Libby, mt weather radar

Libby, mt weather radar DEFAULT

Another Eastern Storm to Bring Severe Thunderstorms and Renewed Flooding

Overnight

Rain after 1am. Patchy fog after 4am. Low around Southwest wind 5 to 10 mph becoming light and variable. Chance of precipitation is 80%.

Thursday

Rain. Patchy fog before 3pm. High near Calm wind. Chance of precipitation is 90%. New precipitation amounts between a tenth and quarter of an inch possible.

Thursday Night

Rain. Low around Calm wind becoming south around 5 mph after midnight. Chance of precipitation is 90%. New precipitation amounts between a quarter and half of an inch possible.

Friday

Rain, mainly before 1pm. High near South wind around 5 mph becoming calm in the morning. Chance of precipitation is 80%. New precipitation amounts between a quarter and half of an inch possible.

Friday Night

A chance of rain before 7pm, then a slight chance of rain and snow after 1am. Patchy fog after 1am. Otherwise, mostly cloudy, with a low around Light and variable wind. Chance of precipitation is 50%. Little or no snow accumulation expected.

Saturday

A slight chance of rain and snow before 7am. Patchy fog before 11am. Snow level feet lowering to feet. Otherwise, mostly sunny, with a high near Chance of precipitation is 20%.

Saturday Night

Mostly clear, with a low around

Sunday

Sunny, with a high near

Sunday Night

Mostly clear, with a low around

Monday

Mostly sunny, with a high near

Monday Night

A slight chance of rain and snow. Snow level feet lowering to feet after midnight . Partly cloudy, with a low around

Tuesday

A slight chance of rain and snow. Snow level rising to feet in the afternoon. Mostly sunny, with a high near

Tuesday Night

A slight chance of rain and snow. Snow level feet rising to feet after midnight. Partly cloudy, with a low around

Wednesday

A slight chance of rain and snow. Partly sunny, with a high near

Sours: https://forecast.weather.gov/zipcity.php?inputstring=Libby,MT&Go2=Go

Libby Doppler Radar Loop

Clear Air dBZ ScalePrecipitation dBZ Scale
Rainrate - inches per hour

The colors are the different echo intensities (reflectivity) measured in dBZ (decibels of Z) during each elevation scan. "Reflectivity" is the amount of transmitted power returned to the radar receiver. Reflectivity (designated by the letter Z) covers a wide range of signals (from very weak to very strong). So, a more convenient number for calculations and comparison, a decibel (or logarithmic) scale (dBZ), is used.

The dBZ values increase as the strength of the signal returned to the radar increases. Each reflectivity image you see includes one of two color scales. One scale (far left) represents dBZ values when the radar is in clear air mode (dBZ values from to +28). The other scale (near left) represents dBZ values when the radar is in precipitation mode (dBZ values from 5 to 75). Notice the color on each scale remains the same in both operational modes, only the values change. The value of the dBZ depends upon the mode the radar is in at the time the image was created.

The scale of dBZ values is also related to the intensity of rainfall. Typically, light rain is occurring when the dBZ value reaches The higher the dBZ, the stronger the rainrate. Depending on the type of weather occurring and the area of the U.S., forecasters use a set of rainrates which are associated to the dBZ values.

These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time. Hail is a good reflector of energy and will return very high dBZ values. Since hail can cause the rainfall estimates to be higher than what is actually occurring, steps are taken to prevent these high dBZ values from being converted to rainfall.

Sours: https://www.weatherwx.com/radar_loop/mt/libby.html
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Klcb-Am Libby Doppler Radar Loop

Clear Air dBZ ScalePrecipitation dBZ Scale
Rainrate - inches per hour

The colors are the different echo intensities (reflectivity) measured in dBZ (decibels of Z) during each elevation scan. "Reflectivity" is the amount of transmitted power returned to the radar receiver. Reflectivity (designated by the letter Z) covers a wide range of signals (from very weak to very strong). So, a more convenient number for calculations and comparison, a decibel (or logarithmic) scale (dBZ), is used.

The dBZ values increase as the strength of the signal returned to the radar increases. Each reflectivity image you see includes one of two color scales. One scale (far left) represents dBZ values when the radar is in clear air mode (dBZ values from to +28). The other scale (near left) represents dBZ values when the radar is in precipitation mode (dBZ values from 5 to 75). Notice the color on each scale remains the same in both operational modes, only the values change. The value of the dBZ depends upon the mode the radar is in at the time the image was created.

The scale of dBZ values is also related to the intensity of rainfall. Typically, light rain is occurring when the dBZ value reaches The higher the dBZ, the stronger the rainrate. Depending on the type of weather occurring and the area of the U.S., forecasters use a set of rainrates which are associated to the dBZ values.

These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time. Hail is a good reflector of energy and will return very high dBZ values. Since hail can cause the rainfall estimates to be higher than what is actually occurring, steps are taken to prevent these high dBZ values from being converted to rainfall.

Sours: https://www.weatherwx.com/radar_loop/mt/klcb-am+libby.html
NEXRAD: Eye to the Sky

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Weather libby, radar mt

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Looking at weather radar - #11

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