The first weekend of June belonged to a deep area of low pressure that ran in close to the UK on Saturday the 6th — the first proper test of the new positive-NAO regime, and a windstorm-flavoured day landing in what is nominally peak convective season.
How it played
The Met Office's weekend briefing had the picture right: tightly packed isobars on the low's southern flank brought a windy start across south-western Britain, with coastal gales developing for a time and peak gusts around 50 mph along the north coast of Cornwall, Devon and through the Bristol Channel — squarely inside our chase domain's western edge.
Saturday morning brought widespread rain across large parts of England, Wales, Northern Ireland and southern and central Scotland, heaviest in western and south-western areas, with the wind strengthening through the morning as the low's centre approached. Sunday flipped the script: drier for much of England and Wales, showers retreating to western and northern coasts, and the east staying largely dry.
The chaser's read
June lows of this depth are worth logging for two reasons:
- They calibrate the wind atlas. A 50 mph coastal gust event under a tight gradient is a clean benchmark for the deep-shear and jet diagnostics we lean on during HSLC convective days — same engine, different mode.
- They reset the ground state. A soaking like Saturday's recharges catchments and soils that late-May heat had been baking dry — which changes both the flood-gauge picture and the wildfire calculus for the rest of the month.
No convective risk verified inside the domain — this was gradient wind and warm-sector rain, not instability. But as a marker of how decisively the pattern has flipped since the May ridge, the first Saturday of June was hard to beat.
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