Tweed 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.
Tweed 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 ». It should provide useful weather information as far west as Glen Innes, south to Kempsey and north to the Gold Coast. There is a tendency to observe areas of false echoes within approximately kilometres of the radar over the sea. These are normally easy to recognise because they are usually the lowest intensity level and randomly scattered with erratic movement from one radar scan to the next. True rain echoes normally have a consistent direction of movement from one scan to the next. Due to its location, this radar is often unable to detect light showers or drizzle beyond a range of kilometres. Although largely removed from the display, anyone to the south west of the radar 50 kilometres or more from Grafton may find an occasional false echo generated by the mountains in this region. There is a small blind spot within a few kilometres of the radar. Charts Australian Charts International Charts. Long Range Forecasts day Rainfall Charts day rainfall forecast month rainfall forecast. Related Links. About Farmonline Weather Radar.
Saturday Sunny. Depending on the type of weather occurring and the area of the Tweed radar loop. You accept all risks and responsibility for losses, damages, costs and other consequences resulting directly or indirectly from using this site and any information or material available from it.
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 located on an isolated hill about m above mean sea level, just east of Beenleigh. This site provides good low-level coverage, ideal for Doppler observations, of the Greater Brisbane area. The Great Dividing Range to the west and the Lamington Plateau to the south, reduce the radar's view from the south through to the west, affecting its ability to detect weak rainfall from low clouds beyond these obstructions. The radar's coverage, based on detecting echoes at an altitude of m, extends to a range of about km in the north to Tin Can Bay, then it follows a smooth arc through the east to the south-south-east, where it rapidly reduces to about km at Evans Head.
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 located on an isolated hill about m above mean sea level, just east of Beenleigh. This site provides good low-level coverage, ideal for Doppler observations, of the Greater Brisbane area. The Great Dividing Range to the west and the Lamington Plateau to the south, reduce the radar's view from the south through to the west, affecting its ability to detect weak rainfall from low clouds beyond these obstructions. The radar's coverage, based on detecting echoes at an altitude of m, extends to a range of about km in the north to Tin Can Bay, then it follows a smooth arc through the east to the south-south-east, where it rapidly reduces to about km at Evans Head. Meteorological Aspects: The radar is well sited to detect rainfall from the west through to the north, the east and to the south. Storms that move into, or develop in and around the Brisbane valley may be tracked and monitored effectively.
Tweed radar loop
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Hail is a good reflector of energy and will return very high dBZ values. Gale Warning for South West Coast. The dBZ values increase as the strength of the signal returned to the radar increases. These usually show up as small, stationary patches of rain, mostly along the higher ground. Gold Coast Tomorrow Partly cloudy. Depending on the type of weather occurring and the area of the U. View legend ». The colours and symbols used on the radar and satellite maps are described on our legend page. The colors are the different echo intensities reflectivity measured in dBZ decibels of Z during each elevation scan. Storms that move into, or develop in and around the Brisbane valley may be tracked and monitored effectively. Monday Possible shower. Weather satellite cloud imagery is originally processed by the BOM from the geostationary satellite Himawari-8 operated by the Japan Meteorological Agency.
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Mcleans Ridges. Tropical Cyclone Synoptic Charts. High chance of rain, most likely in the morning. The other scale near left represents dBZ values when the radar is in precipitation mode dBZ values from 5 to These are normally easy to recognise because they are usually the lowest intensity level and randomly scattered with erratic movement from one radar scan to the next. Typically, light rain is occurring when the dBZ value reaches It should provide useful weather information as far west as Glen Innes, south to Kempsey and north to the Gold Coast. Use the map search tool if you want to place a location marker on the radar map Later on Sunday or Monday, a cold front will pass well to the south. Canungra Defence. The radar's coverage, based on detecting echoes at an altitude of m, extends to a range of about km in the north to Tin Can Bay, then it follows a smooth arc through the east to the south-south-east, where it rapidly reduces to about km at Evans Head. In winter time, rain bearing systems approaching from the southwest and south may be partially obscured by the Great Dividing Range and the Lamington Plateau.
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