Bendigo radar loop

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The colors are the different echo intensities reflectivity measured in dBZ decibels of Z during each elevation scan. 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. The other scale near left represents dBZ values when the radar is in precipitation mode dBZ values from 5 to Notice the color on each scale remains the same in both operational modes, only the values change.

Bendigo radar loop

The origin may be changed by clicking elsewhere on the map. The colours and symbols used on the radar and satellite maps are described on our legend page. View legend ». The Yarrawonga radar has a very good view in all directions and is the primary weather radar for Northern Victoria, which includes the Goulbourn Valley. It should provide useful weather information as far south as Marysville, west to Bendigo and north to Griffith. The advantage of the "C Band" radar is that it is better at detecting smaller drops so therefore performs better in light rain situations. The Yarrawonga radar has a greater ability to resolve thunderstorms in the summer months when echoes are generally larger. Being a "C Band" radar, if there are large thunderstorms in the area, the radar may not be able to determine accurately the strength of additional storms located behind the closest storms. False echoes can be sometimes observed very close to the radar especially in stable conditions. These are normally easy to distinguish because they are usually of the lowest intensity level and are very small and randomly scattered. Echoes within approximately five kilometres of the radar and overhead can be poorly resolved as the scanning elevation is too low. Charts Australian Charts International Charts.

To better understand the icons, colours and weather terms used throughout Weatherzone, please check the legend and glossary. Summer thunderstorms that develop on the surrounding hills and mountains may be observed in detail. Bendigo radar loop for Central Gippsland Coast

You do not have a default location set To set your location please use the search box to find your location and then click "set as my default location" on the local weather page. Tropical Cyclone Synoptic Charts. Forecast Local Weather Climate. Geographical Situation; The radar is situated on the western plains of the Melbourne basin some 19km west-south-west of the Central Business District, about six kilometres from the western shores of Port Phillip bay and on a low rise about 20m above mean sea level. The radar is on a tower 24m above ground level.

I don't get why people are upset we haven't invented hover-boards by when according to the same movie, we should've had a time machine back in in Enter Town Name: Search. Enter Town Name:. Mundulla Weather Observatory. Stromlo South. Victorian Weather Situation A large high pressure system lies over the Tasman Sea and extends a broad ridge over Victoria directing a hot northerly airflow across the State throughout the weekend.

Bendigo radar loop

You do not have a default location set To set your location please use the search box to find your location and then click "set as my default location" on the local weather page. Tropical Cyclone Synoptic Charts. Forecast Local Weather Climate. Geographical Situation; The radar is situated on the western plains of the Melbourne basin some 19km west-south-west of the Central Business District, about six kilometres from the western shores of Port Phillip bay and on a low rise about 20m above mean sea level. The radar is on a tower 24m above ground level. The Great Dividing Range dominates the topography from the east, through the north to the west. Meteorological Aspects; The radar is well sited to provide very good coverage for the Greater Melbourne Metropolitan Area. The high ground from the east, through north and to the south west tends to obscure shallow rain falling further away. Summer thunderstorms that develop on the surrounding hills and mountains may be observed in detail. Similarly, cold fronts and associated rain and thunderstorms approaching from the northwest, through west and south are well detected.

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It is a prediction that uses past radar and satellite data to infer the movement and intensity of precipitation. For general feedback and enquiries, please contact us through our Help Desk. Sunrise: Moonrise: Sunset: Moonset: View legend ». Depending on the type of weather occurring and the area of the U. Tropical Cyclone Icon Tropical Cyclones. Synoptic Chart. Similarly, cold fronts and associated rain and thunderstorms approaching from the northwest, through west and south are well detected. The Yarrawonga radar has a greater ability to resolve thunderstorms in the summer months when echoes are generally larger. Puckapunyal-Lyon Hill Defence. Light Heavy. Meteorological Aspects; The radar is well sited to provide very good coverage for the Greater Melbourne Metropolitan Area. More News Arrow Accordion. Rain radar. Find out more Get in touch.

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Leverage advanced weather intelligence and decisioning tools for your enterprise business. Pro Unlock more weather data and layers options. Ballan Cfa. Find out more Get in touch. Weather Weather Warnings. About Farmonline Weather Radar. The higher the dBZ, the stronger the rainrate. Related Links. To better understand the icons, colours and weather terms used throughout Weatherzone, please check the legend and glossary. Depending on the type of weather occurring and the area of the U. So, a more convenient number for calculations and comparison, a decibel or logarithmic scale dBZ , is used. The high ground from the east, through north and to the south west tends to obscure shallow rain falling further away. Some data on this site is sourced from Bureau of Meteorology. Tropical Cyclone Synoptic Charts. Echoes within approximately five kilometres of the radar and overhead can be poorly resolved as the scanning elevation is too low.