
Food & Water Watch
Fracking causes many public health and environmental problems and the last thing that Pennsylvanians need is another way for the oil and gas industry to capitalize on the Marcellus Shale at the expense of their health and well-being. But Governor Corbett lured the multinational oil and gas giant, Shell Oil Company into the state to do just that.
Corbett, who has received $1.8 million in campaign contributions from the oil and gas industry, forced through legislation in February 2012 that would exempt the company from property and corporate income taxes for 15 years if they build a petrochemical ethane cracker plant in the western part of the state. A cracker plant creates chemicals like ethylene, in this case from Marcellus Shale gas, to manufacture plastics and fertilizer.
Cracker plants are known to emit large amounts of toxic air pollution including nitrogen oxide and volatile organic compounds, which can contribute to ozone creation and increase airborne particulates. To date, approximately 44 total cracker plants exist in the U.S., mostly in Louisiana and Texas.
By March 2012, Shell announced that it selected a preferred site in Beaver County that is already home to a zinc smelting company, Horsehead Inc. Shell and Horsehead have drafted a land-option agreement and Shell has until June 2013 to decide whether or not it will purchase the property.
In June 2012, the Senate approved the proposed state budget for Fiscal Year 2012- 2013, and on July 2, 2012, the General Assembly signed into effect a Tax Code component, which included the Pennsylvania Resource Manufacturing Tax Credit, otherwise known as the “Cracker Credit.” Through the Corbett Administration’s own admission, the Cracker Credit, which goes into effect in 2017, “was part of the initial agreement Shell made with Pennsylvania this spring.” It will ultimately provide Shell Oil Company with up to $1.65 billion in tax credits over the next 25 years.
This deal was fast-tracked and the media pointed out that the tax deal was kept quiet. StateImpact reported, “When Governor Corbett announced in March that Shell was targeting Beaver County, he never mentioned a $1.65 billion tax break.”
Already there seems to be a lot of closed-door collaboration between decision makers, with little transparency or public involvement. In June 2012, the Pittsburgh Regional Alliance, a regional economic development organization, organized a tour to one of Shell’s cracker plants Louisiana. There were attendees from the Beaver County, Beaver County Corporation for Economic Development, Potter Township, Central Valley School District, Center Township, PA Governor’s Action Team and the Greater Pittsburgh Chamber of Commerce. Following the trip, the Pittsburgh Regional Alliance held “community education sessions” in Beaver County. These sessions appear to be the only opportunities for public participation in the process so far.
Although Shell will likely have to complete environmental and engineering assessments and studies, and garner appropriate permits, things seem to be moving forward. In a press release, Beaver County Commission Chairman, Tony Amadio said: “Over the next several months, we will be working closely with the other local governments to take the official steps that are part of the KOEZ application.” This is the application that if approved, would make the land tax exempt for Shell.
During fracking volatile organic compounds, including benzene and toluene, are released and can mix with nitrogen oxide emissions from diesel-fueled vehicles and equipment to form ground-level ozone. These emissions contribute to the enhanced greenhouse effect and climate change and air quality could conceivably worsen in the region if the plant is approved.
The company states that a project like this can be completed within a five-year timespan. Residents need to use this window as an opportunity to demand transparency and tell their elected officials that closed door sessions with Shell are not in the public’s best interest—that protecting the integrity of their health and air quality should be the priority.
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The speed and scale of the response to COVID-19 by governments, businesses and individuals seems to provide hope that we can react to the climate change crisis in a similarly decisive manner - but history tells us that humans do not react to slow-moving and distant threats.
A Game of Jenga
<p>Think of it as a game of Jenga and the planet's climate system as the tower. For generations, we have been slowly removing blocks. But at some point, we will remove a pivotal block, such as the collapse of one of the major global ocean circulation systems, for example the Atlantic Meridional Overturning Circulation (AMOC), that will cause all or part of the global climate system to fall into a planetary emergency.</p><p>But worse still, it could cause runaway damage: Where the tipping points form a domino-like cascade, where breaching one triggers breaches of others, creating an unstoppable shift to a radically and swiftly changing climate.</p><p>One of the most concerning tipping points is mass methane release. Methane can be found in deep freeze storage within permafrost and at the bottom of the deepest oceans in the form of methane hydrates. But rising sea and air temperatures are beginning to thaw these stores of methane.</p><p>This would release a powerful greenhouse gas into the atmosphere, 30-times more potent than carbon dioxide as a global warming agent. This would drastically increase temperatures and rush us towards the breach of other tipping points.</p><p>This could include the acceleration of ice thaw on all three of the globe's large, land-based ice sheets – Greenland, West Antarctica and the Wilkes Basin in East Antarctica. The potential collapse of the West Antarctic ice sheet is seen as a key tipping point, as its loss could eventually <a href="https://science.sciencemag.org/content/324/5929/901" target="_blank">raise global sea levels by 3.3 meters</a> with important regional variations.</p><p>More than that, we would be on the irreversible path to full land-ice melt, causing sea levels to rise by up to 30 meters, roughly at the rate of two meters per century, or maybe faster. Just look at the raised beaches around the world, at the last high stand of global sea level, at the end of the Pleistocene period around 120,0000 years ago, to see the evidence of such a warm world, which was just 2°C warmer than the present day.</p>Cutting Off Circulation
<p>As well as devastating low-lying and coastal areas around the world, melting polar ice could set off another tipping point: a disablement to the AMOC.</p><p>This circulation system drives a northward flow of warm, salty water on the upper layers of the ocean from the tropics to the northeast Atlantic region, and a southward flow of cold water deep in the ocean.</p><p>The ocean conveyor belt has a major effect on the climate, seasonal cycles and temperature in western and northern Europe. It means the region is warmer than other areas of similar latitude.</p><p>But melting ice from the Greenland ice sheet could threaten the AMOC system. It would dilute the salty sea water in the north Atlantic, making the water lighter and less able or unable to sink. This would slow the engine that drives this ocean circulation.</p><p><a href="https://www.carbonbrief.org/atlantic-conveyor-belt-has-slowed-15-per-cent-since-mid-twentieth-century" target="_blank">Recent research</a> suggests the AMOC has already weakened by around 15% since the middle of the 20th century. If this continues, it could have a major impact on the climate of the northern hemisphere, but particularly Europe. It may even lead to the <a href="https://ore.exeter.ac.uk/repository/handle/10871/39731?show=full" target="_blank" rel="noopener noreferrer">cessation of arable farming</a> in the UK, for instance.</p><p>It may also reduce rainfall over the Amazon basin, impact the monsoon systems in Asia and, by bringing warm waters into the Southern Ocean, further destabilize ice in Antarctica and accelerate global sea level rise.</p>The Atlantic Meridional Overturning Circulation has a major effect on the climate. Praetorius (2018)
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