
Gulf Shores Doppler Radar
![]() | ![]() |
![]() |
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 -28 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 20. 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.
Gulf Shores Doppler Radar Loop
![]() | ![]() |
![]() |
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 -28 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 20. 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.
- Blue and yellow cotton fabric
- What are chipset drivers
- Blue letter bible app
- Outdoor swing chair with footrest
Gulf Shores Weather Radar
Today's Forecast
















Trending Stories
Be patient a little, now I will send you to heaven. Well, go, darling. Like this.
Shores weather radar gulf
The stranger's eyes slid down and his gaze appeared an exhausted hole with the petals of her bosom wide open. He closed the door and with the words - Well, let's continue what we started?, He took her by the arms, lifted. Her and pressed her against the wall.
Furuno's WR2120 Doppler Radar InstallationHe began like a tiger, slowly with stops and fading sensations. Irishka, who suddenly felt that the guy's hand, bursting with heat, was on the inside of her thigh, and began to warm her skin in the immediate vicinity of. The crack hidden under the fabric of her panties, and that this touch caused a pleasant and warm wave in her body, warming everything her frozen body, did not push the guy away and demand his retreat, reassuring herself that it was just a leg, and that she was frozen, and that she needed to be warmed up.
Similar news:
- 7 types of narcissism
- Affinity designer t shirt template
- Home depot frame it all
- Wells fargo phone number
- Hp pavilion slimline video card
- Potter county jail mugshots 2021
- Used doggie doors for sale
- Er nurse salary los angeles
- Command strips home depot
- Starting soon video free download
- Dog adoption frederick md
Christina nodded. Alice called the waiter and paid the bill - There is my car, sit down, let's go to me, let's see what you're worth. We drove for about 40 minutes, Alisa Vladimirovna lived in the center and owned, apparently alone, a large apartment - about 120 meters.
As soon as they entered, Alice immediately went into action, apparently decided to take Christina, who still had her will, by surprise. - Take off your clothes.