Author: Neville

  • James Hansen: Fossil fuel addiction could trigger runaway global warming

    James Hansen: Fossil fuel addiction could trigger runaway global warming

    Without full decarbonisation by 2030, our global emissions pathway guarantees new era of catastrophic climate change

    Nasa image of planet Earth

    Nasa image of planet Earth. Photograph: Ho/Reuters

    The world is currently on course to exploit all its remaining fossil fuel resources, a prospect that would produce a “different, practically uninhabitable planet” by triggering a “low-end runaway greenhouse effect.” This is the conclusion of a new scientific paper by Prof James Hansen, the former head of NASA‘s Goddard Institute for Space Studies and the world’s best known climate scientist.

    The paper due to be published later this month by Philosophical Transactions of the Royal Society A (Phil. Trans. R. Soc. A) focuses less on modelling than on empirical data about correlations between temperature, sea level and CO2 going back up to 66 million years.

    Given that efforts to exploit available fossil fuels continue to accelerate, the paper’s principal finding – that “conceivable levels of human-made climate forcing could yield the low-end runaway greenhouse effect” based on inducing “out-of-control amplifying feedbacks such as ice sheet disintegration and melting of methane hydrates” – is deeply worrying.

    The paper projects that global average temperatures under such a scenario could eventually reach as high as between 16C and 25C over a number of centuries. Such temperatures “would eliminate grain production in almost all agricultural regions in the world”, “diminish the stratospheric ozone layer”, and “make much of the planet uninhabitable by humans.”

    Hansen and his co-authors find that:

    “Estimates of the carbon content of all fossil fuel reservoirs including unconventional fossil fuels such as tar sands, tar shale, and various gas reservoirs that can be tapped with developing technology imply that CO2 conceivably could reach a level as high as 16 times the 1950 atmospheric amount.”

    They calculate that there is “more than enough available fossil fuels” to generate emissions capable of unleashing “amplifying feedbacks” that could trigger a “runaway” greenhouse effect “sustained for centuries.” Even if just a third of potentially available fossil fuel resources were exploited, calculations suggest, this scenario would still be guaranteed, meaning decisions we make this century will determine the fate of generations to come.

    James Hansen ‘We don’t have a leader who is able to grasp [the issue] and say what is really needed. Instead we are trying to continue business as usual,’ said James Hansen in 2009. Photograph: Gareth Fuller/PA”Governments are allowing and encouraging fossil fuel companies to go after every conceivable fuel”, said Hansen, “which is an obtuse policy that ignores the implications for young people, future generations and nature. We could make substantial parts of the Earth uninhabitable.”

    The conclusions of Hansen’s latest paper are stark:

    “Most remaining fossil fuel carbon is in coal and unconventional oil and gas. Thus, it seems, humanity stands at a fork in the road. As conventional oil and gas are depleted, will we move to carbon-free energy and efficiency – or to unconventional fossil fuels and coal?

    … It seems implausible that humanity will not alter its energy course as consequences of burning all fossil fuels become clearer. Yet strong evidence about the dangers of human-made climate change have so far had little effect. Whether governments continue to be so foolhardy as to allow or encourage development of all fossil fuels may determine the fate of humanity.”

    The new paper by James Hansen is just the latest confirming that we are on the verge of crossing a tipping point into catastrophic climate change. Other recent scientific studies show that the current global emissions trajectory could within three years guarantee a 2C rise in global temperatures, in turn triggering irreversible and dangerous amplifying feedbacks.

    According to a scientific paper given at the Geological Society of London last month, climate records from Siberian caves show that temperatures of just 1.5C generate “a tipping point for continuous permafrost to start thawing”, according to lead author Prof Anton Vaks from Oxford University’s Department of Earth Sciences. Conventional climate models suggest that 1.5C is just 10-30 years away.

    Permafrost thawing releases sub-ice undersea methane into the atmosphere – a greenhouse gas twenty times more potent that carbon dioxide. In June, NASA’s new five-year programme to study the Arctic carbon cycle, Carbon in Arctic Reservoirs Vulnerability Experiment (CARVE), declared:

    “If just one percent of the permafrost carbon released over a short time period is methane, it will have the same greenhouse impact as the 99 percent that is released as carbon dioxide.”

    Another paper suggests that conventional climate modelling is too conservative due to not accounting for complex risks and feedbacks within and between ecosystems. The paper published in Nature last Wednesday finds that models used to justify the 2C target as a ‘safe’ limit focus only on temperature rise and fail to account for impacts on the wider climate system such as sea level rise, ocean acidification, and loss of carbon from soils. It concludes that the 2C target is insufficient to avoid dangerous climate change.

    The problem is that our current global emissions trajectory already commits us to a 2C rise anyway. Papers published by the Royal Society in 2011 showed that emissions pledges would still put the world on track for warming anywhere between 2.5C and 5C – and that a failure to deliver these pledges could see global temperatures rise by 7C by 2100. Amongst them, a Met Office study concluded that strong amplifying feedbacks – such as the oceans’ reduced ability to absorb atmospheric carbon dioxide leading to further warming – could see us reach 4C as early as 2060.

    But as Hansen explained in a recent interview:

    “Four degrees of warming would be enough to melt all the ice… you would have a tremendously chaotic situation as you moved away from our current climate towards another one. That’s a different planet. You wouldn’t recognise it… We are on the verge of creating climate chaos if we don’t begin to reduce emissions rapidly.”

    After the last round of climate talks in Doha, a report by Climate Action Tracker concluded that the world is currently on path to see warming of 3C by 2040, triggering the melting of the Greenland ice sheet and Arctic permafrost.

    This was corroborated last month by the International Energy Agency (IEA), which found that even with current climate policies in place, we are locked into a rise of between 2C and 5.3C. Two years ago, the IEA concluded that we had five years left to implement urgent energy reforms after which we would no longer be able to avoid dangerous climate change. We are now three years away from that point-of-no-return.

    To make matters worse, the IEA’s analysis is based on conventional models which do not fully account for amplifying feedbacks such as methane releases from permafrost thawing. The IPCC’s forthcoming Fifth Assessment Report, like its predecessors, will specifically exclude the permafrost carbon feedback from its projections.

    The implication is that policymakers are riding blind – we do not really know how close we are to a tipping point into catastrophe.

    There is a solution. According to Hansen, we need to focus on a maximum target of 1C. “The goal of keeping warming close to 1C is to keep climate close to the Holocene range, thus avoiding any major amplifying feedbacks,” he said.

    “The 1C goal requires rapid phase out of fossil fuel emissions, which would require a rising carbon fee. To continue to burn every fuel that can be found is the opposite approach – they are day and night.”

    Such a rapid fossil fuel phaseout was proposed to the Parliamentary Environment Audit Committee early last year in the form of complete decarbonisation of power by 2030. Unfortunately, the UK bill to that effect was narrowly defeated in the House of Commons last month.

    There is still hope – the bill is currently up for consideration by the House of Lords. If the bill eventually passes, Britain might still play a leading role in heralding the energy revolution that could help save the planet, while saving the nation up to £100 billion.

    Dr Nafeez Ahmed is executive director of the Institute for Policy Research & Development and author of A User’s Guide to the Crisis of Civilisation: And How to Save It among other books. Follow him on Twitter @nafeezahmed

  • Pine Island glacier loss must force another look at sea-level forecasts as giant iceberg is spawned

    climate code red


    Pine Island glacier loss must force another look at sea-level forecasts as giant iceberg is spawned

    Posted: 09 Jul 2013 02:54 PM PDT

    A crack has opened across the full width of the
    PIG ice shelf, spawning a new berg

    Update 10 July 2013: Pine Island spawns giant new iceberg as fissure extends full width of glacier

    BBC New reports that, as anticipated for two years (story below), “Pine Island Glacier (PIG), the longest and fastest flowing glacier in the Antarctic, has spawned a huge iceberg… The block measures about 720 square kilometres in area, roughly eight times the size of Manhattan Island in New York.”

