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A nor'easter (also northeaster; see below) is a type of macro-scale storm along the East Coast of the United States and Atlantic Canadamarker, so named because the winds come from the northeast, especially in the coastal areas of the Northeastern United States and Atlantic Canadamarker. More specifically, it describes a low pressure area whose center of rotation is just off the East Coast and whose leading winds in the left forward quadrant rotate onto land from the northeast. The precipitation pattern is similar to other extratropical storm. Nor'easters also can cause coastal flooding, coastal erosion, hurricane force winds, and heavy snow.Nor'easters can occur at any time of the year but are mostly known for their presence in the winter season.Nor'easters can be devastating and damaging, especially in the winter months, when most damage and deaths are cold related, as nor'easters are known for bringing extremely cold air down from the Arctic air mass. Nor'easters thrive on the converging air masses; that is, the polar cold air mass and the warmer ocean water of the Gulf Stream.

Geography and formation characteristics

Nor'easters form along the East Coast of the United States, usually in the months between October and April, although nor'easters can form any time of the year.When a nor'easter starts forming in the Gulf of Mexico, moist air and high dew points feed into the developing storm. The storm will then reach the Atlantic Oceanmarker and begin to strengthen. Some nor'easters will deepen rapidly in intensity, sometimes becoming as strong as moderate hurricanes by feeding on the warm waters of the Gulf Stream.

The sharp contrast in the cold Labrador current and the warm Gulf Stream, as well as the topographic nature of the Northeast, make the Mid-Atlantic and New Englandmarker coast one of the most conducive areas in the world for nor'easter formation. It is thought that nor'easters are caused by the Arctic oscillation, which is a band of air circulating at about 55°N. The Arctic oscillation has two phases: positive and negative. In the positive phase, the predominant phase for the past twenty years, the air moves quickly and acts almost like a dam in preventing the intrusion of Arctic air into the mid-latitude regions. In its negative phase, the air moves more slowly and is more subject to disruption. This allows cold Arctic air to penetrate into the mid-latitudes. There can be a fluctuation between positive phase and negative phase days over the course of a winter, and a correlation between negative phase days and nor'easters has been found.


Most Nor'easters start from a low-pressure system that forms in the south, most often the Gulf of Mexico, and are drawn across to the Northeast by the Jet Stream. The divergence or diffluence in the upper atmosphere caused by the Jet Stream removes and disperses the rising air at a faster rate than it is replaced at the surface, which, along with the Coriolis Effect, creates and develops a storm. Their northeast track brings them up along the East Coast past the mid-Atlantic and New England coastal states. The counterclockwise flow around a low pressure system brings the warm moist oceanic air over land. The warm moist air meets cold air carried southward by the trough. The deepening low enhances the surrounding pressure gradient, which acts to spiral the very different air masses toward each other at an even faster rate. The greater the temperature differences between the two air masses, the greater the turbulence and instability, and the more severe the storm can become. .

If the nor'easter takes the East Coast track, that usually indicates the presence of a high pressure area in the vicinity of Bermudamarker. The storm will then reach the North Carolinamarker coast and begin to develop. At this time, the nor'easter can move slightly offshore, which would be the more destructive path, or, it can move slightly inland, which would present mostly rain. If it takes the offshore path, it would begin to rapidly strengthen. Now, the effects would start reaching the major cities of the Northeast, such as New York Citymarker. The storm, now rapidly intensifying, tracks northward. These storms sometimes intensify during their entire existence. The storm moves northward, following the topography of the East Coast. It usually reaches its peak intensity while off the Canadian coastmarker. The storm then reaches Arctic areas, and can reach intensities equal to a strong hurricane. They then meander throughout the North Atlanticmarker and can last for several weeks.


Nor'easters are usually formed by an area of vorticity associated with an upper-level disturbance or from a kink in a frontal surface that causes a surface low pressure area to develop. Such storms very often are formed from the merging of several weaker storms, a "parent storm" and a polar jet stream mixing with the tropical jet stream.

Until the nor'easter passes, thick, dark, low-level clouds often block out the sun. During a single storm, the precipitation can range from a torrential downpour to a fine mist. Low temperatures and high wind gusts are also associated with a nor'easter. On very rare occasions, such as in the North American blizzard of 2006 and a nor'easter in 1979, the center of the storm can take on the circular shape more typical of a hurricane and have a small eye.All precipitation types can occur in a nor'easter, although they are well-known for their frozen precipitation.

Difference from tropical cyclones

Often, people mistake nor'easters for tropical cyclones and do not differentiate between the two weather systems. Nor'easters differ from tropical cyclones in that nor'easters are cold-core low-pressure systems, meaning that they thrive on cold air. Tropical cyclones are warm-core low-pressure systems, which means they thrive on warm temperatures.

