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A decaying cold front brings rain across SA's east, southwest QLD, & western NSW. A coastal low is weakening & slowly tracking SE, causing winds & showers to ease in VIC, but still bringing showers to eastern TAS. Showers are occurring over SW WA due to a moist onshore airstream.

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Min

Max

Mostly CloudySydneyNSW

9.3°C

8°C
19°C

Mostly CloudyMelbourneVIC

8.7°C

7°C
14°C

Increasing SunshineBrisbaneQLD

8.6°C

9°C
21°C

Mostly CloudyPerthWA

14.3°C

12°C
21°C

Clearing ShowerAdelaideSA

10.5°C

8°C
16°C

Mostly CloudyCanberraACT

2.9°C

0°C
13°C

Mostly SunnyHobartTAS

10.0°C

10°C
16°C

Mostly SunnyDarwinNT

21.7°C

21°C
31°C

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Latest News


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Today, 9:07AM UTC

The 'bombing low' behind Sydney's weekend deluge

Sydney endured its second wettest June day on record on the weekend as a bombing low pressure system rapidly intensified off the NSW coast. The radar animation below shows heavy and persistent rain hammering central eastern NSW on the weekend. #Sydney's 142.6mm during the last 24 hours was the city's heaviest daily rain in 4 years and its wettest June day since 1991. It's also more than one month's rain for this time of year. Sydney's June monthly average is about 132mm. pic.twitter.com/HxDXg762PR — Ben Domensino (@Ben_Domensino) June 1, 2024 Sydney was inundated by heavy rain on Saturday into Sunday morning, with the Observatory Hill weather station collecting 142.6 mm of during the 24 hours ending at 9am on Sunday. This was more than the city’s entire June average (about 132 mm) and Sydney’s second wettest June day in records dating back to 1859, beaten only by 150.6 mm in 1991. The weekend’s torrential rain, which caused flash flooding in parts of Sydney, was driven by a rapidly deepening low pressure system over the Tasman Sea. The low formed on Saturday and intensified so quickly that its central pressure dropped by 19 hPa during the 24 hours ending at 4pm on Sunday. At Sydney’s latitude, this rate of pressure change was enough to classify the system as a ‘bombing low’, which is the name given to mid-latitude low pressure system that deepens rapidly in a process called explosive bombogenesis. Images: Mean sea level pressure (MSLP) analysis charts from 4pm AEST Saturday, June 1 (top) and 4pm AEST Sunday, June 2 (bottom), showing a deepening low pressure system over the Tasman Sea. Source: Bureau of Meteorology The threshold for a bombing low pressure system differs depending on latitude. For example, at 60° latitude in either hemisohere, a pressure drop of 24 hPa in 24 hours is required a system to be classifies as a bombing low. But at Sydney’s latitude around -34° south, a system’s central pressure only needs to drop by around 16 hPa in 24 hours for it to be a bombing low. This made the weekend’s 19 hPa pressure drop more than enough to call the Tasman Sea system a bombing low. Other impacts from the weekend’s bombing low in the Tasman Sea included: Maximum wave heights reaching 9.6 metres off Sydney at midday on Sunday Mallacoota’s 112 mm of rain during the 24 hours ending at 9am on Monday was its wettest winter day on record, with data dating back to the 1970s This was the second bombing low pressure system near Australia in one week, after another low deepened by 30 hPa in 24 hours over the Great Australian Bight last Wednesday and Thursday. Abnormally warm sea surface temperatures near Australia southern and eastern coastlines may have helped these two low pressure systems undergo bombogenesis.

Today, 6:31AM UTC

Darwin's hottest May in over a century

Australia's northernmost capital city Darwin has just sweated through its hottest May in reliable records for maximum temperatures, as well as one of its most humid despite no rain falling. Darwin's maximum temperatures averaged 33.7°C this May, +1.6°C warmer than the long-term average for the site. This makes it the warmest May in 117 years of reliable records*, just warmer than previous title-holder in 2022 (averaging 33.6°C).  Image: Maximum temperature deciles for May, showing they were the highest on record for Darwin and surrounding areas, with much of the Top End and eastern NT above average. Temperatures ranged from a high of 35.1°C on Friday 10th and a low of 30.5°C on Tuesday 21st. Oddly enough, both of these days featured gusty east-southeasterly winds coming off the Australian continent. The difference between these two days was cloud-cover, with warm conditions in clear skies, and cooler conditions if its cloudy. Minimum temperatures averaged 23.7°C, +1.5°C above average. While this seems warm (even hot by southerner's standards) this was only the 10th warmest May on record. Only one night fell below 20°C (19.1°C on Tuesday 21st), the common threshold beyond which locals add an extra blanket to the bed. Darwin did not record a drop of rain during May, although that is fairly common. 24 out of the 78 Mays the current Darwin Airport site has been recording for have been completely dry, with a further eight recording 1mm or less. Despite the dry, Darwin and much of the Northern Territory were more humid than normal during May. The map below shows specific humidity (akin to dew point temperature) anomalies during May. The large region in blue and purple reflect humidity being higher than normal. Darwin and the NT is far from alone with this increased humidity, with locations near the equator from Africa to the central Pacific Ocean showing a similar pattern. This reflects how much warmer ocean and air temperatures were during May, and for the last 12 months, especially for the world's tropics. Climate outlooks are suggesting Darwin will continue with a run of warmer than average temperatures each month during the dry season. However, if La Niña starts to develop, increasing cloud would be expected over the Top End later in the year, reducing temperatures closer to average. *Note: Prior to 1907, records at Darwin's Post Office site are not considered always reliable as this was before weather measurment standards were enforced at the site.