    Confirmation that a fissure had spread across the full width of the glacier was confirmed on 8 July with images obtained from the German TerraSAR-X satellite (pictured at right).  The fissure was first observed in October 2011 (image below).
         Of all the Antarctic glaciers, Pine Island is contributing most to sea-level rises. Ted Scambos of the National Snow and Ice Data Center (NSIDC) in Boulder, Colorado told National Geographic in early 2012 that iceberg calving is a normal cycle in which the floating section grows, stresses mount, and an iceberg breaks off, but when the pattern deviates, glaciologists take notice:

    In this case, the crack is forming significantly farther “upstream” than has previously been the case. That “signifies that there are changes in the ice,” Scambos said.
    When “that point of rifting starts to climb upstream, generally you see some acceleration of the glacier.” That means that the ice will flow into the ocean at a faster rate, contributing even more to sea level rise.
    Such an acceleration is of particular concern at the Pine Island Glacier, because, among Antarctic glaciers, it’s “the one that’s contributing the most to sea level rise.”
    In fact, he said, ice flows from that glacier alone account for a quarter to a third of Antarctica’s total contribution to sea level rise.

    Pine Island Glacier’s vast crack, pictured in October 2011.
    View hi-res image.
    Image courtesy NASA/METI/ERSDAC/JAROS

    Update 4 February 2012:  A giant crack in Antarctica’s Pine Island Glacier signals birth of monster iceberg

    National Geographic reports that Antarctica’s fastest-melting glacier is about to lose a chunk of ice larger than all of New York City, with implications for the rate of rise for sea levels. The crevasse (pictured) is 30 kilometres long and up to 80 metres wide, cutting across the floating tongue of the Pine Island Glacier in West Antarctica, and expected to create an iceberg of about 900 square kilometres.
    That is larger than the area of Manhattan, Brooklyn, Queens, Staten Island and the Bronx combined, according to NASA. In Australian terms, it is larger than the Adelaide Metropolitan Region.
    Eric Rignot of NASA’s Jet Propulsion Laboratory says the monster iceberg will be created  “in the coming months for sure.”

    Update 28 June 2011: Columbia University researchers have just reported that “Ocean Currents Speed Melting of Antarctic Ice”. They find that “Stronger ocean currents beneath West Antarctica’s Pine Island Glacier Ice Shelf are eroding the ice from below, speeding the melting of the glacier as a whole, according to a new study in Nature Geoscience. A growing cavity beneath the ice shelf has allowed more warm water to melt the ice, the researchers say—a process that feeds back into the ongoing rise in global sea levels. The glacier is currently sliding into the sea at a clip of four kilometers (2.5 miles) a year, while its ice shelf is melting at about 80 cubic kilometers a year – 50 percent faster than it was in the early 1990s – the paper estimates.”
    For discussion of map/image, see here.

    Post of 24 January 2010:

    New research suggest that just two collapsing West Antarctic glaciers could add another half a metre to sea levels this century

    The Victorian and Queensland governments decisions to stick to an “upper boundary” sea-level rise estimate of 0.8 metres by 2100 (and NSW at 0.9 metre) for planning purposes needs urgent revision, with new modelling showing two West Antarctic glaciers are past their tipping points.
    The 0.8 metre estimate for sea-level rises to 2100 is already obsolete:

    • The Copenhagen climate science congress of March 2009 estimated a sea-level rise of 0.75–1.9 metres by 2100
    • The federal Department of Climate Change’s November 2009 climate update reports estimates of a 0.5–2 metre rise by 2100
    • A study published in the Proceedings of the National Academy of Sciences in December found that global average sea levels are likely to rise by between 75cm and190cm by the end of the century.

    So how far could we reasonably expect sea levels to rise by 2100? As the world’s oceans warm, they expand and sea-levels rise, but how quickly the loss of polar ice sheets will add to the rise is difficult to estimate, principally because ice-sheet and sea-ice dynamics are not sufficiently well understood, and they are subject to non-linear (rapid and unexpected) changes, such as is occurring with sea-ice in the Arctic. The question is no longer whether the Greenland and West Antarctic ice sheets (WAIS) are losing mass (they are!) but if and when they pass tipping points for large, irreversible ice mass loss, and how fast that will occur.
    Recent research by Blancon et. al published in Nature in 2009 examining the paleoclimate record shows sea level rises of 3 metres in 50 years due to the rapid melting of ice sheets 120,000 years ago. Mike Kearney, of the University of Maryland, said it’s “within the realm of possibility” that global warming will trigger a sudden collapse of the West Antarctic ice sheet, which could lead to a rapid increase in sea levels like that predicted by the study.
    Given the catastrophic failure to date of global climate policy-making (Copenhagen outcome =4-degree rise by 2100), big sea level rises are on the way for the sort of temperature increases now on the table. NASA climate science chief James Hansen wrote in New Scientist that:

    Oxygen isotopes in the deep-ocean fossil plankton known as foraminifera reveal that the Earth was last 2°C to 3°C warmer around 3 million years ago, with carbon dioxide levels of perhaps 350 to 450 parts per million. It was a dramatically different planet then, with no Arctic sea-ice in the warm seasons and sea level about 25 meters higher, give or take 10 meters.

    Even more compelling, Professor Eelco Rohling of University of Southampton says:

    Even if we would curb all CO2 emissions today, and stabilise at the modern level (387 parts per million by volume), then our natural relationship suggests that sea level would continue to rise to about 25 metres above the present.

    Then on 13 January this year, New Scientist published this story showing calculations that the Pine Island glacier in the West Antarctic has likely passed its tipping point, with researchers estimating that this one glacier alone could add a quarter of a metre to sea levels by 2100:

    Major Antarctic glacier is ‘past its tipping point’

    A major Antarctic glacier has passed its tipping point, according to a new modelling study. After losing increasing amounts of ice over the past decades, it is poised to collapse in a catastrophe that could raise global sea levels by 24 centimetres.
    Pine Island glacier (PIG) is one of many at the fringes of the West Antarctic ice sheet. In 2004, satellite observations showed that it had started to thin, and that ice was flowing into the Amundsen Sea 25 per cent faster than it had 30 years before.
    Now, the first study to model changes in an ice sheet in three dimensions shows that PIG has probably passed a critical “tipping point” and is irreversibly on track to lose 50 per cent of its ice in as little as 100 years, significantly raising global sea levels.
    The team that carried out the study admits their model can represent only a simplified version of the physics that govern changes in glaciers, but say that if anything, the model is optimistic and PIG will disappear faster than it projects.
    Richard Katz of the University of Oxford and colleagues developed the model to explore whether the retreat of the “grounding line” – the undersea junction at which a floating ice shelf becomes an ice sheet grounded on the sea bed – could cause ice sheets to collapse.
    ….
    The model suggests that within 100 years, PIG’s grounding line could have retreated over 200 kilometres. “Before the retreating grounding line comes to a rest at some unknown point on the inner slope, PIG will have lost 50 per cent of its ice, contributing 24 centimetres to global sea levels,” says Richard Hindmarsh of the British Antarctic Survey, who did not participate in the study.
    This assumes that the grounding line does eventually stabilise, after much of PIG is gone. In reality, PIG could disappear entirely, says Hindmarsh. “If Thwaite’s glacier, which sits alongside PIG, also retreats, PIG’s grounding line could retreat even further back to a second crest, causing sea levels to rise by 52 centimetres.” The model suggests Thwaite’s glacier has also passed its tipping point.

