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Updated 20 August, 2004

US National Assessment of
the Potential Consequences
of Climate Variability and Change
Educational Resources
Regional Paper: The Northeast

 
 

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Introduction

In this section...

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Camden, Maine

The Northeast evokes images that range from quaint villages of historical significance to intense congestion along one of our nation's most densely populated corridors. For this paper, the area is defined as including the six New England states and upstate New York (in the New England Regional Assessment - NERA), and portions of seven Mid-Atlantic states and the District of Columbia (in the Mid-Atlantic Assessment - MARA). [This description does not include the New York City metropolitan area (the Metro East Coast region-MEC), it is a separate region focused almost entirely on urban issues.]. The region is home to approximately 20% of the US population. This part of our nation includes a vast network of waterways, extensive shorelines, and a varied landscape. These provide great opportunities for water recreation, fishing, skiing, hiking, and the annual autumn tree color change that defines New England for so many.

The Northeast's economy and population are as diverse as its geography. Livelihoods are based on: service industries that depend heavily on communication networks and travel; the manufacture and transport of industrial goods and materials; recreation and tourism; agriculture; and resource extraction - forestry, fisheries, and mining. The populations that live and work in the Northeast, especially those in major metropolitan areas, are ethnically, racially, and economically diverse - a characteristic that is expected to continue to evolve.

Potential changes in the climate over the 21st century could affect many facets of life in the Northeast, particularly those that are currently sensitive to climate. For example, climate change is likely to have direct impacts on agriculture, forestry, fishing, tourism, and outdoor recreation such as skiing. Human health is also likely to be effected, because changes in climate could aggravate existing health stresses and those posed by pollutants emitted here or carried by the winds from other regions. In coastal areas, infrastructure (the institutions, facilities, and services available to a community) is likely to be affected by climate-induced rise in sea level. Other potential concerns include impacts on the region's ecosystems, water supply and quality, commerce, and infrastructure (including energy sources and transportation systems).

Weather and Climate

Distinguishing clearly between the terms weather and climate is important to understanding how to interpret the results of this section. Weather is the hour-to-hour and day-to-day state of the atmosphere: whether, at a particular time, it is rainy or sunny, warm or cold, windy or calm. Climate is the average weather over time: a locale's typical weather patterns, including frequency and intensity of storms, cold outbreaks, and heat waves.

Just as the weather varies naturally, the climate varies naturally in response to such factors as sunspots, volcano eruptions, and atmosphere-ocean interactions (e.g., El Niño events). Climate change is a shift in the climate that lasts a few decades or more. Human activities in the last two centuries have become important drivers of climatic change. For this paper, whether the cause of an impact is natural or anthropogenic (human) is less important than whether it has to do with long-term trends or shorter patterns of variation. Thus we use more intuitive definitions: 1. variability refers to day-to-day, season-to-season, year-to-year, and decade-to-decade patterns of weather and climate; 2. climate change refers to longer-term trends in the average weather and climate, usually measured and experienced by long-term changes in temperature, precipitation, and sea level.

Historic Climate Trends

Diversity characterizes the Northeast's climate, with severe storms, winter blizzards, heat-waves, floods, and droughts. Over the past century, air temperatures have warmed as much as 4˚F along the coast from Chesapeake Bay to Maine. Precipitation (both rain and snow) has, depending on the location, increased from 4% - 20% since 1895. For the region as a whole, the average number of days with snow on the ground has decreased by over a week (7.5 days since 1953 for VT/NH/ME) over the last 50 years. Six of the last 40 years of the 20th century were characterized by significant drought in portions of the region. At the same time, precipitation extremes appear to be increasing and the land areas experiencing drought appear to be decreasing.

Global Warming or Climate Change

The media often uses the term global warming when talking about changes to the global climate. The phrase climate change, however, actually encompasses the more intricate set of changes that scientists are projecting. For example, the world is not expected to warm uniformly and some areas actually could become cooler as other parts of the Earth warm. Although more rain and snowfall are expected as the globe warms, some areas will become drier at the same time that other areas become wetter. The phrase climate change is, therefore, a more accurate way to describe projected changes to the global environment.

Possible Future Climates

Note about
General Circulation
Models

Global computer models, although imperfect at describing local conditions, suggest that the recently observed trends in climate that were described above will continue. These trends are expected to result in warmer winters and longer and hotter summertime conditions. Coastal regions and winter minimum temperatures are projected to undergo the greatest change, with warming from 4˚F to as much as 10˚F by 2100. Projections of changes in precipitation are less certain, with models estimating from 10 - 30% increases, primarily during the summer in New England.

Changes elsewhere are generally uncertain although most results indicate a larger percentage of precipitation is likely to come in heavy downpours. Coastal precipitation is likely to be variable, but increasing as well. Some models project more frequent occurrence of intense extreme weather events, while other models do not. If model projections of more frequent and intense extreme weather events were to occur, winter thaw events, flooding, and summer droughts would be more likely. Although the Northeast is considered ‘water rich' because of its high level of precipitation, drought has been and remains a significant concern for this region. Limited water storage, and large, aging water supply systems that are challenged to respond to changing water demands in the Northeast enhance the region's vulnerability to future drought or flooding episodes.

 

 

Temperature Change, 20th & 21st Centuries

The largest warming during the last century has occurred along the coastal region (as much as 4ºF).  Future model scenarios project relatively uniform increases in annually averaged temperatures. However, the Canadian model projects increases that are twice as large as the Hadley model.

 

Precipitation Change, 20th & 21st Centuries

Observed precipitation changes during the last century are a patchwork of moderate increases and decreases.  The Canadian model scenario for the next century indicates near neutral trends or modest increases, while the Hadley model projects increases of near 25% for the region.

 

 

Winter minimum temperatures, important for ski areas to maintain snowpack, warm substantially in both scenarios. Over much of the eastern seaboard, minimum temperatures increase by 4°F in the Hadley scenario and by more than 5°F in the Canadian scenario.

21st Century, Winter Minimum Temperature and July Heat Index Change

Summer heat index is expected to increase; the Hadley scenario shows greater than 3-5°F increase for much of the eastern seaboard while the Canadian scenario shows increases from 8°F to more than 10°F.

 

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