A late evening rainstorm / thunderstorm impacted a narrow corridor between Hornsby to the north and Horsley Park to the south late Saturday evening. The event followed a warm humid day across the city.

While short lived thunderstorms impacted rural areas south and west of Sydney during Saturday, none of these impacted the city.

The storm formed north of Hornsby after sunset then tracked southwest over Castle Hill, then Blacktown before tracking slowly towards Horsley Park where it weakened. In this regard, it tracked southwest into Western Sydney from the northeast but was no more than approximately 10 km in width.

Sydney radar showing the core of the storm directly over Blacktown. The area of brightest red is over Doonside. Heavy rainfall was a standout feature and given that the storm was slow moving, rainfall figures quickly accumulated. The cell was rather isolated in nature. The storm went into rapid decline as it passed over Horsley Park.

The storm was:

  • Slow moving (Similar to the Wednesday afternoon storm) and as such, considerable rainfall fell across all suburbs in its path.
  • Had little wind except that it became windy as its northern edge crossed over.
  • No hail but the strong rainfall was sustained for its entire duration.
  • Intracloud lightning was contained within the core but no cloud to ground flashes observed.

I have attached the cumulative rainfall information using the Sydney radar information and the track of the storm is visible. This is highlighted in red as its width was narrow.

The graphic shows rainfall accumulations. The width and path of the storm is shown within the red ellipse. It formed north of Hornsby but went into decline south of Horsley Park. All those suburbs on either side of this received little in the way of rainfall.

When zoomed in, it can be seen that falls amounted to between 25 mm and 40 mm.

Kings Langley received 26.5 mm. Unfortunately, there were limited rain gauges within the path of the storm but the computer models clearly suggest falls of 25 mm to 40 mm within the narrow path.

My rain gauge picked up 33.7 mm and consistent with the model shown.

Seen against a nearby streetlight, the intensity of the rainfall is visible at the height of the storm. Intense rainfall is visible which is rare to see in low light conditions. This correlates with the radar image shown above. The primary feature of the thunderstorm was the intense rainfall and with the storm slow moving, amounts quickly accumulated.

I managed to take some night time photos of the rainfall intensity which is added to the post.

It is likely that brief flooding would have occurred within some low lying areas given the intensity of the rain that occurred.

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