    …. and now comes a new report in Science that an undersea ridge that may have once helped slow the loss of the Pine Island glacier is no longer doing so…

    Antarctic Glacier Off Its Leash

    An unmanned autonomous submarine has discovered a sea-floor ridge that may have been the last hope for stopping the now-accelerating retreat of the Pine Island Glacier, a crumbling keystone of the West Antarctic Ice Sheet, researchers announced at the fall meeting of the American Geophysical Union.
    An unmanned autonomous submarine has discovered a sea-floor ridge that may have been the last hope for stopping the now-accelerating retreat of the Pine Island Glacier, a crumbling keystone of the West Antarctic Ice Sheet. The ridge appears to have once protected the glacier, but no more. The submarine found the glacier floating well off the ridge and warmer, ice-melting water passing over the ridge and farther under the ice. And no survey, underwater or airborne, has found another such glacier-preserving obstacle for the next 250 kilometers landward.
    The Pine Island and adjacent Thwaites glaciers are key to the fate of West Antarctic ice, says glaciologist Richard Alley of Pennsylvania State University, University Park, in an e-mail. And West Antarctica is key to how fast and far sea level will rise in a warming world. “To a policymaker, I suspect that the continuing list of [such] ice-sheet surprises is not reassuring,” he writes.
    At the meeting, glaciologist Adrian Jenkins of the British Antarctic Survey in Cambridge and colleagues described how the instrument-laden Autosub3 cruised for 94 hours along 510 kilometers of track beneath the floating portion of the Pine Island Glacier in January 2009. The sub found a 300-meter-high ridge across the ocean cavity formed by the floating end of the glacier. Deep, warmer water was overtopping the ridge and passing through the gap between floating ice and the ridge top on its way to melting back more of the glacier. That gap has been growing, Jenkins said, perhaps since the 1970s. An aerial photograph from 1973 shows a bump in the ice where the ridge is now known to be, suggesting that the ice was then resting on the ridge and no warmer water could have been getting through.
    Although the last physical obstacle to continued melting and retreat of the Pine Island Glacier has been breached, the ice’s fate remains murky, says glaciologist David Holland of New York University in New York City. That’s because glaciologists aren’t sure what got the glacial retreat started in the first place, he notes. It wasn’t the greenhouse simply warming the ocean, researchers agree. Instead, shifting winds around Antarctica in recent decades may have driven warmer waters up to the ice and dislodged it from its perch on the ridge. But what caused the winds to shift? Global warming? The ozone hole? Random variability? Glaciologists—and policymakers—would like to know.

    … which makes Fred Pearce’s prediction (which we quoted in Climate Code Red two years ago, page 47) look spot on….

    Another vulnerable place on the West Antarctic ice sheet is Pine Island Bay, where two large glaciers, Pine Island and Thwaites, drain about 40 per cent of the ice sheet into the sea. The glaciers are responding to rapid melting of their ice shelves and their rate of fl ow has doubled, whilst the rate of mass loss of ice from their catchment has now tripled. NASA glaciologist Eric Rignot has studied the Pine Island glacier, and his work has led climate writer Fred Pearce to conclude that ‘the glacier is primed for runaway destruction’. Pearce also notes the work of Terry Hughes of the University of Maine, who says that the collapse of the Pine Island and Thwaites glaciers — already the biggest causes of global sea-level rises — could destabilise the whole of the West Antarctic ice sheet. Pearce is also swayed by geologist Richard Alley, who says there is ‘a possibility that the West Antarctic ice sheet could collapse and raise sea levels by 6 yards [5.5 metres]’, this century.

    So much for 0.8 metres being a risk-averse foundation for sea-level rise planning and policy-making.
    And for a fuller discussion on the current research on PIG and recent observations, there is a great overview, Is Pine Island Glacier the Weak Underbelly of the West Antarctic Ice Sheet?” at RealClimate, from November 2009.

    David Spratt
    24 January 2010

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  • ‘Critical decade’ for climate risks in Australia, world sea levels

    ‘Critical decade’ for climate risks in Australia, world sea levels

    TEXT SIZE bigger text smaller text

    2013-07-09


    A rise in sea levels and greater frequency of heavy rain will have an impact on property and infrastructure in Australia and around the world, according to a recent report from the country’s Climate Commission Secretariat.

    Critical decade for Australia climate risks

    “Climate change is likely to affect much of Australia’s infrastructure, including commercial and residential buildings, utilities (such as energy and water services) and transportation systems, in a variety of ways,” according to the report, dubbed “The Critical Decade 2013: Climate change science, risks and responses.”

    The report noted that the global average sea level is rising by 3cm every 10 years and will contribute to an increase in coastal flooding around the world.

    “Rainfall patterns are shifting,” according to the report, written by professors Will Steffen and Professor Lesley Hughes. “The southwest corner of Western Australia and much of eastern Australia has become drier since 1970. The southwest and southeast corners of Australia are likely to remain drier than the long-term average or become even drier.”

    Steffen is a researcher at the Australian National University, Canberra and Hughes is an ecologist in the Department of Biological Sciences at Macquarie University.

    Climate change impact on New South Wales

    They noted that in some regions of the world, there is “high confidence that the intensity and frequency of heavy precipitation are likely to increase.” Those regions include northern Europe, Alaska, northwest and east Canada, Greenland, Iceland, east Africa and northern Asia and central Europe in winter.

    Quoting from earlier Climate Commission Secretariat reports, the authors noted that in Australia, the combined value of commercial, light industrial, transport and residential buildings at risk from a sea-level rise of 1.1 metres is about 226 billion Australian dollars.

    “Much of Australia’s commercial buildings, industrial facilities, airports, ports, hospitals, schools, roads and railways and many residential buildings are in close proximity to the coast, putting much property and infrastructure at risk from sea-level rise.”

    The report added there an increased risk of” extreme fire weather” in some parts of Australia, “especially the populous southeast.”

     2
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  • ACTION ALERT – It’s time to protect Antarctica​’s Southern Ocean!

    ACTION ALERT – It’s time to protect Antarctica​’s Southern Ocean!

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    Stephen Campbell steve@antarcticocean.org via createsend4.com
    6:22 PM (1 hour ago)

    to me
    10,000 species need your help!

    Antarctic Ocean Alliance

    SHARE THIS EMAIL

    Dear NEVILLE,

    As you read this leaders from 25 countries are converging on a small seaside town in Germany to decide the fate of Antarctica’s Southern Ocean – behind closed doors.

    Wonder what these decision makers are up to right now? Making phone calls? Having dinner in a hotel restaurant? For sure, they are discussing whether or not to say YES to protect the last pristine ocean wilderness left on earth.

    These decision makers, who are part of CCAMLR, are meeting this week in Bremerhaven to discuss two key proposals for Antarctic marine protection, one for the Ross Sea, and one for East Antarctica. Either of them would see the creation of the world’s largest marine sanctuary.

    With your help, we’re going to make sure they know the world is watching their meeting. Tomorrow, Thursday 11 July, we’re going to project your Twitter messages from all points of the earth onto a wall at the meeting, calling for the protection of these waters.

    Here’s how to send them your message:

    1. Use the hashtag #AntarcticOcean in a tweet to decision makers calling on them to protect Antarctica’s Southern Ocean.

    2. Head straight to the Twitter wall website and click on the #AntarcticOcean hashtag, sign into your Twitter account and hit send.

