NWS Radar: Introduction

Introduction

The Basics

The most effective tool to detect precipitation is radar. Radar, which stands for RAdio Detection And Ranging, has been utilized to detect precipitation, and especially thunderstorms, since the 1940's. Radar enhancements have enabled NWS forecasters to examine storms with more precision.

The radar used by the National Weather Service is called the WSR-88D, which stands for Weather Surveillance Radar - 1988 Doppler (the prototype radar was built in 1988). As its name suggests, the WSR-88D is a Doppler radar, meaning it can detect motions toward or away from the radar as well as the location of precipitation areas.

This ability to detect motion has greatly improved the meteorologist's ability to peer inside thunderstorms and determine if there is rotation in the cloud, often a precursor to the development of tornadoes.

There are 155 WSR-88D Doppler radar in the nation, including the U.S. Territory of Guam and the Commonwealth of Puerto Rico, operated by the National Weather Service and the Department of Defense.

WSR-88D BMX located at Exit 234
off Interstate 65 in Calera, AL

Radar Coverage over Central Alabama

Central Alabama is fortunate in that there are portions of 7 WSR-88D radars that scans its skies.

These include 4 National Weather Service radars:
Birmingham (BMX)
Atlanta (FFC)
Hytop (HYT)
Mobile (MOB)

and 3 Department of Defense (DoD) radars:
Maxwell AFB (MXX)
Columbus AFB (GWX)
Fort Rucker (EOX).

This makes central Alabama one of the most well covered areas in the country. To understand why this is important, click here.

Radar Coverage over Central Alabama

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