![]() ![]() These terms may change from time to time without notice. You also agree that we shall not be liable for any compensatory, direct, indirect, incidental, consequential or punitive damages, income or profit loss, or any claims of any parties whatsoever with respect to this service. By using this forecast, you agree that there may be differences in forecast conditions and actual flying conditions. Use extreme caution before flying any aircraft. We do not guarantee the weather forecast is accurate enough to be used for flying. Please contact the FAA for more information on pilot briefings or call 1-800-WX-BRIEF.Īs with all forecasts, weather conditions can change dramatically from what has been forecasted. This forecast and the related content/links on this page are not a substitution for the official weather briefing from the FAA. The user assume the entire risk associated with the use of this data. Check your conditions before you launch and only launch in conditions that you are familiar with and are certified to fly in. Regardless of what this program has forecasted, it is not intended to be a substitution for good common sense. The contents, including graphics and display format, are under copyright by Air Sports Net. The Raw Data used in this forecast was obtained from the National Weather Service's National Blend of Models and is not subject to copyright protection. Search for the Nearest Winds Aloft Forecast Station Of upper and lower values of current conditions amongst 24 locations Station: KIND North: 39.73 West: -86.28 Timezone: Eastern Daylight Saving Time UTC: -4 Model: National Blend of Models - Aviation Format ![]() 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.Aviation Weather Forecast at Indianapolis Intl, Indiana Hail is a good reflector of energy and will return very high dBZ values. These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time. 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. The higher the dBZ, the stronger the rainrate. Typically, light rain is occurring when the dBZ value reaches 20. The scale of dBZ values is also related to the intensity of rainfall. The value of the dBZ depends upon the mode the radar is in at the time the image was created. Notice the color on each scale remains the same in both operational modes, only the values change. The other scale (near left) represents dBZ values when the radar is in precipitation mode (dBZ values from 5 to 75). One scale (far left) represents dBZ values when the radar is in clear air mode (dBZ values from -28 to +28). Each reflectivity image you see includes one of two color scales. The dBZ values increase as the strength of the signal returned to the radar increases. So, a more convenient number for calculations and comparison, a decibel (or logarithmic) scale (dBZ), is used. Reflectivity (designated by the letter Z) covers a wide range of signals (from very weak to very strong). "Reflectivity" is the amount of transmitted power returned to the radar receiver. The colors are the different echo intensities (reflectivity) measured in dBZ (decibels of Z) during each elevation scan. ![]()
0 Comments
Leave a Reply. |