    3. Use our suggested tweets you can send from here.

    Don’t have Twitter?

    Email key decision makers directly through visiting our new interactive infographic here. Click on all the countries that are ‘critical to success’ and send an email calling on them to make history this year by protecting Antarctica’s ocean.

    Have you seen our new video?

    Screen Shot 2013-07-10 at 9.01.02 AM

    If not click on the picture above or watch it here and share it with your friends to see the beauty that’s at stake in the Southern Ocean.

    It’s time to get busy Watchers!

     

    Thanks for your support
    The AOA Team
    FOLLOW THE CAMPAIGN:      
    Antarctic Ocean Alliance
    info@antarcticocean.org
    SIGN THE PETITION

    You’re receiving this email because you signed the petition to protect Antarctica’s waters with AOA or a partner.
  • Kuwait is one of the world’s top producers and net exporters of oil.

    Last Updated: July 8, 2013  (Notes)

    full report

    Overview

    Kuwait is one of the world’s top producers and net exporters of oil.

    As a member of the Organization of the Petroleum Exporting Countries (OPEC), Kuwait was the world’s 10th largest oil producer in 2012. Despite having the second smallest land area among the OPEC member countries, Kuwait exports the third largest volume of oil. Kuwait’s economy is heavily dependent on petroleum export revenues, accounting for nearly half of its gross domestic product and nearly 70 percent of export revenues. EIA estimates these revenues were 75 billion dollars in 2012. Kuwait should remain one of the world’s top oil producers as the country pushes towards a target of 4 million barrels per day (bbl/d) of production capacity by 2020.

    In an effort to diversify its oil-heavy economy, Kuwait has expanded efforts to develop its non-associated natural gas fields, which remain a small portion of its natural gas production. Greater production of gas can provide fuel for electricity generation which frequently falls short during periods of peak electricity demand.

    Energy policy is set by the Supreme Petroleum Council, overseen by the Ministry of Petroleum, and executed by The Kuwait Petroleum Corporation and its various subsidiaries. In addition, Kuwait has an active sovereign-wealth fund, the Kuwait Investment Authority, which oversees all state expenditures and international investments. Despite, Kuwait’s constitutional ban on foreign ownership of its resources, the government has taken measures to increase foreign participation in the oil and gas sectors. Kuwait is a constitutional emirate led by the Emir of Kuwait, a hereditary seat led by the Al-Sabah family. The Prime Minister and his deputy and council of ministers are approved by the Emir.

    Map of Kuwait

    Oil

    Kuwait holds the world’s sixth largest oil reserves and is one of the top ten global producers and exporters of total petroleum liquids.

    According to Oil & Gas Journal, as of January 2013, Kuwait’s territorial boundaries contained an estimated 102 billion barrels of proven oil reserves, roughly 6 percent of the world total. Kuwait ranked sixth in terms of oil reserves among all countries in 2012. Additional reserves are held in the Partitioned Neutral Zone (PNZ), which Kuwait shares on a 50-50 basis with Saudi Arabia. The Neutral Zone holds an additional 5 billion barrels of proven reserves, bringing Kuwait’s total oil reserves to 104 billion barrels.

    Graph showing the countries with the top proven oil reserves for 2013

    Sector organization

    Kuwait Petroleum Corporation, Kuwait’s national oil company, and its subsidiaries controls the entire oil sector from upstream to downstream and exports.

    The government of Kuwait owns and controls all development of the oil sector. The Supreme Petroleum Council (SPC) oversees Kuwait’s oil sector and sets oil policy. The SPC is headed by the Prime Minister. The rest of the council is made up of six ministers and six representatives from the private sector, all of whom serve three-year terms, and are selected by the Emir. The Ministry of Petroleum supervises all aspects of policy implementation in the upstream and downstream portions of both the oil and natural gas sectors.

    The Kuwait Petroleum Corporation (KPC) manages domestic and foreign oil investments. Kuwait Oil Company (KOC), the upstream subsidiary of KPC, was taken over by the Kuwaiti government in 1975 and manages all upstream development in the oil and gas sectors. The Kuwait National Petroleum Company (KNPC) controls the downstream sector, while the Petrochemical Industries Company (PIC) is in charge of the petrochemical sector. Export operations are overseen by both KNPC and the Kuwait Oil Tanker Company (KOTC). Foreign interests of KPC are handled by the Kuwait Foreign Petroleum Exploration Company (Kufpec), and international upstream development and downstream operations are controlled by Kuwait Petroleum International (KPI). Finally, Kuwait Energy Company (KEC) is a privately-held company that has developed a number of foreign interests over the past decade, including interests in Yemen, Egypt, Russia, Pakistan, and Oman.

    The Partitioned Neutral Zone (PNZ) has its own managing companies, separated by onshore and offshore activities. The onshore sector was developed by American Independent Oil Company (Aminoil), which was nationalized in 1977. Getty Oil, which would eventually be subsumed by Chevron, was brought in to develop onshore PNZ fields Wafra, South Umm Gudair, and Humma. Chevron remains a participant along with KPC, although management of all KPC PNZ interests has been transferred to the Kuwait Gulf Oil Company (KGOC). Offshore, a Japanese company, the Arabian Oil Company (AOC) discovered Khafji, Hout, Lulu, and Dorra oil fields in the 1960s. The concessions with Saudi Arabia and Kuwait expired in 2000 and 2002, respectively. KGOC was established in 2002 to oversee the offshore operations for KPC. Subsequently, KGOC, along with Aramco Gulf Operations Company (AOGC), set up a joint operating company, Al-Khafji Joint Operations Company (KJO), which manages offshore PNZ production.

    Map of oil fields in Kuwait Source: Kuwait Oil Company (KOC)

    Exploration and production

    Kuwait has implemented enhanced oil recovery measures to boost stagnant production rates. New discoveries have been made, but Kuwait’s regulated oil sector hinders further exploration and production.

    In 2012, Kuwait’s total oil production was approximately 2.8 million barrels per day (bbl/d), including its share of approximately 250,000 bbl/d of oil production from the PNZ. Of the country’s 2012 production, approximately 2.6 million bbl/d was crude oil and 200,000 bbl/d was non-crude liquids. Slightly over half of Kuwaiti crude production in 2011 came from the southeast of the country, largely from the Burgan field. Production from the north has increased to approximately 650,000 bbl/d according to KOC. In early 2011, as one of the few OPEC members with spare capacity, Kuwait increased oil production to compensate for the loss of Libyan supplies.

    Because of a greatly debated constitutional ban on foreign ownership of Kuwait’s natural resources, domestic production of Kuwait’s fields have stalled. Discoveries of lighter crudes in the center of the country have been successful, but progress has not moved beyond the planning stages. In 1984, a discovery was made in South Maqwa, revealing light crude of API 35° to 40° grade, and after drilling began at Kra’a al-Mara in 1990, significant volumes of 49° API crude were found. Negotiations began with ExxonMobil, but the conditions to move this project to full development have not been reached. Another successful discovery was made in 2006 in the Sabriya and Umm Niqa areas, in the north of the country, which added an estimated 20 to 25 billion barrels of reserves, although mostly of a heavier, sour quality.

