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  • Have your say before the 22nd of November

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    Have your say before the 22nd of November

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    Coal Terminal Action Group via email.nationbuilder.com
    2:26 PM (27 minutes ago)

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    Coal Terminal Action Group

    The Preferred Project Report (PPR) for the proposed fourth coal terminal (T4) in Newcastle is open for public comment until the end of this week. Can you make a submission right now on the PPR on T4, it will only take a few minutes of your time and you can make a real difference!

    Have your say before the 22nd of November

     
    Port Waratah Coal Services have said there is no immediate need for another coal terminal in Newcastle, and yet they are pushing ahead to get Government approval for their controversial “T4” coal terminal. They have produced a ‘Preferred Project Report’ (PPR), which is supposed to respond to the submissions we all made about the air pollution, noise, biodiversity, traffic, and toxics impacts of the project.

    T4 will be reviewed by a Planning and Assessment Commission in coming months. We are urging community members and groups to participate actively in the PAC hearing.

    But before that, we need all our friends and supporters to make submissions on the PPR to the Department of Planning and Infrastructure to demonstrate why we are opposed to another coal terminal in our community and estuary!

    Closing date for submissions from the public is Friday, 22 November 2013.

     

    Here’s 10 good reasons to say ‘No’ to T4:

    [I object to this project and believe that the community health, environmental and socioeconomic impacts will have far outweighed any short-term benefits it is claimed it will deliver. These include:]

    1. Global warming: The burning of an additional 70Mt of coal a year will add 174.2Mt of carbon dioxide to the atmosphere. This is equal to 30% of Australia’s total annual GHG emissions. The International Energy Agency predicts that to limit global warming to under 2 degrees Celsius, global coal demand must peak in 2016, at least a year before PWCS indicates T4’s will begin operation.
    2. The Hunter Estuary supports 112 species of waterbirds and nationally and internationally listed threatened species, including the Australasian bittern (Botaurus poiciloptilus), listed as endangered under the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act).
    3. Deep and Swan Ponds: The Project will wipe out 80% of Deep Pond, which supports at least 11 species of migratory recorded and above the threshold of 0.1 per cent of the Australian flyway population for three migratory shorebird species, and will develop part of Swan Pond which supports three species in numbers that exceed the threshold of 0.1 per cent of the Australian flyway population.
    4. Misuse of public conservation lands: Swan Pond is public land, owned and managed by the National Parks Service under Part 11 of the NSW National Parks and Wildlife Act. It is part of a highly successful long-term restoration project, the Kooragang Wetland Rehabilitation Project (KWRP) and has been the site of significant hours of volunteer labour by the local bird watching club.
    5. Air quality: Newcastle and the Hunter Valley communities are impacted by dust from the mining, transport and stockpiling of coal. An additional 70Mt of coal exported will mean about an additional 7000 trips of 80 wagon trains between the Hunter mines and the port and back again per year, the capacity to export coal from an additional 8 to 10 mega mines and four new 1.5km coal stockpiles will substantially add to PM10 emissions in Newcastle and the Hunter Valley.
    6. Air quality modelling flaws: PWCS’s air quality modelling continues to use 2010 as a base year. NSW Health has suggested that PWCS should have included “a justification for assuming the PM10 levels in 2010 would be a realistic baseline for modelling future particulate levels or alternatively use, as a baseline, average levels over a longer period of time”.  This recommendation is ignored in the PPR.
    7. Particle pollution from rail transport: The PPR does not address air quality issues from rail transport returning to the Upper Hunter Valley. PWCS continues to focus on air quality impacts within 20m of the rail corridor, but there are almost 30,000 people living within 500m of the rail corridor and 23,000 students attend 16 schools in that vicinity. The submission to the EA by NSW Health noted that the contribution of coal dust from coal trains beyond 20m from the rail corridor needs to be carefully considered, but this recommendation is ignored.
    8. Justification for the project: There is no justification for the project. PWCS does not commit to building T4 and only suggests an indicative build date of 2015 with operation maybe in 2017.  During a major downturn in global coal demand, Newcastle’s approved coal export port capacity of 211Mt seems optimistic. Last year only 141Mt of coal was exported meaning 60Mt or 42 per cent of capacity was uninstalled.
    9. Employment:  The 120 Mt facility proposed in the EA identified no additional employment would result from its operation. The revised T4 project of 70Mt million of the RT/PPR is identified as employing 80 additional people. How is this possible? This dubious additional employment is not explained.
    10. Economics: PWCS’s claimed economic benefits to the region are based on a type of economic modelling the Australian Bureau of Statistics calls “biased” and the Productivity Commission says is regularly “abused”, usually to overstate the economic importance of specific projects. The original economic assessment of the T4 project suggests its annual operating costs will only be between $45-50 million a year.  Since that assessment was made, the size of the project has “almost halved”, so the amount of money it will “inject” into the economy has presumably declined considerably. For the terminal to achieve its economic potential, a lot more coal has to be dug up and exported. This means that a lot more bush and agricultural land needs to be turned into coal mines. A lot more coal trains need to pass through Newcastle’s suburbs. At the site of the proposal, a significant wetland would have to be destroyed.  And, of course, the extra coal being burned would contribute to climate change. None of these costs are considered in the economic assessment commissioned by PWCS. (Read Rod Campbell’s economic analysis here.)

