Executive Summary
The pulse of life and economic activity across the Northeast is marked by the region’s dramatic seasonal cycle, changeable weather, and extreme events such as floods and nor’easters. This familiar climate is already changing in noticeable ways. Temperatures have been rising, particularly in winter, and the number of extremely hot days in summer has been increasing. Snow cover is decreasing and spring is arriving earlier in the year. Recent changes in our climate in the Northeast are consistent with those expected due to increasing levels of carbon dioxide and other heat-trapping gases in the atmosphere. These gases are released by the burning of fossil fuels and other human activities.
This study draws on recent advances in climate modeling to assess how global warming may further affect the Northeast’s climate. Using projections from three state-of-the-art global climate models, we compare the types and magnitude of climate changes that will result from higher emissions of heat-trapping gases versus lower emissions. The first scenario is a future where people— individuals, communities, businesses, states, and nations—allow emissions to continue growing rapidly, and the second is one in which society transitions onto a pathway of economic development with substantially lower emissions.
Over the next few decades, similar changes in climate are expected under either emissions scenario. For example, temperatures across the region are likely to rise by 2.5 to 4 degrees Fahrenheit (°F) in winter and 1 to 3°F in summer, regardless of the emissions during that period. These changes have already been set in motion by our emissions over the past few decades, but it takes years or decades for the climate to respond in noticeable ways.
By mid-century and later, however, most changes projected to occur depend strongly on the emissions choices we make in the near future and carry through the rest of the century. Specifically, under the higher-emissions scenario, in which the world remains on a pathway of highly fossil fuel- intensive economic growth (with heat-trapping emissions from automobiles, power plants, and industries continuing to increase through the end of the century), new projections for the Northeast show that:
• By the end of this century, winters could warm by 8 to 12°F and summers by 6 to 14°F.
• Historically, major cities in the Northeast experience 10 to 15 days per year when temperatures exceed 90°F. By mid-century, cities such as Philadelphia, New York City, and Boston could experience 30 to 60 days of temperatures over 90°F each summer. By late in the century, most cities in the region are likely to experience more than 60 days with temperatures over 90°F, including 14 to 28 days with temperatures over 100°F (compared with one or two days per year historically).
• As winter temperatures rise, more precipitation will fall as rain and less as snow. By the end of the century, the length of the winter snow season could be cut in half.
• The frequency of late summer and fall droughts is projected to increase significantly, with short- term droughts (lasting one to three months) becoming as frequent as once per year over much of the Northeast by the end of the century.
• The character of the seasons will change significantly, with spring arriving three weeks earlier by the end of the century, summer lengthening by about three weeks at both its beginning and end, fall becoming warmer and drier, and winter becoming shorter and milder.
• Sea-level rise will continue, reaching anywhere from a few inches to more than one foot by mid- century. By the end of the century, global sea level could rise from eight inches up to nearly three feet, increasing the risk of coastal flooding and damage from storm surges.
• Higher global temperatures also imply a greater risk of destabilizing the Greenland and West Antarctic ice sheets. It is possible, particularly under the higher-emissions scenario, that warming could reach a level during this century beyond which it would no longer be possible to avoid rapid ice sheet melting and a sea-level rise of more than 20 feet over the next few centuries.
In contrast, under the lower-emissions scenario, in which the world follows a pathway of high economic growth but shifts toward less fossil fuel-intensive industries and introduces clean and resource-efficient technologies, heat-trapping emissions would peak by about mid-century and then decline. New projections for this region show that smaller climate-related changes can be expected if the world follows the lower-emissions pathway—typically, about half the change expected under the higher-emissions scenario. In this case, projected changes for the region include:
• End-of-century temperature increases of 5 to 7.5°F in winter and 3 to 7°F in summer.
• An average of 30 rather than 60 days over 90°F for most cities in the region by the end of the century, and only a few days over 100°F.
• A 25 percent loss of the winter snow season.
• A likelihood of short-term drought only slightly higher than today.
• Arrival of spring one to two weeks earlier by century’s end; summer would arrive only one week earlier and extend a week and a half longer into the fall.
• Sea-level rise of a few inches to less than two feet by century’s end, reducing though not eliminating the risk of exceeding the warming threshold that would destabilize major ice sheets.
Under either emissions scenario, the Northeast of the future will be a tangibly different place. Additional future changes that do not show dramatic differences between scenarios include:
• Increases in the likelihood and severity of heavy rainfall events, including more than a 10 percent increase in the number of annual extreme rainfall events and a 20 percent increase in the maximum amount of rain that falls in a five-day period each year.
• Increases in winter precipitation on the order of 20 to 30 percent, with slightly greater increases under the higher-emissions scenario.
• A combination of higher temperatures, increased evaporation, expanded growing season, and other factors that will cause summer and fall to become drier, with extended periods of low streamflow. This will reduce the availability of water from northeastern rivers to natural ecosystems, agriculture, and other needs.
Although some changes are now unavoidable, the extent of change and the impact of these changes on the Northeast depend to a large degree on the emissions choices we in the Northeast and the world make today. The “higher” emissions scenario described here is not a ceiling on what our future emissions might be, but neither is the “lower” scenario a floor on the lowest emissions we can achieve. While actions to reduce emissions in the Northeast alone will not stabilize the climate, the region is a center of global leadership in technology, finance, and innovation. Ranked against the nations of the world, it is also the seventh largest source of carbon dioxide emissions from energy use. As such, the Northeast is well positioned to be a technology and policy leader in reducing emissions and driving the national and international progress essential to providing our children and grandchildren with a safe and stable future climate.