    In a plan to circumvent the constitutional ban, international oil companies (IOCs) were allowed involvement through Enhanced Technical Service Agreements (ETSA). Royal Dutch Shell, in February 2010, signed an ETSA to exploit these new discoveries; however, progress has been slow in boosting production. KOC is also having trouble developing the Lower Fars reservoir of al-Ratqa field. KOC initially negotiated with ExxonMobil, Shell, and Total to develop this field, but KOC subsequently abandoned plans for a joint project development. KPC also signed a memorandum of understanding (MOU) in July 2010 with Japan Oil, Gas, and Metals National Corporation (JOGMEC) to assess the feasibility of injection of carbon dioxide as a potential enhanced oil recovery (EOR) technique.

    KPC announced a $100-billion capital spending plan over five years encompassing both the upstream and the downstream sectors. Included are plans to upgrade Kuwait’s production and export infrastructure and its tanker fleet, expand exploration, and build downstream facilities, both domestically and abroad. This effort is expected to boost total oil production capacity to 4 million bbl/d by 2020, and it is projected that the production capacity would be maintained through 2030. In order to achieve its 2020 target, IOC investment and participation will be necessary.

    Much of Kuwait’s reserves and production are concentrated in a few mature oil fields discovered in the 1930s and 1950s. The Greater Burgan oil field, which comprises the Burgan, Magwa, and Ahmadi reservoirs, makes up the dominant portion of both reserves and production. Burgan is widely considered the world’s second largest oil field, surpassed only by Saudi Arabia’s Ghawar field. Greater Burgan was discovered in 1938, but it did not become fully developed until after World War II. Burgan has been producing consistently since production first began. Generally, production from Burgan is medium to light crudes, with API gravities in the 28° to 36° range. Although Burgan’s recent production of between 1.1 and 1.3 million bbl/d accounted for about half of Kuwait’s total production, Burgan could be further developed to produce as much as 1.7 million bbl/d. KOC is seeking to boost Burgan’s capacity largely from the Wara reservoir through water injection recovery methods.

    Other production centers in the south of the country include Umm Gudair, Minagish, and Abduliyah. Umm Gudair and Minagish produce a variety of crude oil grades, which largely fall in the medium range, with gravities of 22° to 34° API.

    In January 2003, water injection began at Minagish to enhance oil recovery and offset natural production declines. In 2009, an exploration well drilled discovered light crude and associated natural gas at the Mutriba oil field to the west of Rudhatain. As much as 80,000 bbl/d are expected from this field, with plans for production coming on-stream by 2014.

    Northern Kuwait holds the majority of Kuwait’s larger fields other than Greater Burgan. Kuwait’s second largest source of crude production is from the northern Raudhatain field, with a capacity of 350,000 to 400,000 bbl/d. Sabriya field is adjacent to Raudhatain and adds another 100,000 bbl/d. The frontier fields of al-Ratqa, the southern extension of Iraq’s Rumaila structure, and the smaller Abdali field were both obtained after the new border was established in 1993 following the end of the Persian Gulf War. They add another 75,000 bbl/d of production capacity. In August 2010, British Petrofac signed a deal with KOC to boost production capacity at Raudhatain and neighboring Sabriyah fields. In the same month, Kuwaiti and Iraqi officials agreed in principle to jointly develop shared oil fields, as well as to allow IOCs to aid in such projects.

    Project Kuwait

    In an otherwise nationalized oil sector, Project Kuwait attempts to incentivize foreign investment to bring production capacity to 4 million bbl/d by 2020.

    A focal point of Kuwait’s aspirations to attain a production capacity of 4 million bbl/d is Project Kuwait. Proposed in 1998, Project Kuwait was a concerted effort to create proper incentives to attract foreign participation. The contract structure that resulted was challenged as unconstitutional and the National Assembly has impeded progress of Project Kuwait for a number of years. Kuwait’s constitution bars foreign ownership of the country’s natural resources, which precludes the product-sharing agreements (PSAs) that provide the desired incentive for IOC investment. In order to allow IOC involvement, an “incentivized buy-back contract” (IBBC) arrangement was created, which neither involves production sharing nor concessions.

    The structure of the IBBC agreements allows the Kuwaiti government to retain full ownership of oil reserves, control over oil production levels, and strategic management of the ventures. Foreign firms are to be paid a “per barrel” fee, along with allowances for capital recovery and incentive fees for increasing reserves. In May 2007, the Kuwaiti ruling family conceded the responsibility to approve each related IBBC for Project Kuwait to the National Assembly, which has caused further delays. Additionally, more performance-based incentives have been introduced in an ETSA structure, although only one has been awarded so far.

    Project Kuwait aims to increase the country’s oil production capacity from four northern oil fields (Raudhatain, Sabriya, al-Ratqa, and Abdali) and targets 1 million bbl/d of output from the fields by 2015. This serves as a pivotal component to increase overall oil production capacity to 3.5 million bbl/d by 2015, and 4 million bbl/d by 2020, which KOC admits will require the help of IOCs. Some agreements, such as the ETSA with Royal Dutch Shell forged in February 2010 and continued negotiations with other IOCs over EOR developments have enhanced prospects for foreign participation, yet no other final agreements have been made. Production from the northern fields is expected to rise with the installation of a 165,000 bbl/d early production center at the Sabriya field.

    Heavy oil is also a major long-term component of Project Kuwait, providing a projected 60,000 bbl/d by 2016 and 270,000 bbl/d by 2020, although this is much lower than the original forecast production of 750,000 bbl/d. Estimated heavy oil reserves of approximately 13 billion barrels are located primarily in the north of Kuwait, with other reserves concentrated in the PNZ.

    An unconventional source of potential production will come from the clean-up of the large pools of crude that have remained since the withdrawal of the Iraqi army after the Persian Gulf War. The KOC has awarded tenders to HERA Company of Spain, GS Engineering and Construction Corporation of South Korea, and TERI Company of India in February 2012 to aid in soil remediation, which could result in significant crude volumes. The entire operation will take a number of years and cost roughly $3.5 billion, paid for by the UN reparations fund; however, the first phase involves only three sites. During the Persian Gulf War, the Iraqi army set more than 800 wells ablaze and estimates indicate that as much as 5 million bbl/d were lost over the nine months it took to extinguish the fires, which resulted in the creation of thousands of crude oil lakes. Additionally, the crude lakes restrict access to producing areas and known reserves, which further restricts exploration and production.

    Partitioned Neutral Zone

    Territorial dispute between Kuwait and Saudi Arabia led to the creation of the Partitioned Neutral Zone. Both countries divide equally the production of oil and gas in the zone.

    The Partitioned Neutral Zone (PNZ) was established in 1922 to settle a territorial dispute between Kuwait and Saudi Arabia. The PNZ encompasses a 6,200 square-mile area and contains an estimated 5 billion barrels of oil and 1 trillion cubic feet (Tcf) of natural gas. Oil production capacity in the PNZ is currently about 600,000 bbl/d, all of which is divided equally between Saudi Arabia and Kuwait.

    Onshore production in the PNZ centers on the Wafra oil field, which began producing oil in 1954. Wafra is the largest of the PNZ’s onshore fields with approximately 3.4 billion in proven and probable reserves. Wafra has related production facilities and gathering centers with South Umm Gudair and South Fuwaris. Onshore production in the PNZ has a capacity of 240,000 bbl/d, but it is in decline. A full-field steam injection project led by Chevron is under development to offset field declines and boost production by over 80,000 bbl/d. The anticipated project is set to start in 2017.