    If you made a submission on the Environmental Assessment of T4, we encourage you to read the response to submissions and see if PWCS have addressed your concerns. We do not think they have addressed ours.

    Thank you for your continued support,
  • Griffith by-election 2014

    Griffith by-election 2014

    Likely by-election date
    With the vacancy arising barely five weeks before Christmas, it is not possible to have a by-election this year. Generally it is considered to be undesirable to hold a by-election during the summer holidays, so the by-election will likely take place in February or March 2014.

    Cause of by-election
    Former Prime Minister Kevin Rudd announced his resignation from Parliament and retirement from politics on Wednesday 13 November 2013, after losing power at the September 2013 federal election.

    Read the profile for the seat of Griffith at the 2013 federal election.

    Margin – ALP 3.0%

    Geography
    Southern Brisbane. Griffith covers the suburbs of Brisbane on the south side of the Brisbane river across the river from the Brisbane CBD, including South Brisbane itself, as well as Greenslopes, Holland Park, Kangaroo Point, East Brisbane, Coorparoo, Carina, Seven Hills, Morningside, Balmoral and Bulimba.

    History
    Griffith was created for the 1934 election, replacing the original seat of Oxley which was abolished at that election. Both Oxley and Griffith have been marginal seats, with Griffith swinging back and forth regularly between the Liberal Party and the ALP since 1949, although this has not usually coincided with national changes. The seat has become relatively safe for the ALP since it was won by Kevin Rudd in 1998.

    The seat was first won in 1934 by Labor MP Francis Baker, who had previously won the seat of Oxley off the United Australia Party, ironically at an election when the UAP swept away the federal Labor government.

    Baker was re-elected in 1937, but was killed in a car accident in 1939 at the age of 36. Ironically his father was elected to federal parliament in Maranoa in 1940, after his son’s term in Parliament.

    The 1939 Griffith by-election was won by Labor candidate William Conelan. Conelan held the seat until he lost Griffith to Liberal candidate Douglas Berry in 1949.

    Berry was re-elected in 1951 but lost to the ALP’s Wilfred Coutts. Coutts held on in 1955 but failed to win re-election in 1958, losing to the Liberal Party’s Arthur Chresby, and winning it back in 1961.

    Coutts lost the seat once again in 1966, when the seat was won by Liberal candidate Donald Cameron. Cameron held the seat for eleven years, moving to the new seat of Fadden in 1977. He held Fadden until his defeat in 1983, and returned to Parliament at the 1983 Moreton by-election, which he held until his retirement in 1990.

    The ALP regained Griffith in 1977, with Ben Humphreys winning the seat. Humphreys served as a minister in the Hawke/Keating government from 1987 until 1993, and retired at the 1996 election.

    The ALP preselected Kevin Rudd, but he lost to Graeme McDougall (LIB). McDougall only held on for one term, losing to Rudd in 1998. Rudd joined the ALP shadow ministry in 2001 as Shadow Minister for Foreign Affairs, a role he held for five years.

    Rudd’s profile rose as Shadow Foreign Minister, and he was considered a contender for the ALP leadership when Simon Crean resigned in 2003 and when Mark Latham resigned in 2005, but he waited until late 2006 when he challenged Kim Beazley, and was elected leader, and then proceeded to win the 2007 federal election, becoming Prime Minister.

    Kevin Rudd was removed as Labor leader and Prime Minister in June 2010, and was re-elected in Griffith as a Labor backbencher. He returned to the ministry as Foreign Minister following the election. He returned to the backbench as part of a failed challenge to Julia Gillard’s leadership in February 2012.

