A low pressure system lies in central Western Australia has a trough extending along the South Australian coast into western Victoria and off of the Victorian Surf coast. This system driving a thick band of cloud over the southern half of Western Australia that stretches along the trough into western Victoria ahead of a cold front off the western coast of Tasmania. Mid to high level cloud persists over the central parts of Australia, remnants from thunderstorm activity overnight. Low level convective cloud from day time heating is visible over northeast New South Wales, and over much the majority of Queensland. In the Tropics of Australia, convective low through middle level cloud is visible over the northern Top End with wispy remnants of yesterday's thunderstorms. In the Kimberley district of Western Australia, an organised system of thunderstorms is driving mid through high level cloud over the region. Patchy low level cloud blankets much of the southeast with high cloud drifting east from the Bight.