    The production capacity of offshore fields in the PNZ is 350,000 bbl/d, with plans to double production to 700,000 bbl/d by 2019. Nearly 90 percent of current offshore production comes from Khafji. Offshore production is about four times as expensive in the PNZ as in the rest of Kuwait. Production offshore originates from Khafji, an extension of Saudi Arabia’s Safaniyah (the world’s largest offshore field); Hout, which is also an extension of Safaniyah; and Dorra, an extension of Iran’s Arash and shared with Saudi Arabia. Dorra is not currently under production, pending resolution of boundary demarcation negotiations and plans for joint development between Kuwait and Iran.

    Graph showing Kuwait's oil production and consumption for 1987-2012

    Exports and consumption

    Kuwait’s domestic consumption has been increasing, but a majority of its production heads to Asia.

    In 2012, Kuwaiti net exports of total liquids were estimated at 2.4 million bbl/d, making Kuwait the third largest exporter of total liquids among OPEC producers behind Saudi Arabia and Iran. Most Kuwaiti crude oil is sold on term contracts. Kuwait’s crude exports are a single blend of all its crude types. The largest proportion is the medium Burgan crude, which is blended with heavier, sour crude from northern fields, as well as marginal amounts from Minagish and Umm Gudair. Kuwait’s single export blend (“Kuwait Export”) has a specific gravity of 31.4°API (a typical medium Mideast crude), and is generally considered sour, with 2.52 percent sulfur content. In 2011, the Asia-Pacific region received approximately 1.5 million bbl/d of crude oil, while exports to the United States totaled 191,000 bbl/d, and Europe received around 80,000 bbl/d.

    With the majority of its export volumes headed to Asian markets, the most significant price benchmark for Kuwaiti exports is Dubai or Oman or a combination of both, to which oil exports are priced at a slight discount. As of the beginning of 2010, the price of Kuwaiti crude oil for U.S. customers was tied to the Argus Sour Crude Index (ASCI), a weighted average of various North American medium, sour crudes. European buyers purchase from a benchmark linked between a Brent weighted-average and Saudi Arab Medium.

    Mina al-Ahmadi is the country’s main port for the export of crude oil. Kuwait also has operational oil export terminals at Mina Abdullah, Shuaiba, and at Mina Saud, otherwise known as Mina al-Zour. Increased production generated by Iraq and the northern fields has necessitated the construction of a new terminal on Bubiyan Island. This terminal is still in the planning stages.

    Kuwait consumes only a small portion of its total petroleum production. The country consumed a total of 406,000 bbl/d in 2012, leaving the vast majority of its production available for exports. However, domestic consumption has been steadily increasing, partially as a result of increased petroleum-fired electricity generation.

    Refining

    Kuwait maintains refining and marketing interests in Europe and looks to expand into Asia, particularly China, Vietnam, and Indonesia.

    Oil & Gas Journal reports nameplate refining capacity in Kuwait at 936,000 bbl/d, the third-largest capacity in the Middle East. This production capacity is derived from three refinery complexes: al-Ahmadi, Abdullah, and al-Shuaiba. All of the refineries are located near the coastline, about 30 miles south of Kuwait City and are owned and operated by Kuwait National Petroleum Company (KNPC). The largest refinery, Mina al-Ahmadi, was built in 1949 and has a capacity of 466,000 bbl/d. Mina Abdullah and al-Shuaiba have nameplate capacities of 270,000 bbl/d and 200,000 bbl/d, respectively.

    Kuwait Petroleum International (KPI), also known as Q8, manages KPC’s refining and marketing operations internationally. Its operations include approximately 4,000 retail stations across Belgium, Spain, Sweden, Luxembourg, and Italy. KPI has interests in two refineries, owning an 80,000 bbl/d refinery in Rotterdam, Netherlands and a 50-50 joint venture with Italian major ENI in the 240,000 bbl/d capacity refinery in Milazzo, Italy.

    Kuwait is seeking to cultivate downstream interests in markets with high potential demand growth, the Asian market in particular, specifically China, Vietnam, and Indonesia. In China’s Guangdong Province, KPC is negotiating a refinery and petrochemical joint venture with China’s Sinopec, with a remaining stake allocated to Total. The plant will feature a 300,000 bbl/d capacity refinery, which will also have an ethylene steam cracker with the capacity to produce 1 million tons per year (mtpa) of ethylene and its derivatives. In March 2011, China’s National Development and Reform Commission (NDRC) gave final approval to the project, making Kuwait the second Arab oil producer behind Saudi Arabia to have a major downstream facility in China. Sinopec has announced a planned commission date of 2014; however, analysts predict a much longer timeframe, with a likely start-up in 2018-2019. Kuwait aims to increase its exports from 200,000 bbl/d to 500,000 bbl/d with the completion of the refinery.

    Kuwait Petroleum International (KPI) joined with PetroVietnam and Japanese Idemitsu in April 2008 to construct a 200,000 bbl/d refinery in Nhi Son, Vietnam. In November 2010, the Vietnamese government approved the project, with an expected completion date of 2014. KPI currently holds a 35-percent stake, which will be reduced for PetroVietnam to take a majority stake once the refinery comes online. Indonesian officials have also announced a possible $8-9 billion, 300,000 bbl/d refinery with KPC on the island of Java.

    Clean Fuels Project and Al-Zour

    In June 2011, Kuwait’s Supreme Petroleum Council approved two long-delayed projects: the Clean Fuels Project and the al-Zour refining facility. These two ambitious projects have an estimated combined cost of over $31 billion and come at a time of increasing domestic demand, especially in the petrochemical sector, and for higher quality products in Kuwait’s traditional export markets.

    The Clean Fuels Project (CFP) will upgrade Kuwait’s existing refineries. The planned overhaul of Kuwait’s refining sector includes building a new al-Zour refinery, shutting down the al-Shuaiba refinery, and retiring old units and installing new components at the remaining refineries. A crude distillation unit will be taken out of commission at the Mina al-Ahmadi, while Mina Abdullah will lose a number of components, but its overall capacity will increase by 184,000 bbl/d.

    The al-Zour refinery was originally put out for bids in 2008, but political opposition led to the cancellation of the bid round. This opposition forced KPC to compensate those companies who had spent resources preparing their bids, placing the entire project on hold. KNPC received the final approvals necessary to develop the Al-Zour project in 2012 and plans to re-tender contracts. The new refinery is expected to add another 615,000 bbl/d of capacity by 2018.

    Kuwaiti refineries and expansion plans
    Facility Current capacity
    (bbl/d)
    Planned capacity
    (bbl/d)
    Mina al-Ahmadi 466,000 346,000
    Mina Abdullah 270,000 454,000
    Al-Shuaiba 200,000 N/A
    Al-Zour N/A 615,000
    Total Capacity 936,000 1,415,000
    Source: Middle East Economic Survey, Middle East Economic Digest

    Natural gas

    Kuwait has recently become a net importer of natural gas, leading the country to focus more on natural gas exploration and development for domestic consumption.

    According to Oil & Gas Journal, as of January 2013, Kuwait had an estimated 63 Tcf of proven natural gas reserves. Natural gas reserves have remained at the same level since 2006. Kuwait’s intent to diversify its economy has spurred an extensive drive in natural gas exploration. Vast discoveries of non-associated gas in the north of the country attracted interest from IOCs; however, contract structures and political uncertainty remain principal impediments to any rapid expansion of both reserves and production. Additionally, new discoveries are geologically more complex, mainly tight and sour gas deposits that require more sophisticated and costly development.

    Sector organization

    Kuwait’s gas sector is also managed by the Kuwait Petroleum Corporation.