    Kevin Rudd defeated Julia Gillard to regain the Labor leadership in June 2013, and led the ALP to defeat at the 2013 federal election.

    Candidates
    Possible Labor candidates include local state MP Di Farmer, local councillor Shayne Sutton and lawyer Terri Butler. The Liberal National Party is expected to run former AMA President Bill Glasson, who ran for the seat in 2013. The Greens are again running 2013 candidate Geoff Ebbs.

    Assessment
    Governments, even new governments, don’t usually gain seats off an opposition.

    Kevin Rudd has always had a strong personal vote, and the loss of that vote could see Glasson gain even more ground in an area where he has a very high profile.

    It is quite easy to see a scenario where Labor loses, but the LNP may not perform as strongly in its new position in government.

    2013 result

    Candidate Party Votes % Swing
    Kevin Rudd ALP 36,481 42.22 +6.42
    Bill Glasson LNP 34,878 40.36 -3.72
    Geoff Ebbs GRN 8,799 10.18 -5.21
    Karin Hunter PUP 2,903 3.36 +3.36
    Greg Sowden IND 705 0.82 +0.82
    Adam Kertesz FF 643 0.74 -0.71
    Luke Murray KAP 595 0.69 +0.69
    Anne Reid SEC 445 0.51 +0.51
    Sherrilyn Church RUA 418 0.48 +0.48
    Liam Flenady SA 377 0.44 +0.44
    Jan McNicol SPP 165 0.19 +0.19

    2013 two-candidate-preferred result

    Candidate Party Votes % Swing
    Kevin Rudd ALP 45,805 53.01 -5.45
    Bill Glasson LNP 40,604 46.99 +5.45

    Polling places in Griffith at the 2013 federal election. Bulimba in green, East in red, Greenslopes in blue, South Brisbane in yellow. Click to enlarge.

    Polling places in Griffith at the 2013 federal election. Bulimba in green, East in red, Greenslopes in blue, South Brisbane in yellow. Click to enlarge.

    Booth breakdown
    Booths have been divided into four areas. Bulimba in the north, Greenslopes in the south, South Brisbane in the west and a series of booths along the eastern boundary.

    The ALP won a majority in three areas, ranging from 54% in the east to just under 60% in South Brisbane. The LNP won a slim majority in Bulimba. The ALP suffered a swing in all four areas, ranging from 2.6% in South Brisbane to 6.6% in Bulimba.

    The Greens vote varies widely, from 6% in the east and 7% in Bulimba up to almost 17% in South Brisbane.

    Voter group GRN % ALP 2PP % ALP swing Total votes % of votes
    Bulimba 7.10 49.42 -6.63 19,116 22.12
    Greenslopes 10.15 54.85 -3.67 18,880 21.85
    South Brisbane 16.93 59.74 -2.62 12,686 14.68
    East 6.21 54.07 -4.28 7,772 8.99
    Other votes 10.35 50.87 -7.45 27,955 32.35

    Two-party-preferred votes in Griffith at the 2013 federal election.

    Two-party-preferred votes in Griffith at the 2013 federal election.

    Greens primary votes in Griffith at the 2013 federal election.

  • Ocean Acidification Summary for Policymakers 2013


    • Nov 14, 2013

      Expert assessment:

      Ocean acidification may increase 170% this century with substantial costs expect…

    • Urban air pollution:
      a new look at an old problem

      Large urban agglomerations inevitably lead to air pollution. But despite the significant impacts on human health and climate, we lack systematic measurements of air pollution in many cities. Megan L Melamed, Tong Zhu and Liisa Jalkanen discuss a new global assessment that illuminates the knowns and unknowns.

    • What to do while the water rises?

      Rising sea levels will eventually threaten many coastal cities. But a dominant focus on the long-term endgame should not unduly restrict our options to deal with the more immediate consequences of climate change, says Richard Little .

    Published: November 14, 2013

    Ocean Acidification Summary for Policymakers 2013

    This summary for policymakers reports on the state of scientific knowledge on ocean acidification, based on the latest research presented at The Third Symposium on the Ocean in a High-CO2 World, held in Monterey, California, in September 2012. Experts present the projected changes from ocean acidification for ecosystems and the people who rely on them, according to levels of confidence for these outcomes.

    Ocean Acidification Summary for Policymakers
    Third Symposium on the Ocean in a High-CO2 World

    Download the full pdf.