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Today, 6:17AM UTC

Stormy end to southwest WA's driest autumn

The taps turned on during the opening days of winter in the southwest of WA, after some areas recorded the driest autumn on record.  The rain and thunderstorms over the weekend were triggered by a strong cold front sweeping across the state, interacting with tropical moisture and the warm sea surface temperatures off the WA coastline.  The image below shows a line of thunderstorms marching towards the state’s southwest on Saturday night.  Image: Radar and lightning for the three hours leading up to 11pm AWST on Saturday, June 1.  This line of storms brought Perth a third of their average monthly rainfall, with 42.2mm falling in just 10 and a half hours leading up to 9am on Sunday, June 2. Lancelin to the north of Perth saw 37.8mm fall, while Geraldton picked up 29mm during this event.   The thunderstorms also produced damaging wind gusts on Saturday night, with Rottnest Island recording a 102km/h gust, Busselton Jetty a 91 km/h gust and Armament Jetty 93 km/h gust.   Rain continued to fall in the southwest and Pilbara on Sunday, with Carraba in the Pilbara picking up 50mm in the 24 hours leading up to 9am Monday, June 3.   While rain has continued in the northwest of the state on Monday, the skies will clear up for a couple of days from Tuesday, as a high-pressure system moves in.  Looking ahead, another cold front is setting its sights on WA later this week and is expected to bring significant rainfall to the southwest and interior.  The map below shows the rain forecast for the next week across parts of WA.     Image: Accumulated rainfall total for the 7 days leading up to 8pm on Sunday, June 9.  The taps turning on in the first week of winter is welcome, after some areas of southwest WA saw the lowest autumn rainfall on record.   The map below shows that while the interior saw above average rainfall and, in some areas, the highest rainfall on record in autumn, the southwest was parched.   Image: Australian rainfall deciles for autumn 2024. Source: Bureau of Meteorology  Meanwhile the daytime and nighttime temperatures were the highest on record for the west coast of WA.   The map below shows the above average temperatures in the state’s west, while the interior had a cooler autumn.  Image: mean temperature deciles for autumn 2024. Source: Bureau of meteorology  The warm and dry autumn in the west was dominated by stubborn high-pressure systems which forced many cold fronts and their associated rain and cooler air further south.    

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14 May 2024, 3:01AM UTC

Can auroras affect aeroplanes?

Auroras lit up the skies on the weekend amid one of the strongest geomagnetic storms in years, but did this display impact aeroplanes and the aviation industry?  The spectacular exhibit was the aurora borealis/australis, or northern and southern lights seen in both hemispheres.      Images: Aurora Australis on Saturday, May 11 from Bendleby Ranges, SA (top), source: @bendlebyranges and Ricketts Point, Vic (bottom), source: @dayofthedreamer  These lights are typically only seen in the polar latitudes, but this weekend they were spotted in the Southern Hemisphere as far north as Mackay in Queensland. This was caused by the strongest solar flare and storm seen in over 20 years.  This auroral display was caused by a solar flare and multiple coronal mass ejections (CMEs) which erupted from the sun over a few days last week. Charged particles were then carried from the sun to earth by a solar wind.   When these particles reached earth, they interacted with our planet’s magnetic field and were driven towards the magnetic poles.   In the upper layer of the atmosphere called the ionosphere (90km above the surface) the solar wind collides with oxygen and nitrogen in this layer and produces a colorful display.  The southern lights typically occur between 50 and 800km above the surface, well above the layer of atmosphere that planes typically fly in.   So, do they impact aviation despite occurring well above the flight level?   Yes, space weather events like this can impact aviation communications, navigation and surveillance systems. They can also increase the radiation exposure of aircraft in the air.       Images: Aurora Australis from Virgin plane cockpit on Saturday, May 11. Source: @shelbytillett  The charged particles caused by CMEs can modify the upper layer of earth's atmosphere called the ionosphere, which can impact our technology systems.   High frequency radio communication depends on the ionosphere reflecting radio waves back down to earth.  Satellite communication, navigation and surveillance rely on the transmission of signals through the ionosphere.   According to the Bureau of Meteorology’s space weather department, >Space weather events that modify the density and/or structure of the ionosphere can therefore significantly impact the performance of HF COM, SATCOM and SATNAV systems". While communication and navigation can be impacted by the modification of the ionosphere, the electricity network can also be impacted. The storms can induce currents in power lines, overheating transformers, which can potentially cause power outages.   The strongest geomagnetic storm ever recorded occurred during September 1859, called the Carrington Event. This event caused multiple fires of telegraph systems across Europe and North America.  There have been no reports of negative major impacts of this solar storm, it was merely a spectacular display that captivated people across the world.   Unfortunately, auroras are notoriously difficult to forecast as they need multiple factors to line up for these beautiful lights to occur.  Looking ahead, the sun is nearing its solar maximum, which means we could see more sunspots on the sun's surface this year. This could increase our chance of seeing more spectacular displays in the coming months.