    As in the oil sector, all of the natural gas resources are owned by the Kuwait Petroleum Corporation (KPC). The Kuwaiti constitution prohibits any use of production-sharing agreements (PSAs) that allow for an equity stake by an IOC in development projects. Therefore, Kuwait is using technical service agreements (TSAs) in order to bring in IOCs to develop more difficult projects. In February 2010, Royal Dutch Shell signed an ETSA for the 2006 natural gas discoveries in the north, known as the Jurassic fields, which contains 35 Tcf of reserves in place, the nature of which are too sour for local firms to develop.

    Graph showing Kuwait's natural gas production and consumption for 2001-2011

    Exploration and production

    Kuwait plans to increase gas production to 4 billion cubic feet per day by 2030 in efforts to satisfy domestic consumption and decrease imports of LNG.

    In 2011, Kuwait produced 1.3 billion cubic feet per day (Bcf/d) of natural gas. This volume was an increase of around 15 percent compared with 2010. Given the predominance of associated natural gas in Kuwaiti production, domestic natural gas supplies increased at a small rate as a result of lower OPEC crude production quotas. Kuwait requires increasing supplies of natural gas for the generation of electricity, water desalination, and petrochemicals, as well as increased use for enhanced oil recovery (EOR) techniques to boost oil production. Kuwait is shifting its exploration drive to focus on natural gas discoveries to mitigate imports of liquefied natural gas (LNG) and decrease the proportion of oil used domestically, particularly for electricity and desalination plants. KOC has announced a production target of 4 Bcf/d by 2030, about four times the current production level.

    Associated natural gas production makes up the vast majority of Kuwait’s overall production. In 2010, approximately 1 billion cubic feet per day (Bcf/d) was produced from associated gas, while non-associated gas production amounted to only 150-200 million cubic feet per day (MMcf/d). Production of non-associated natural gas from the north is seen as the most promising future source of natural gas production growth. Given Kuwait’s fiscal and political climate, not much progress has been made in exploring the mainly offshore prospects, leaving Kuwait to focus on its natural gas discoveries in the north. KPC intends to produce about 400 MMcf/d of non-associated gas by 2020.

    The Jurassic non-associated gas field was discovered in 2006, with an estimated 35 Tcf of reserves. This project has been described as the most difficult in the world, based on the geologic composition and the technical complexities it presents. A first phase envisioned 175 MMcf/d of natural gas and 50,000 bbl/d of condensate production by 2008; however, it seems to have reached a production plateau at 140 MMcf/d. The second phase is being constructed by Kharufi National and Saipem, with a projected capacity of 500 MMcf/d due to come online by 2013. Original development plans of Jurassic forecast production of 600 MMcf/d by 2012 and 1 Bcf/d and 350,000 bbl/d of light crude or condensate, by 2015, although industry experts see the 2015 target date as unlikely. Royal Dutch Shell has been developing the Jurassic project through its 2010 ETSA.

    The other prospect for non-associated natural gas production is the Dorra gas field offshore PNZ. This field is shared by Kuwait, Saudi Arabia, and Iran, which calls the field Arash. Kuwait and Saudi Arabia have already announced plans to begin production at Dorra by 2017, providing an additional 500-800 MMcf/d. Iran, in response, has indicated that it will develop its own side of the field in the near future. Political tensions between the Gulf States and Iran are likely to preclude any near-term settlement of mutual development.

    Kuwait is also expanding its gas processing infrastructure to meet rising domestic demand. Daelim of South Korea is currently constructing Kuwait’s fourth and largest gas processing plant with 800 MMcf/d of capacity. This unit will be on the site of the Ahmadi refinery and give Kuwait a gas processing capacity of 2.3 Bcf/d by 2013. A fifth train of an additional 800 MMcf/d is also in the planning stages, taking potential capacity over 3 Bcf/d. However, neither the current production plans nor the expansion of processing facilities is expected to meet the growing levels of domestic demand.

    Consumption and imports

    In 2011, Kuwait consumed approximately 502 Bcf of natural gas, which is equal to 1.4 Bcf/d. Since 2009, Kuwait has consumed more natural gas than it has produced, compounding the problem of electricity outages by making the availability of feedstock uncertain. In 2011, Kuwait imported about 245 MMcf/d of LNG, largely from Qatar and Nigeria. Kuwait’s electricity demand, fueled increasingly by natural gas, has outpaced natural gas production during the summer months, resulting in the shutdown of refinery and petrochemical operations to meet the increased demand of electricity. As such, Kuwait has resorted to importing LNG to make up for this supply gap.

    In June 2009, Kuwait signed a deal with Royal Dutch Shell to import LNG, receiving the first cargo in August 2009. KPC made another deal with the international energy trading firm, Vitol, in April 2010, which will supply Kuwait with LNG cargoes through 2013. Kuwait takes delivery of the LNG at the Persian Gulf’s first regasification terminal, Mina al-Ahmadi GasPort, a floating facility that has the flexibility to supply LNG to Kuwait during its periods of high seasonal demand. The regasification capacity of al-Ahmadi is approximately 500 MMcf/d of LNG.

    Kuwait has also recently exhibited interest in supplies from the impending natural gas project in Southern Iraq. Royal Dutch Shell, Mitsubishi, and Iraqi state-owned Southern Oil Company (SOC) are developing infrastructure to gather associated natural gas from Iraq’s southern oil fields. A potential pipeline from Iran’s South Pars gas field has been placed on hold, as political considerations make the project less likely. These prospective pipeline imports would still not mitigate the need for continued LNG imports.

    Electricity

    Kuwait’s electric sector capacity has been extremely slow to expand despite rapidly rising consumption rates over the past decade and persistent power shortages during peak demand periods.

    Kuwait relies on fossil fuels, oil and natural gas, to supply its electricity generation needs. The country struggles to produce and import sufficient natural gas to meet peak demand, and as a result, depends on more expensive fuel oil. In 2011, Kuwait had an installed electric generation capacity of 13.5 gigawatts (GW) and generated electricity at a 46-percent capacity factor, resulting in an average output of 6.3 GW. According to IHS, peak demand for 2010 was 10.5 GW and has increased every year since 2008. The rate of growth of generation is not keeping up with the rate of growth of demand, which means electricity is not flowing to the consumers as fast as the capability is built.

    Kuwait has come to embody the difficulties facing the region’s electricity networks, with rapid demand growth causing rolling blackouts at times of peak energy demand. Slow implementation of development plans rooted in the political infighting between the Emir and the National Assembly, as well as a lack of natural gas feedstock, has created chronic shortages in electricity supply during the hot summer months. Formerly having one of the largest reserve margins in the region, Kuwait is perpetually in a state of electricity supply shortage and experiences frequent blackouts and brownouts each summer. In the past decade, the development of Kuwait’s electricity sector has stalled because of political factors and lack of investment, despite average annual demand growth of 6 percent. Only one power plant was commissioned during that time, bringing a comfortable reserve margin to a shortage beginning in 2006. According to the World Bank, Kuwait was the world’s third largest electricity consumer on a per capita basis in 2010.

    Given the rapidly increasing demand over the past decade, the Kuwaiti government has unveiled an extensive development plan for the electric grid. Kuwait is in the planning stages to bring on an additional power plant, Al-Zour North, with a generating capacity of 1.5 GW by 2015 and plans to nearly double its generation capacity by 2017 in an effort to meet an anticipated peak demand of 25 GW by 2025. Most of this planned capacity will come from natural gas or oil, although Kuwait aims to generate 10 percent of its electricity from renewable sources by 2020 through capitalizing on its potential wind and solar potential.