    A3 size high resolution jpg of pH infographic (4.7mb)

    A3 size high resolution jpg of Aragonite infographic (4.4mb)

     

    Download the summary here, as well as the infographics that illustrate the problems that ecosystems and humans face as ocean acidification increases over the next century. The summary addresses outcomes based on whether humans continue to emit carbon dioxide at current rates to the atmosphere, or what could happen if policymakers take action to mitigate these emissions.

    Ocean pH in 2100

    The average pH of ocean surface waters has fallen by about 0.1 units, from 8.2 to 8.1, since the beginning of the industrial revolution. This corresponds to a 26% increase in acidity. Please see original infographic for sources and further information.

    Ocean pH in 1850

    Compared with preindustrial levels shown here, the projected increase in ocean acidity is about 170% by 2100 if high CO2 emissions continue (RCP* 8.5).

    Atmospheric CO2 and ocean pH

    Observations of CO2 (parts per million) in the atmosphere and pH of surface seawater from Mauna Loa and Hawaii Ocean Time-series (HOT) Station Aloha, Hawaii, North Pacific.

    Credit: Adapted from Richard Feely (NOAA), Pieter Tans, NOAA/ESRL (www.esrl.noaa.gov/gmd/ccgg/trends) and Ralph Keeling, Scripps Institution of Oceanography (scrippsco2.ucsd.edu)

    Observed CO2 emissions and emissions scenarios to 2100

    Global CO2 emissions (white dots, uncertainty in grey) from fossil fuel use is following the high emissions trajectory (red line, RCP* 8.5) predicted to lead to a significantly warmer world. Large and sustained emissions reductions (blue line, RCP* 2.6) are required to increase the likelihood of remaining within the internationally agreed policy target of 2°C.

    Credit: Glen Peters and Robbie Andrew (CICERO) and the Global Carbon Project, adapted from Peters et al., 2013 (reference 8). Historic data from Carbon Dioxide Information Analysis Center.

    Ocean surface pH projections to 2100

    Modelled global sea-surface pH from 1870 to 2100. The blue line reflects estimated pH change resulting from very low CO2 emissions to the atmosphere (IPCC Representative Concentration Pathway, RCP* 2.6). The red line reflects pH from high CO2 emissions (the current emissions trajectory, RCP* 8.5).

    Credit: Adapted from Bopp et al., 2013 (reference 9).

    Aragonite saturation in 2100

    This map shows the “saturation state” for the mineral form of calcium carbonate called aragonite.

    If Ω is less than 1 (Ω<1), conditions are corrosive (undersaturated) for aragonite-based shells and skeletons. Coral growth benefits from Ω≥3.

    By 2100, computer model projections show that Ω will be less than 3 in surface waters around tropical reefs if CO2 emissions continue on the current trajectory.

    Aragonite saturation 1850-1860

    Aragonite saturation for surface ocean waters, at the beginning of the industrial revolution.


    • Global Change Magazine No. 81

      This issue’s cover story puts 2000 years of regional temperature histories into perspective. Also featured: two full-spread maps visualising the PAGES 2k regional temperature records and ocean acidifi…


    • Global Change Magazine No. 80

      The cover story in this issue explores the phenomenon of land grabs by taking a closer look at the Southeast Asian nation of Laos. Also featured are articles on resilience in the face of sea-level…

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  • New USGS Study on Chesapeake Bay: Groundwater Delaying the Effects of Some Water Quality Actions

    New USGS Study on Chesapeake Bay: Groundwater Delaying the Effects of Some Water Quality Actions
    Released: 11/12/2013 9:00:00 AM

    Contact Information:
    U.S. Department of the Interior, U.S. Geological Survey
    Office of Communications and Publishing
    12201 Sunrise Valley Dr, MS 119
    Reston, VA 20192
    Jon Campbell 1-click interview
    Phone: 703-648-4180

    Ward Sanford 1-click interview
    Phone: 703-648-5882

    New research by the U.S. Geological Survey conducted on the Delmarva Peninsula, which forms the Eastern Shore of the Chesapeake Bay, indicates it may take several decades for many water-quality management practices aimed at reducing nitrogen input to the Bay to achieve their full benefit due to the influence of groundwater.