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07 May 2024, 11:23PM UTC

How severe thunderstorms impact energy infrastructure

Earlier this year destructive thunderstorms and winds equivalent to a category two cyclone lashed Victoria, bending towers and toppling trees and poles.  So, how can thunderstorms damage energy infrastructure, and are these events getting worse?   This event occurred during mid-February 2024, when a strong cold front generated severe thunderstorms and localised wind gusts of 130km/h after a prolonged period of extreme heat. The image below shows a squall line around 1,500km long causing lightning across four states in February.  Image: Himawari-9 satellite image, lightning and radar on Tuesday, February 13 at 3pm AEDT.  The destructive winds were caused by microbursts, which bent towers and toppled trees and poles in Vic, leaving thousands without power.   Image: Damaged transmission towers at Anakie, Source: AAP  Microbursts are a localised column of sinking air (downdraft) within a thunderstorm and is usually less than 4km wide. The cold, heavy air within this downdraft descends rapidly to the surface and then spreads out in all directions as it hits the ground. The image below shows how wind gusts are produced in thunderstorms.    Microbursts can be destructive and cause wind gusts above 100 km/h, which can be a risk for power infrastructure. The force applied to the structure is roughly proportional to the speed squared.  Fierce wind gusts from thunderstorms can:  Knock down trees, which can fall onto power lines  Topple poles  Knock out transmission towers.  Microbursts typically occur during the warmer months of the year and, unfortunately, they can develop rapidly and last for only a short period of time, making them difficult to predict and warn communities about.   Have these thunderstorm events become more severe in Victoria?   The severe thunderstorm season across southern Australia occurs during the warmer months of the year, between November and April.   While thunderstorms are more common across northern Australia, Qld, and NSW, they do occur frequently in the summer months. The map below shows the annual average lightning density in Vic between July 2014 and June 2023, with the most lightning occurring in the northeast high country each year.      Image: Weatherzone’s Total Lightning Network Annual lightning density mean between July 2014 and June 2023.  You can see in the map above that lightning is common to the north of Ballarat near Learmonth and Miners Rest, with the region seeing 37.7 pulses per year. The high country near Benalla and Whitfield recorded an average of 28.1 pulses, Thorpdale in Gippsland saw 24.5 pulses, and Melbourne only 8.2 pulses per year.    Research has shown that the warming climate is increasing the risk of heatwaves and bushfires, which can impact energy infrastructure. Unfortunately, it is unknown how global warming will affect thunderstorms and their associated destructive winds. To research climate change's impact on thunderstorms, we would need quality data that dates back well into history. Unfortunately, detecting lightning is a fairly new phenomena, so a solid climate base to compare data to is not currently existent.   According to the University of Melbourne researchers and Watt Clarity, ‘The evidence we do have suggests continued climate change may potentially increase the risk of extreme winds from thunderstorms. This is partly due to more moist and unstable air, which are essential for thunderstorms to form. We think these conditions could occur more often with climate change, in part because warmer air can hold more moisture.’   Indeed, much of Australia had an unusually stormy summer 2023/24, with Melbourne, Canberra and Brisbane all seeing 5 to 6 extra storm days a season. The map below shows that an unusually high number of thunder days were seen over most of Qld, NSW, SA, Vic, the ACT and Tas during the summer of 2023/24 compared to the average of the most recent nine years.  Image: Thunder day anomalies for summer 2023-24 versus the average thunder days for the nation’s nine most recent summers (2014/15 to 2022/23). 

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