Nor’Easter After Easter: After a Quiet Winter, an Unusual Storm
Videos, Tue, Jun 19th, 2012
In late-April 2011, an unusual, post-winter Nor’easter brought much-needed rain the Northeast United States.
Ned Gardiner, Climate Visualization Project Manager, NOAA Climate Program Office.
The Tropics provide a steady stream of clouds and storms that generally move east to west. In mid-latitudes weather moves west to east with some twists and turns due to Earth’s rotation. An important kind of storm moves north and east along the United States’ East Coast, especially in winter. People in the New England states call these “Nor’easters,” and they usually bring snow, rain, and driving wind. In late-April, an unusual, post-winter Nor’easter brought much-needed rain to an especially dry eastern United States.
To understand the climate connections driving Nor’easters, here are satellite loops that track the storm through late April.
A low pressure system developed off the coast of Florida on April 21 as light, warm moist air rose from the warm ocean surface. Warm water is a climate characteristic of the Gulf, the Caribbean, and the Gulf Stream which warms the entire East Coast before heading off towards northern Europe. Earth’s rotation interacts with the prevailing movement of air from west to east to spin these storms up and along the East Coast.
The difference in temperature between land which is cold, and the ocean which is warm, fuels driving rains. The ocean in this part of the world stays warm due to the Gulf Stream. The land is especially cold when Arctic air plunges southward. During winter, this temperature difference is more common, but notice how the polar jet stream dipped south of the Great Lakes on April 22.
The East Coast has been drier than normal so far this year, in part because winter didn’t bring any major Nor’easters. This map shows rainfall differences from average for January through April. The brown areas were drier than normal for this time of year.
Farmers are often the first to feel water shortages. In Maryland, some farmers lost their spinach crops and had to delay soy and corn planting because the soil was so dry. Farmers and residents in Delaware-Maryland-Virginia, Connecticut, Rhode Island, and Massachusetts have all delayed their Spring planting and have been conserving water.
This springtime storm made up for most of April’s rainfall deficit in a single event, dumping over 2″ along much of the Atlantic coast and between 4″ and 6″ in parts of Maine. Unfortunately, the year-to-date through April was still well below average, not only for the Mid-Atlantic and New England, but much of the United States.
Recapping the climate connections for a Nor’easter: warm ocean water fuels a low pressure system with moisture; Earth’s rotation moves that air mass in a counter-clockwise motion along the East Coast; and cold air from the North drives toward the storm’s center. That was the climate story for one strange Nor’easter after Easter.
For climate.gov, I’m Ned Gardiner.Nor'Easter After Easter: After a Quiet Winter, an Unusual Storm,
Spring 2013 has brought something fairly unusual in recent years—colder-than-average temperature for the nation as a whole. NOAA’s Deke Arndt talks about how spring temperatures in three U.S. climate divisions compare to the local long-term trend.
During late winter, Texas, Oklahoma, and Kansas received sorely needed rain which helped reduce short-term impacts, like wildfire and dry topsoil. But it has taken months to develop deep and severe drought in the region, and a few wet weeks won’t erase that situation. It can take months of ideal conditions to bring soil, rivers, and vegetation back to health.
On any given day or any given month, somebody somewhere experiences colder-than-average temperature, even though the globe as a whole is warmer than average. We know this through climate monitoring, which entails measuring temperature on land and across the ocean.