    The USGS findings provide critical information on how long it may take to see the water quality in the Bay improve as more stringent practices are implemented to reduce nutrients and sediment to tidal waters.  Having established a calculation for the total nitrogen, phosphorus, and sediment pollutants that are allowable for the Chesapeake watershed, known as the total maximum daily load (TMDL), the U.S. Environmental Protection Agency (EPA) is working with Maryland, Pennsylvania, Virginia and the four other Bay watershed jurisdictions to ensure that all water-quality practices needed to reduce the flow of nutrients and sediment to the Bay are in place by 2025. 

    “This new understanding of how groundwater affects water-quality restoration in the Chesapeake Bay will help sharpen our focus as many agencies, organizations, and individuals work together to improve conditions for fish and wildlife,” said Lori Caramanian, Department of the Interior Deputy Assistant Secretary for Water and Science.  “In turn, improved environmental conditions will serve to further people’s enjoyment and promote the economic benefits of the Nation’s largest estuary.”

    The responses of watershed systems and ecosystems to environmental management actions at any location can vary from rapid changes (such as the swift beneficial effect of a wastewater treatment plant upgrade) to longer improvement intervals of several decades. In the Chesapeake Bay, “lag response time” refers to the time between implementing management actions and the resulting improvements in water quality. Lag times will vary for nitrogen, phosphorus, and sediment.

    This USGS study focused on nitrogen. Some of the nitrogen will run off directly into a stream, but a large portion on the Delmarva (more than two thirds) is affected by the slow travel times of nutrients moving from their land source through underground aquifers to a receiving stream or estuary.

    Sources of nitrogen include fertilizer and manure applications to agricultural land, wastewater and industrial discharges, runoff from urban areas, domestic septic drain fields, and air emissions. Excess nitrogen contributes to algal blooms that cause low dissolved oxygen in the Bay and related fish kills each summer and impact recreational activities.

    For this study USGS scientist Ward Sanford developed a complex model for water, geology, and chemical interactions that he applied to seven separate watersheds on the Delmarva Peninsula. Based on the concept of nitrogen mass-balance regression, the model was able to reproduce the time history of nitrate concentrations in area streams and wells, including a recent slowdown in the rate of concentration increase in streams. The model was then also used to forecast future nitrogen delivery from the Delmarva Peninsula to the Bay under different nitrogen management scenarios.

    The new study shows that ages of groundwater and associated nitrogen from the Delmarva Peninsula into the Chesapeake Bay range from less than a year to centuries, with median ages ranging from 20 to 40 years. These groundwater age distributions are markedly older than previously estimated for areas west and north of the Bay, which has a median age of 10 years. The older ages occur because the porous, sandy aquifers on the Delmarva yield longer groundwater return times than the fractured-rock areas of the Bay watershed.

    The USGS research found that in some areas of the Delmarva the groundwater currently discharging to streams is gradually transitioning to waters containing higher amounts of nitrate due to fertilizer used during the 1970s through the 1990s. Similarly, the total amount of nitrogen in the groundwater is continuing to rise as a result of the slow groundwater response times.

    Without additional management practices being implemented, the study forecasts about a 12% increase in nitrogen loads from the Delmarva to the Bay by 2050. The study provides several scenarios for reducing nitrogen to the water table and the amount of time needed to see the reductions in groundwater discharging to streams. For example, the model predicts that a 25% reduction in the nitrogen load to the water table will be required to have a 13% reduction in load to the bay.

    However, the results also indicate that nutrient management practices implemented over the past decade or so have begun to work and confirm that the amount of the nitrogen loading to streams in the future will depend on the rigor of water-quality practices implemented to reduce nutrients at present.

    This study highlights the complexities of environmental restoration of the Bay. The findings help refine the expectations of resource managers and citizens alike of how long it may take to see substantial water-quality improvements in the Bay, and they may provide additional insight into the effectiveness of different types of land management practices given the time lag created by local groundwater response times.

    The study was done as part of increased federal efforts under the President’s 2009 Chesapeake Executive Order, which directs Federal agencies, including the EPA and the Department of the Interior, to “begin a new era” in protection and restoration of the Chesapeake Bay. With a watershed that spreads across six states and Washington, DC, the Chesapeake Bay is the largest estuary in the United States and one of the largest and most biologically productive estuaries in the world.

    Learn more

    “Quantifying Groundwater’s Role in Delaying Improvements to Chesapeake Bay Water Quality,” Environmental Science & Technology

    USGS Chesapeake Bay Activities


    USGS provides science for a changing world. Visit USGS.gov, and follow us on Twitter @USGS and our other social media channels.
    Subscribe to our news releases via e-mail, RSS or Twitter.

