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By Erika Spanger-Siegfried
Today’s Emissions, Tomorrow’s Climate To determine the extent to which climate change could have an impact on this populous region, the Northeast Climate Impacts Assessment (NECIA), a collaboration between the Union of Concerned Scientists and a group of independent experts, used state-of-the-art climate models to project the future climate under higher-emission and lower-emission pathways. The findings indicate that the severity of future warming—and the quality of climate our children and grandchildren will inherit—depends on choices people in the Northeast and around the world make today: will we continue to rely heavily on fossil fuels, or will we transform our use of energy to be far more efficient and produce far less emissions? Some climate changes are inevitable because of the continued effect of past emissions that are still in the atmosphere. For example, current and past emissions will likely cause winter temperatures to rise an additional 4 ºF over the next few decades, while summer temperatures will rise an additional 1 to 3 ºF. But our choice between a higher- or lower-emission pathway leads to starkly different climate futures by mid-century and beyond. A higher-emission pathway, in which we continue to rely heavily on fossil fuels, could result in dramatic regional warming of 7 to 12 °F on average by the end of the century. To put such a change into perspective, a similar degree of cooling (compared with today’s temperatures) put the location of present-day New York City under a mile of ice. In short, the projected temperature increases could lead to a climate unrecognizable to current residents of the Northeast.
With the approach of winter, communities and businesses ready themselves for snow, ice, and the deep chill of the season. But despite the occasional hard winter, the season has softened its grip on the Northeast in the past few decades. Less precipitation has fallen as snow, the snow that does fall has become more “slushy” on average, and warmer temperatures have melted the snow more quickly. This warming is expected to continue across the region as a result of increased emissions. Under a higher-emission pathway, winter temperatures will rise between 4 and 7 °F by mid-century (2040–2069), and between 8 and 12 °F by the end of the century (2070–2099). If we choose a lower-emission pathway, the temperature rise will be significantly smaller (between 5 and 7.5 ºF by the end of the century). Winter precipitation is also expected to increase, but with higher temperatures this precipitation is more likely to take the form of rain than snow. In addition, the number of snow-covered days is projected to decline in all of the northeastern states under a higher-emission pathway—even in the historically snowy northern reaches of the region. This would fundamentally change the winter landscape (see the figure, "The Changing Face of Winter"). By contrast, lower emissions would result in significantly smaller reductions in snow-covered days.
Summertime in the Northeast is characterized by warm, often humid days, punctuated by occasional sweltering heat waves. But temperatures are on the rise, and the region faces dramatic increases in summer heat this century (see the sidebar “Summer in the City: No Picnic”) depending on the choices we make. If we stay on a higher-emission pathway we can expect distinctly hotter summer temperatures—between 4 and 8 ºF warmer by mid-century, and between 6 and nearly 14 °F warmer toward the end of the century. These increases are roughly double the change projected for a lower-emission pathway. Compounding the problem is humidity, as warm air can hold more moisture. When rising humidity is factored in, summer days in some states under a higher-emission scenario may feel as much as 20 °F warmer than today—on par with the current climate of the southeastern United States (see migrating climate map). Meeting the Challenge The higher-emission pathway explored here is by no means a ceiling; emissions could conceivably go even higher, driving even more dangerous climate change. But the lower-emission pathway is also not a floor; with strong, near-term action to reduce emissions we could further curtail the magnitude and effect of projected climate change.
The Northeast, as a global leader in technology, policy, finance, and innovation as well as a major source of carbon dioxide emissions (its energy-related emissions in 2001 were surpassed by only six nations), can set a leadership example in emission reduction. In fact, the Northeast has already taken a significant first step in the form of its Regional Greenhouse Gas Initiative (RGGI), the first multi-state cap on U.S. power plant emissions. And nearly all the states in the region have adopted California’s stringent emission standards for vehicles. Encouragingly, more decision makers appear to be listening to the science, understanding the implications, and readying for action than in years past (see the sidebar “A Message that Hits Home”). The new Congress is considering federal climate legislation, and a growing number of U.S. corporations have expressed support for national emission standards. The very character of the Northeast is at stake. Though the NECIA findings are sobering, they also present us with a question that can offer hope: which climate future are we, over the next few years, prepared to create? The choice is ours. Erika Spanger-Siegfried, Northeast climate project manager, wrote this article based on the work of several NECIA authors.
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