    In order to achieve this, Kuwait intends to employ more private capital through public-private projects (PPP), as well as independent water and power projects (IWPP). Kuwait is the last Gulf country to incorporate the private sector into the development of its electric sector. The first evidence of private sector participation is the expansion project of the al-Subiya power plant built by General Electric (GE) and Hyundai Heavy Industries of South Korea. In July 2012, GE and Hyundai completed the 700 MW expansion of the power plant to its nameplate capacity of 2,000 MW. The power plant is a combined-cycle facility, using natural gas primarily, with fuel oil as a back-up. It is the first new power plant to become operational in over 20 years and expected to add needed generation capability to the electric system. Five other power plants, including al-Zour North, are in various stages of development to achieve the forecast capacity and bring an adequate buffer between peak demand and generation capacity.

    Graph showing Kuwait's electricity generation for 2001-2011
    Kuwaiti planned power plants
    Project Generation
    capacity
    Plant type
    Al-Zour North 4,800 MW
    (4 Phases)
    Gas Turbine
    Al-Julaia 1,000 MW Gas Turbine
    Shuwakh 2,000 MW Gas Turbine
    Shuaiba South 1,400 MW Steam Turbine
    Doha East 2,300 MW Steam Turbine
    Total Capacity 11,500 MW
    Source: Ministry of Electricity and Water, Middle East Economic Survey, Middle East Economic Digest

    Nuclear power

    Kuwait began planning to use nuclear energy in 2009 and announced its intention to establish a nuclear commission. Subsequently, in January 2010, the head of the National Nuclear Energy Committee announced a 20-year cooperative deal with the French Atomic Energy Commission to develop nuclear power in Kuwait. Kuwait was considering four nuclear power plants, set to become operational by 2022 and agreed to allow International Atomic Energy Agency (IAEA) inspectors into any future nuclear sites. However, following Japan‘s Fukushima nuclear disaster in 2011, Kuwait dissolved its National Nuclear Energy Committee and decided to abandon its plans to produce nuclear power.

    Gulf Cooperation Council (GCC) grid

    Facing rising electricity demand, the Gulf Cooperation Council, comprised of six Gulf countries, is developing an interconnected power grid.

    The Gulf Cooperation Council (GCC), of which Kuwait is a member, faces rapidly increasing demand growth in electricity. As a result, the six Gulf countries of the United Arab Emirates (UAE), Kuwait, Qatar, Bahrain, Saudi Arabia, and Oman began a region-wide power grid. This three-phase project, completed in late 2012, connected the Northern System—Kuwait, Bahrain, Saudi Arabia, Qatar-to the Southern System— UAE, and Oman. Some analysts believe the GCC Grid has the potential to expand into North Africa and eventually link with Europe’s power grids. Kuwait has already had to import electricity from the Northern System, as it has been plagued by electricity supply shortfalls. In addition to meeting the growing electricity demands and sharing electricity reserve requirements in the Gulf States, the integrated power grids will reduce power outages in the short term and increase power exchange across seasons and time zones.

    Notes

    • Data presented in the text are the most recent available as of July 8, 2013.
    • Data are EIA estimates unless otherwise noted.

    Sources

    Agence France Presse

    APS Gas Market Trends

    APS Oil Market Trends

    APS Review Downstream Trends

    Arab Times

    Associated Press

    Business Monitor International

    Cambridge Energy Research Associates

    CIA World Factbook

    Dow Jones News Wire service

    Economist Intelligence Unit

    Energy Intelligence

    FACTS, Inc

    Financial Times

    Global Insight

    International Energy Agency

    Kuwait Petroleum International

    Kuwait Times

    Kuwaiti Foreign Petroleum Exploration Company

    Kuwaiti News Agency

    Middle East and Africa Oil and Gas Insights

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    World Oil

  • Scientists Image Vast Subglacial Water System Underpinning West Antarctica’s Thwaites Glacier

    Scientists Image Vast Subglacial Water System Underpinning West Antarctica’s Thwaites Glacier

    July 9, 2013 — In a development that will help predict potential sea level rise from the Antarctic ice sheet, scientists from The University of Texas at Austin’s Institute for Geophysics have used an innovation in radar analysis to accurately image the vast subglacial water system under West Antarctica’s Thwaites Glacier. They have detected a swamp-like canal system beneath the ice that is several times as large as Florida’s Everglades.


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    The findings, as described this week in the Proceedings of the National Academy of Sciences, use new observational techniques to address long-standing questions about subglacial water under Thwaites, a Florida-sized outlet glacier in the Amundsen Sea Embayment considered a key factor in projections of global sea level rise. On its own, Thwaites contains enough fresh water to raise oceans by about a meter, and it is a critical gateway to the majority of West Antarctica’s potential sea level contribution of about 5 meters.

    The new observations suggest the dynamics of the subglacial water system may be as important as well recognized ocean influences in predicting the fate of Thwaites Glacier.

    Without an accurate characterization of the bodies of water deep under Thwaites, scientists have offered competing theories about their existence and organization, especially in the rapidly changing region where the glacier meets the ocean.

    Using an innovation in airborne ice-penetrating radar analysis developed by lead author Dusty Schroeder, a doctoral candidate at the Institute for Geophysics, the Texas team shows that Thwaites’ subglacial water system consists of a swamp-like canal system several times as large as Florida’s Everglades lying under the deep interior of the ice sheet, shifting to a series of mainly stream-like channels downstream as the glacier approaches the ocean.

    Scientists have attempted to use ice-penetrating radar to characterize subglacial water for many years, but technical challenges related to the effects of ice temperature on radar made it difficult to confirm the extent and organization of these water systems. Schroeder’s technique looking at the geometry of reflections solves this problem, because the temperature of the ice does not affect the angular distribution of radar energy.

    “Looking from side angles, we found that distributed patches of water had a radar signature that was reliably distinct from stream-like channels,” said Schroeder. He compared the radar signature to light glinting off the surface of many small interconnected ponds when viewed out of an airplane window.

    Distinguishing subglacial swamps from streams is important because of their contrasting effect on the movement of glacial ice. Swamp-like formations tend to lubricate the ice above them whereas streams, which conduct water more efficiently, are likely to cause the base of the ice to stick between the streams. (The effect is similar to the way rain grooves on a tire can help prevent a car from hydroplaning on a wet road.)

    As a result of this change in slipperiness, the glacier’s massive conveyor belt of ice piles up at the zone where the subglacial water system transitions from swamps to streams.

    This transition forms a stability point along a subglacial ridge that holds the massive glacier on the Antarctic continent.

    “This is where ocean and ice sheet are at war, on that sticking point, and eventually one of them is going to win,” said co-author Don Blankenship, a senior research scientist from the Institute for Geophysics.

    Observations of the subglacial stream-and-swamp dynamic and the sub-ice topography suggest that Thwaites Glacier is stable in the short term, holding its current position on the continent. However, the large pile of ice that has built up in the transition zone could rapidly collapse if undermined by the ocean warming or changes to the water system.

    “Like many systems, the ice can be stabilized until some external factor causes it to jump its stability point,” said Blankenship. “We now understand both how the water system is organized and where that dynamic is playing itself out. Our challenge is to begin to understand the timing and processes that will be involved when that stability is breached.”

    Current models predicting the fate of the glacier do not yet account for these dynamic, subglacial processes.

    The findings rely on radar data acquired during airborne geophysical surveys over West Antarctica by the Institute for Geophysics, with operational support from the National Science Foundation. The analysis was enabled through intensive supercomputing supported by the university’s Texas Advanced Computing Center.

    The research was funded through grants from the National Science Foundation and NASA, with additional support from both the Vetlesen Foundation and the Institute for Geophysics, which is a research unit of the university’s Jackson School of Geosciences.

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