    Links and contacts within this release are valid at the time of publication.

    ###
  • In the wake of the horror of Haiyan’s devastation, the Philippines government is desperately calling on the world to act urgently to help them now*

    On Thursday, 14 November 2013 2:21 AM, Iain Keith – Avaaz.org <avaaz@avaaz.org> wrote:
    Dear friends,

    Days after a climate induced typhoon devastated the Philippines, three countries are blocking progress on a deal that could stop global warming. The Philippines is desperately calling for urgent action, but Australia, Japan, and Poland are shamefully putting polluters profits before their responsibility to help stop superstorms. Let’s super-charge the Philippines call:

    In the wake of the horror of Haiyan’s devastation, the Philippines government is desperately calling on the world to act urgently to help them now* AND curb the next climate catastrophe. But shockingly three countries are blocking their heart wrenching appeal.

    Haiyan is a byproduct of climate change. Human pollution makes our planet hotter, the storms get more fierce, and the world’s poorest communities often suffer most. Right now a deal is being discussed to cut pollution and help finance vulnerable countries to meet this crisis. But three governments are obstructing negotiations and outrageously proposing to increase pollution: Australia, Japan, and Poland.

    Haiyan has built media and political pressure at the climate summit taking place right now. The Philippines’ delegate said ‘What my country is going through as a result of this extreme climate event is madness. The climate crisis is madness. We can stop this madness.’  Let’s build a million strong petition to back his call for urgent action. Sign now — let’s make sure these three countries put lives over polluters profits:

    http://www.avaaz.org/en/philippines_vs_polluters_1/?bBYMjdb&v=31036

    Haiyan is the latest in an alarming trend of freak weather events being driven by climate change. These events hit the poorest hardest because their communities are not set up to withstand them. But their scope is increasing and now richer countries like the US, Australia and some in the EU are feeling the brunt of a new climate reality.

    Tragically it has taken these disasters to kick life back into a stalling UN process to agree a climate deal. Governments have now agreed that 2015 is our last chance to get an agreement that can save our planet from a maelstrom of superstorms and disaster. The meeting this week in Warsaw is the most important global meeting this year to lay the groundwork for a deal. But Japan and Australia want to backtrack on their commitments to cut emissions, and Poland is blocking Europe’s ambitions.
    If, even in the wake of Haiyan, these countries do the opposite of what the world needs — our chances of success are grim. We’re in a 2 year race to save the world. Haiyan has given us a powerful reminder of what’s at stake. Let’s get behind the Philipines and stop the madness of Australia, Japan and Poland. Sign the petition now:

    http://www.avaaz.org/en/philippines_vs_polluters_1/?bBYMjdb&v=31036

    With more than 29 million members around the world — Avaaz is in a unique position to get behind the Filipino government and deliver a strong wake-up call to the negotiators in Warsaw. Together, we have influenced international summits, world leaders and our parliaments to get firm action on climate change — now out of the tragedy of Haiyan let’s demand countries start doing more.

    With hope,

    Iain, Alice, Pascal, Luis, Caroline and the entire Avaaz team

    PS: There are many ways to support the relief efforts for the victims of Cyclone Haiyan. Check out 350.org’s list of organisations: http://stories.350.org/donate-to-help-victims-of-typhoon-haiyan/?akid=3777.109376.nH0GMi&rd=1&t=1

    Sources:

    In hard-hit Tacloban, children ripped from arms (CNN)
    http://edition.cnn.com/2013/11/09/world/asia/philippines-tacloban/index.html

    Typhoon Haiyan: what really alarms Filipinos is the rich world ignoring climate change (The Guardian)
    http://www.theguardian.com/commentisfree/2013/nov/08/typhoon-haiyan-rich-ignore-climate-change

    Typhoon Haiyan influenced by climate change, scientists say (Sydney Morning Herald)
    http://www.smh.com.au/environment/climate-change/typhoon-haiyan-influenced-by-climate-change-scientists-say-20131111-2xb35.html

    Typhoon Haiyan: Philippines destruction ‘absolute bedlam’ (BBC)
    http://www.bbc.co.uk/news/world-asia-24894529

    Deadly Typhoon Haiyan Devastates the Philippines, Heads for Vietnam (TIME)
    http://world.time.com/2013/11/10/deadly-typhoon-haiyan-devastates-the-philippines-heads-for-vietnam/



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