Search results
Results From The WOW.Com Content Network
Moving west toward the mountainous interior of the state, the climate becomes markedly colder, the number of cloudy days increases, [1] and winter snowfall amounts are greater. Using the January freezing isotherm, the humid subtropical climate ( Cfa ) only exists in parts of Greater Philadelphia and low-lying areas of the lower Susquehanna ...
Freshly fallen snow and heavy rain can all make a rush-hour commute frustrating, but freezing rain is perhaps the most deceiving and destructive of all winter precipitation. Simply put, freezing ...
Because freezing rain does not hit the ground as an ice pellet (called "sleet") but still as a rain droplet, it conforms to the shape of the ground, or object such as a tree branch or car. This makes one thick layer of ice, often called "glaze". Freezing rain and glaze ice on a large scale is called an ice storm. Effects on plants can be severe ...
The ice storm affected a large part of eastern Ontario, southwest Quebec, and New York state. This map shows the accumulation of freezing rain in those areas. On January 4, 1998, an upper level low system stalled over the Great Lakes, pumping warm and moist air from the Gulf of Mexico toward the upper St. Lawrence Valley.
Freezing rain sometimes marks the southern edge of wintry precipitation in weather systems. That southern edge can dip into areas not used to dealing with wintry weather, such as the South.
4) Don't Forget the Ice. An ice threat comes along with the snow. Sleet and freezing rain are fairly common in the South, with many areas seeing wintry precipitation at least once each season.
The freezing rain coated all surfaces with thick layers of ice, including power lines and tree limbs which break under the additional weight. Some locations in the Mid-Atlantic received several inches of sleet. four inches (100 mm) of sleet caused travel difficulties and hampered cleanup efforts in New York City .
It is often seen on trees atop mountains and ridges in winter, when low-hanging clouds cause freezing fog. This fog freezes to the windward (wind-facing) side of tree branches, buildings, or any other solid objects, usually with high wind velocities and air temperatures between −2 and −10 °C (28 and 14 °F). [6]