Difference from other extratropical storms

Though a nor'easter is formed in a strong extratropical cyclone, which occurs in many places around the world, nor'easters are unique in the combination of northeast winds and moisture content of the swirling clouds. Close to similar conditions sometimes occur during winter in the Pacific Northeast (northern Japan and northwards) with winds from NW-N. In Europe, similar weather systems with such severity are hardly possible; the moisture content of the clouds is usually not high enough (to cause flooding or heavy snow), though NE winds can be strong.

Areas often affected

The northeastern United States, from Virginiamarker to the New Englandmarker coast, Quebecmarker and Atlantic Canadamarker could see nor'easters in some year, most often in the winter and early spring but also sometimes during the autumn. These storms can leave inches of rain or several inches or feet of snow on the region and sometimes last for several days.

The Atlantic coast, from northern Georgia northward up the coast, can suffer high winds, pounding surf, and extremely heavy rains during these storms. However, swells have been known to cause damage through the Caribbean as well. Surfers wait in anticipation when a nor'easter is formed. Nor'easters cause a significant amount of severe beach erosion in these areas, as well as flooding in the associated low-lying areas. Beach residents in these areas may actually fear the repeated depredations of nor'easters over those of hurricanes, because nor'easters happen more frequently and cause substantial damage to beach-front property and their dunes. Nor'easters are often mistaken for Euroclydon, but these are two separate weather patterns. A Euroclydon is a tempestuous northeast wind that blows in the Mediterranean.


Usually nor'easters bring massive amount of precipitation, high winds, large waves, and marginal storm surge to coastal areas. Depending on the circumstances and the time of year, nor'easters can bring rain, ice, and snow. Ice, snow, and high winds can shut down major airports for days leaving thousands stranded. Ice and snow can also shut down major highways and interstates leaving motorists unable to reach their destinations. During nor'easters, many people lose power because of high winds, ice, and snow.

"Nor'easter" usage and origins

Compass card (1607)
The term "nor'easter" comes to American English by way of British English. According to the Oxford English Dictionary (OED), the first recorded use in the English language of the term "nore" ("north") in association with the points of the compass and wind direction is by Dekker in 1612 ("How blowes the winde Syr?" "Wynde! is Nore-Nore-West."), with similar uses occurring in 1688 (". . . Nore and Nore-West . . .") and in 1718 (". . . Nore-west or Nore-nore-west."). These recorded uses are predated by use of the term "noreast," first recorded as used by Davis in 1594 ("Noreast by North raiseth a degree in sayling 24 leagues.") and shown, for instance, on a compass card published in 1607. Thus, the manner of pronouncing from memory the 32 points of the compass, known in maritime training as "boxing the compass", is described by Ansted with pronunciations "Nor'east (or west)," "Nor' Nor'-east (or west)," "Nor'east b' east (or west)," and so forth. According to the OED, the first recorded use of the term "nor'easter" occurs in 1836 in a translation of Aristophanes. The term "nor'easter" naturally developed from the historical spellings and pronunciations of the compass points and the direction of wind or sailing.

As noted in a January 2006 editorial by William Sisson, editor of Soundings magazine, use of "nor'easter" to describe the storm system is common along the U.S. East Coast. Yet, it has been asserted by linguist Mark Liberman (see below) that "nor'easter" as a contraction for "northeaster" has no basis in regional New England dialect and is a "fake" word, which is a parochial view that neglects the little-known etymology and the historical maritime usage described above.

Nineteenth century Downeast mariners pronounced the compass point "north northeast" as "no'nuth-east," and so on. For decades, Edgar Comee, of Brunswick, Mainemarker, waged a determined battle against use of the term "nor’Easter" by the press, which usage he considered “a pretentious and altogether lamentable affectation” and "the odious, even loathsome, practice of landlubbers who would be seen as salty as the sea itself." His efforts, which included mailing hundreds of postcards, were profiled, just before his death at the age of 88, in The New Yorker.

Despite the efforts of Comee and others, use of the term continues by the press. According to Boston Globe writer Jan Freeman, "from 1975 to 1980, journalists used the nor'easter spelling only once in five mentions of such storms; in the past year (2003), more than 80 percent of northeasters were spelled nor'easter."

University of Pennsylvaniamarker linguistics professor Mark Liberman has pointed out that while the OED cites examples dating back to 1837, they represent the contributions of a handful of non-New England poets and writers. Liberman posits that "nor’Easter" may have originally been a literary affectation, akin to "e'en" for "even" and "th'only" for "the only," which is an indication in spelling that two syllables count for only one position in metered verse, with no implications for actual pronunciation.

Notable nor'easters

See also


  1. Ansted. A Dictionary of Sea Terms, Brown Son & Ferguson, Glasgow, 1933
  3. "Talk of the Town". The New Yorker, issue of 5 September 2005.
  4. Jan Freeman, "The Word". The Boston Globe, issue of 21 December 2003.
  5. Mark Liberman, "Nor'easter considered fake". Language Log, 25 January 2004.

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