24/10/2025
Severe Thunderstorms are Likely This Afternoon and Evening Across Portions of Southeastern WA and Southwestern SA
Scattered severe thunderstorms are expected to develop through the afternoon and evening across parts of southeastern Western Australia into southwestern South Australia. Damaging to locally destructive wind gusts and large to very large hail will be possible.
A closed 500hPa low gradually progress eastward over Western Australia during Friday embedded within more broad westerly zonal flow, a 80 kt jet max is forecast to extend across southwestern WA by 06Z. Ahead of this feature, H300 Heights become broadly diffluent downstream within the WA/SA border region, suggesting that large scale ascent should increase as the day progresses and the trough shifts eastward.
Morning visible/water v***r imagery depicts a surface trough across central southern WA, which is expected to deepen through the day as surface cyclogenesis occurs. By early afternoon, the ECMWF indicates a 998 hPa surface low near the WA/SA border with a developing frontal boundary extending northward. A secondary cold front and associated surface cyclone are evident near the southwest capes of WA.
Persistent convection is ongoing from southern WA into the WA/SA border region, extending north toward Giles, consistent with recent lightning observations.
These storms are occurring within an increasingly moist and unstable airmass, with surface dewpoints near 20 °C expected to advect poleward into the Eucla-Nullarbor region. upstream of this feature a Dryline is is expected to be draped East of Laverton
As a result, MLCAPE of 1000-1500 J/kg is forecast beneath steep mid-level lapse rates (7-7.5°C/km), while 0-6 km bulk shear magnitudes of 50-60 kt will be capable of supporting supercells
A complex convective scenario is expected due to possible residual boundaries from morning convection and several competing Synoptic/mesoscale features which may affect the boundary layer air-mass.
Despite this uncertainty, forecast soundings suggest sufficient buoyancy and deep-layer shear for severe thunderstorms capable of Damaging Wind Gusts and Large Hail supported by steep mid-level lapse rates and favourable CAPE profiles. There is a Slight possibility that Destructive Gusts and Very Large Hail could develop particularly within any supercellular structures that initiate.
Near coastal regions, lower LCL heights and a backed low-level wind field via forecast hodographs (H85 northerlies 35-40 kt) may support a marginal but non-zero tornado threat, if surface-based convection can develop where effective SRH of around 150 ms2/s2 is realised, this scenario is dictated by a small region of lower cloud bases heights and is also conditional to the magnitude of ascent capable of overcoming moderate CINH within the coincident region.
Given Shear Vectors are initially orthogonal to initiating Boundaries, prefrontal Supercell activity appears possible, with possible upscale transition toward MCS complexes during later evening hours as vector orientation becomes more parallel with time, in this scenario Severe Gusts would remain the most probable Hazard.