn methane into electricity.
Methane is a high energy fuel, with more energy than other comparable fossil fuels (Wales 2012). Burning methane produces 45% less carbon dioxide than coal and 30% less than petroleum (Naturalgas, 2011). Methane is a potent domestic cooking and heating fuel generating heat in excess of 1093oC (2000oF) and it produces more heat per unit mass (55.7 kJ/g) than other complex hydrocarbons (Zimmerman and Zimmerman, 1995; Wales 2012)
Compressed methane (natural gas) is more environmentally friendly than gasoline or diesel as a vehicle fuel (Cornell 2008). By 2008 there were some 9.6 million vehicles running on methane (India 650,000; Iran 1 million; Brazil 1.6 million; Argentina 1.7 million)(IANGV 2009; Pike Research 2009). Adsorption has been researched as a method of storing methane for a vehicle fuel (Duren et al. 2004).
Liquefied methane has been tested since 1970 as a fuel for aircraft (Tupolev 2011). Methane is some 200$ cheaper to operate per ton than other fuels and there is a large reduction in greenhouse gas emissions. As a jet fuel, liquid methane has more specific energy than standard kerosene mixes and the low temperature of the methane cools the air the engine compresses increasing its volumetric efficiency.
NASA has also conducted research on methane as a potential rocket fuel to make long distance space travel economic (NASA 2007).
Support should be sought from the United nations, World Bank, national governments and other interested parties for a subsidy (such as a tax rebate) of some 5% to 15% of the market price on Arctic permafrost methane and its derivatives to make it the most attractive LNG for sale compared to LNG from other sources. This will guarantee that all the Arctic gas recovered from the Arctic methane hydrate reservoirs and stockpiled, will immediately be sold to consumers and converted into safer byproducts. This will also act as an incentive to oil companies to produce methane in large quantities from the Arctic methane hydrate reserves. In this way the Arctic methane hydrate reservoirs will be continuously reduced in a safe controlled way over the next 200 to 300 years supplying an abundant "Green LNG" energy source to humanity.
12. ACKNOWLEDGEMENTS My sincere thanks to Dr Sigrid Clift of the Bureau of Economic Geology, University of Texas at Austin for giving me access to critical information on the distribution and history of permafrost in the Arctic. Sincere thanks also to Harold Hensel and Sam Carana whose encouragement and hard work have helped me find a complete solution to the catastrophic threat posed to our existence on Earth by the escalating Arctic atmospheric methane emissions. I am indebted to Tenny Naumer of the Arctic Methane Emergency Group for assisting me in the acquisition of the AIRS data which defines precisely the major Arctic methane emission zones.
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FIGURES
(Click on any image to view enlarged versions)
Figure 1. Arctic Ocean slope and deep water methane hydrate regions
Figure 2. AIRS atmospheric methane concentration data for the Arctic
Figure 3. Predicted locations of methane hydrate from surface temperature
Figure 4. Methane atmospheric temperature trends from methane concentrations at Svalbard
Figure 5. Arctic sea ice melting curve from Piomass data
Figure 6. International bathymetric chart of the Arctic Ocean with names of seafloor features
Figure 7. The concentration of methane eruption centres from Airs data
Figure 8. Methane eruption centres (torches) and high fault concentrations
Figure 9. The distribution of methane hydrates in the Arctic Ocean and its relation to extensive subsea methane emission zones (torches)
Figure 10. Modeled subsea permafrost thickness in the Laptev Sea
Figure 11. Modeled subsea permafrost thickness in the Laptev Sea with methane eruption centres
Figure 12. Diagram showing the region of stability of atmospheric Arctic methane erupted from destabilized shelf and slope methane hydrates
Figure 13. Further refined mean global extinction fields using a latent heat of ice melting curve
Figure 14. Highlighted topography of the Arctic Ocean showing the trend of the Gakkel Ridge
Figure 15. Inverted Arctic topography showing the wedge shaped opening of the Gakkel Ridge
Figure 16. Methane emission points related to the wedge like opening of the Gakkel Ridge
Figure 17. Extreme, high and medium priority submarine Arctic clathrate (methane hydrate) atmospheric methane emission zones
Figure 18. Prevention of Arctic methane eruptions
