This revised report presents the key developments behind Storm Dave Eased on Easter Sunday After Severe Winds, Snow and Travel Disruption in a clearer structure, without adding claims beyond the original article.
The worst of Storm Dave moved away from the UK during Easter Sunday, 5 April 2026, allowing weather warnings to be lifted after a disruptive Saturday of strong winds, rain and snow.
The Met Office lifted the amber wind warning at 3am.
Remaining yellow warnings across parts of Wales, northern England and Scotland expired later in the morning.
Improving weather did not mean transport and infrastructure instantly returned to normal.
What was the Easter Sunday forecast?
The Met Office said Storm Dave would clear to the northeast, leaving sunshine and showers.
Where were the heaviest showers expected?
Northern areas were expected to see the most frequent and blustery showers.
Why the north still felt cold
Cooler air remained wrapped around the departing low-pressure system.
Amber warning lifted at 3am
The highest-level warning associated with the storm ended during the early hours.
What areas had been covered?
Parts of northern England, north-west Wales and southern Scotland.
Yellow warnings
Other wind warnings remained temporarily in place after the amber area expired.
Wales
A yellow warning there ended earlier on Sunday morning.
Northern England and Scotland
Warnings continued until later in the morning before being lifted.
Why warnings end at different times
The strongest wind field moves across the country rather than weakening everywhere simultaneously.
Severe gales before clearing
Forecasters still expected strong winds in central and northern areas during the early hours.
Why “easing” does not mean immediately calm
A storm can be weakening overall while still producing dangerous local gusts.
Saturday’s impacts
Storm Dave caused fallen trees, travel disruption, power cuts and ferry cancellations across parts of the UK.
Road closures
Several roads were blocked by trees or debris.
Scotland
Traffic Scotland continued reporting restrictions around major routes and bridges.
Queensferry Crossing
Wind restrictions affected the M90 crossing.
Forth Road Bridge
The nearby crossing also faced controls.
Why bridge restrictions can remain after a warning changes
Operators use local wind measurements rather than relying only on the colour of a national warning.
Rail disruption
ScotRail and other operators reported delays and restrictions.
Why trains do not instantly return to full speed
Lines may need inspection for fallen trees, damaged overhead equipment or debris.
East Coast Main Line
Some services experienced disruption linked to the storm and speed restrictions.
Why timetable recovery can take hours
A delayed train and crew may then be in the wrong place for a later service.
Power cuts
Electricity networks continued restoring supplies to homes affected by Saturday’s winds.
Why restoration can lag behind the weather
Engineers need to locate faults and repair physical damage safely.
Snow
Higher parts of Scotland had seen late-season snow during the storm.
Why snow can remain after wind warnings lift
Cold ground and elevation can preserve lying snow and ice.
Mountain conditions
Walkers still needed to use specialist forecasts rather than assuming a national warning ending made the hills safe.
Rain and saturated ground
Western areas had also received significant rainfall.
Why trees remain vulnerable
Wet soil can reduce root stability after a windstorm.
Peak wind observations
Later Met Office analysis identified a 93mph gust at Capel Curig during the event.
Why early Sunday articles sometimes quoted lower figures
Live reports are written before all observations have been collected and quality checked.
66mph figure
Some early PA reports referenced 66mph at Capel Curig based on data available at the time.
Why the updated figure should now be used
A retrospective article should prefer the final Met Office post-event analysis.
Aberdaron
The post-storm summary recorded an 83mph gust.
St Bees Head
Cumbria reached around 75mph.
Snow depth
Loch Glascarnoch recorded around 6cm of lying snow.
Rainfall
Glen Ample recorded around 50mm through the storm period.
Why Easter timing mattered
Millions of leisure journeys were planned across the holiday weekend.
Return journeys
Some travellers were beginning to move again on Easter Sunday as conditions improved.
Why checking before leaving still mattered
A route could remain closed even after local weather became calmer.
Ferry services
Operators needed time to restore timetables following cancellations.
Air travel
Strong crosswinds can disrupt aviation, but impacts differ greatly by airport and runway.
Why national forecasts cannot predict each flight
Airlines use live wind, aircraft and operational data.
Outdoor events
Easter attractions and activities could reopen as conditions improved.
