Weather Alerts for New York

Recent Locations: Fox Lake, WI   Dobbs Ferry, NY   New Palestine, IN  

1. Cold Weather Advisory for: Eastern Clinton; Eastern Essex; Grand Isle; Western Franklin; Orleans; Essex; Western Chittenden; Lamoille; Caledonia; Washington; Western Addison; Orange; Western Rutland; Eastern Franklin; Eastern Chittenden; Eastern Addison; Eastern Rutland; Western Windsor; Eastern Windsor

2. Cold Weather Advisory for: Niagara; Orleans; Monroe; Wayne; Northern Cayuga; Northern Erie; Genesee

3. Cold Weather Advisory for: Northern Saratoga; Northern Washington; Southeast Warren; Southern Washington

4. Extreme Cold Warning for: Eastern Schenectady; Southern Saratoga; Eastern Albany; Western Rensselaer; Eastern Greene; Western Columbia; Eastern Windham

5. Extreme Cold Warning for: Northern Herkimer; Hamilton; Southern Herkimer; Southern Fulton; Montgomery; Northern Warren; Schoharie; Western Schenectady; Western Albany; Western Greene; Western Ulster; Northern Fulton

6. Extreme Cold Warning for: Northern Oneida; Yates; Seneca; Southern Cayuga; Onondaga; Steuben; Schuyler; Chemung; Tompkins; Madison; Southern Oneida; Cortland; Chenango; Tioga; Broome; Bradford; Susquehanna

7. Extreme Cold Warning for: Northern St. Lawrence; Northern Franklin; Southeastern St. Lawrence; Southern Franklin; Western Clinton; Western Essex; Southwestern St. Lawrence

8. Extreme Cold Warning for: Oswego; Jefferson; Lewis

9. Extreme Cold Warning for: Otsego; Delaware; Sullivan; Northern Wayne; Pike; Southern Wayne

10. Extreme Cold Warning for: Wyoming; Livingston; Ontario; Chautauqua; Cattaraugus; Allegany; Southern Erie

11. Winter Weather Advisory for: Eastern Rensselaer; Bennington

12. Winter Weather Advisory for: Jefferson

13. Winter Weather Advisory for: Monroe; Wayne; Northern Cayuga; Oswego; Livingston; Ontario

14. Winter Weather Advisory for: Niagara; Orleans; Northern Erie; Genesee; Wyoming; Chautauqua; Cattaraugus; Southern Erie

15. Winter Weather Advisory for: Seneca; Southern Cayuga; Onondaga; Tompkins; Cortland

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Current U.S. National Radar--Current

The Current National Weather Radar is shown below with a UTC Time (subtract 5 hours from UTC to get Eastern Time).

Current U.S. National Radar

National Weather Forecast--Current

The Current National Weather Forecast and National Weather Map are shown below.

Today's National Weather Map

National Weather Forecast for Tomorrow

Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.

Tomorrows National Weather Map

North America Water Vapor (Moisture)

This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.

North American Water Vapor Map

Weather Topic: What is Precipitation?

Home - Education - Precipitation - Precipitation

Precipitation Next Topic: Rain

Precipitation can refer to many different forms of water that may fall from clouds. Precipitation occurs after a cloud has become saturated to the point where its water particles are more dense than the air below the cloud.

In most cases, precipitation will reach the ground, but it is not uncommon for precipitation to evaporate before it reaches the earth's surface. When precipitation evaporates before it contacts the ground it is called Virga. Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog and mist are not considered precipitation because the water vapor which constitutes them isn't dense enough to fall to the ground.

Next Topic: Rain

Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

Shelf Clouds Next Topic: Sleet

A shelf cloud is similar to a wall cloud, but forms at the front of a storm cloud, instead of at the rear, where wall clouds form.

A shelf cloud is caused by a series of events set into motion by the advancing storm; first, cool air settles along the ground where precipitation has just fallen. As the cool air is brought in, the warmer air is displaced, and rises above it, because it is less dense. When the warmer air reaches the bottom of the storm cloud, it begins to cool again, and the resulting condensation is a visible shelf cloud.

Next Topic: Sleet

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