Tweed radar loop

Books replaced tablets over a thousand years ago. Enter Town Name: Search. Enter Town Name:. Mcleans Ridges.

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.

Tweed radar loop

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. 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. These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time.

The other scale near left represents dBZ values when the radar is in precipitation mode dBZ values from 5 to

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.

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. During summertime, rain depressions and storms approaching from the northwest and the north may be readily detected as can any tropical cyclones over the ocean to the north through to the south east.

Tweed radar loop

First day of spring: Meteorological and astronomical spring difference. Storms to gather on US East Coast with weekend rain, wind and snow. Clipper storm to unload snow in Minneapolis, Chicago and eye Northeast. DC cherry blossoms peaked so early, the famous festival hasn't begun. United CEO tries to reassure customers following multiple safety incid A California superbloom is springing to life and the best is yet to co Global ocean heat has hit a new record every single day for the last y

Catziilla

Tweed River tide times are derived from astronomical tide predictions issued by the BOM. Tropical Cyclone Synoptic Charts. E-mail the Tweed Heads Weather Forecast. Tweed Heads Weather Map. Geographical Situation: The radar is located on an isolated hill about m above mean sea level, just east of Beenleigh. Notice the color on each scale remains the same in both operational modes, only the values change. Sunrise: Moonrise: Sunset: Moonset: Use the map search tool if you want to place a location marker on the radar map National Two Day Weather Forecast. Hail is a good reflector of energy and will return very high dBZ values. Site search. This pattern will bring mostly settled conditions for the first half of the week. 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. Latest Radar Image.

.

Depending on the type of weather occurring and the area of the U. Related Links. Charts Australian Charts International Charts. Tropical Cyclone Synoptic Charts. Books replaced tablets over a thousand years ago. Gold Coast Today Cloudy. Hail is a good reflector of energy and will return very high dBZ values. Help with Farmonline Weather. Sunrise: Moonrise: Sunset: Moonset: Tweed Heads Radar Loop Weather. Non-meteorological echoes: In most cases, processing of the radar signal removes permanent echoes caused by hills, buildings and other solid objects, but sometimes a few slip through. 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. Typically, light rain is occurring when the dBZ value reaches