Why local checks mattered
Individual parks, heritage sites and events might still have closed paths or damage.
Was Sunday a completely dry day?
No.
The main storm moved away, but showers remained widespread.
Why showers can be heavy after a low clears
Cold unstable air behind a weather system can generate convective showers.
Sunshine between showers
That produces rapidly changing spring conditions.
Why the storm was historically notable
The Met Office later called it the most severe April windstorm since the UK’s naming system began in 2015 based on widespread high gusts.
Why that is not an all-time record
Older April storms produced stronger individual gusts before the naming system existed.
Recovery phase
Post-storm work included power restoration, tree removal and transport inspection.
Insurance claims
Property owners affected by wind damage needed to document damage and contact insurers.
Why immediate safety comes first
People should avoid unstable roofs, trees and fallen cables while taking photographs.
Flooded roads
Standing water may remain after heavy rain even in sunshine.
Why drivers should not enter unknown floodwater
Depth and road condition can be difficult to judge.
What “all clear” actually meant
Warnings expiring indicated that the forecast severe-weather threshold had passed.
It did not guarantee every local hazard had disappeared.
Why this is the right way to update the page
The original article looked forward to conditions easing.
We now know that warnings were lifted as expected while residual disruption continued.
Conclusion
Storm Dave eased across Easter Sunday as the main low moved northeast and weather warnings expired.
The worst wind threat passed, but rail delays, bridge restrictions, power restoration and difficult mountain conditions did not disappear instantly.
Later Met Office data also showed the storm had been more severe than some early Sunday figures suggested, including a 93mph peak gust at Capel Curig.
The accurate historical picture is therefore one of improving weather alongside a slower infrastructure recovery.
Sources and further reading
See ITV News’ Easter Sunday update and the Met Office post-storm analysis.
Why post-storm travel disruption can last a full day
Transport networks are highly interconnected. A blocked railway can leave trains and crews displaced, while a cancelled ferry can mean the vessel is no longer positioned for the next scheduled sailing.
Why road reopening can be slower than tree removal
After a fallen tree is cut away, authorities may still need to inspect barriers, power cables or the road surface before declaring the route fully safe.
Why bridges use their own local wind thresholds
National forecasts describe broad areas, while bridge operators have instruments on or near the structure. Restrictions can therefore remain even after a wider warning expires.
Why high-sided vehicles may face longer restrictions
A wind speed manageable for a low car can still be dangerous for a lorry or caravan because of the larger side area exposed to crosswinds.
Why showers mattered after Dave
The storm’s departure did not produce settled high pressure. Unstable air behind the low created showers, meaning conditions could switch quickly between sunshine, hail, rain and gusts.
Why mountain users had to remain cautious
Upland snow, saturated paths and residual strong wind can persist long after conditions improve in towns and valleys.
Why the final 93mph figure changed the historical record
Early reports naturally relied on observations available during the event. The later Met Office review consolidated verified station data and provided a more authoritative peak figure.
Why this does not mean early reports were dishonest
Weather reporting evolves as observations arrive. Live figures should be understood as provisional when the event is still unfolding.
Why Easter Sunday recovery was economically important
Hotels, attractions, restaurants and transport operators had already faced cancellations. Improving weather allowed some holiday activity to resume rather than losing the entire weekend.
Why travellers still needed flexibility
A national forecast of improvement could not guarantee a specific train, ferry or road would operate normally. Checking the operator remained essential.
Why insurance claims often begin after the storm
People may not safely inspect roofs, fences or vehicles until winds drop. Damage totals therefore become clearer only during the recovery phase.
The difference between meteorological recovery and infrastructure recovery
The atmosphere can improve in hours, while repairing power lines, clearing trees and restoring timetables may take much longer.
Why the page remains useful
It documents the transition from warning to recovery and explains why “warnings lifted” should never be interpreted as “every consequence is over”.
Why recovery messaging matters after severe weather
Authorities have to communicate two ideas at once: the main meteorological danger is reducing, but local hazards may remain. That balance helps people resume normal activity without assuming roads, railways, hills and power networks are instantly back to normal.
Storm Dave’s Easter Sunday transition illustrated that distinction clearly. The official warnings ended during the morning, while transport operators and engineers continued dealing with the consequences left behind.