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Last updated: 20:00, 5 Oct 2026
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Longridge sits below Longridge Fell in the Ribble Valley, a few miles north-east of Preston, with Jeffrey Hill and the open moorland rising steeply behind the town. That height means the fell often catches rain that the Ribble Valley floor below misses. That is where a Longridge rain radar helps most, since hyperlocal radar reads the live position of the rain instead of an area forecast.
Showers reach Longridge off the Irish Sea and lift sharply over the fell behind the town, so Jeffrey Hill and the moorland can be soaked while the town centre in the valley below stays comparatively dry. Atlantic fronts cross the Irish Sea, pick up moisture and meet the West Pennine Moors and the Pennine ridge. Orographic lift turns moderate rain into heavy rain over the hills, and the Mersey and Irwell valleys funnel that runoff towards the cities.
RainViewer draws the live rain radar for Longridge, England, from Met Office data, with real-time rain refreshed on every 5-minute radar update. The live map shows whether a shower has crossed the top of Longridge Fell or is still climbing towards Jeffrey Hill, a hyperlocal detail that a Lancashire-wide forecast does not give.
Autumn and winter fronts pile up against Longridge Fell, and the moorland roads above the town are the first to feel the worst of it. Named storms and repeated fronts arrive from the Atlantic, and the ground stays saturated for weeks. The Irwell, Mersey and Ribble respond quickly, and moorland roads and low-lying streets flood first.
The last fronts of the season mix with cold showers, hail and wet snow over the tops. Because these showers are so narrow, forecasts often miss the exact timing, leaving hill walks and weekend sport the most exposed to a sudden change. Spring showers cross the fell quickly, and walks up towards Jeffrey Hill are the plans most often cut short.
Showers become less frequent, but the warm plain still builds thunderstorms over the Pennines that then drift toward the cities. Outdoor events and seafront trips depend on finding a short dry gap, because a storm cell can be at the coast within the hour. Summer showers are lighter, but thunderstorms can build over the fell on warm afternoons and catch walkers on the open moor.
The open moorland above Longridge catches rain well before the town does, and there is no shelter once above the treeline. Checking the radar before setting out shows whether the fell is already in cloud and rain.
Longridge's market and high street sit in the sheltered valley below the fell, and a shower on the moor above does not always reach the town at the same time. A look at the radar shows what is actually falling in the centre.
The road from Longridge down towards Preston slows in heavy rain, and spray builds where it drops off the fell towards the valley floor. Checking the radar before setting off helps decide whether to leave now or wait a few minutes.
The steep lanes up Longridge Fell are exposed once above the town, and a shower can arrive on the tops well before it reaches lower ground. Watching the cell on the radar helps time the climb for a dry spell.
RainViewer shows UK precipitation using data from the Met Office, the national weather service, which runs a network of C-band dual-polarization weather radars. The Met Office network also feeds the European OPERA composite, and the RainViewer map refreshes with each new scan, about every 5 minutes. From Longridge the map also covers Preston, Clitheroe and Chorley.
Longridge Fell rises steeply behind the town and catches showers off the Irish Sea before they reach the valley floor, so the moorland can already be wet while Longridge itself is still dry. Walkers heading for Jeffrey Hill check the radar rather than the forecast for the town. RainViewer shows the shower lifting over the fell before it clears the top.
Yes, the road down from Longridge towards Preston slows in heavy rain, and spray builds where it descends off the fell onto the valley floor. Check the radar before heading out. RainViewer shows whether the cell is still on the tops or already down at valley level.
Longridge itself sits on the lower slopes of the fell and drains reasonably well, but heavy rain on the moorland above can send fast runoff down the lanes into the town after a downpour. The open fell holds very little water itself. The radar shows whether a heavier band is still crossing the tops.
May to August is the best window to visit Longridge, when the fell paths towards Jeffrey Hill are driest underfoot. The moorland can still catch showers that miss the town in spring. Look at the radar early and fit the walk into the gap.
The fell behind Longridge lifts approaching showers off the Irish Sea and takes the first and heaviest of the rain, while the town centre in the sheltered valley below can stay dry until the band finally drops down. Live radar shows the edge of each cell, so checking Longridge Fell and the town centre separately shows which side of the line you are on.
The Longridge radar in RainViewer uses Met Office data, updated every 5 minutes, to show precipitation as it falls rather than a modelled prediction. Met Office C-band radars in northern England measure the bands before they reach the Pennine slopes, and dual-polarization data helps separate heavy rain from sleet on the tops. That hyperlocal radar picture shows where a shower starts and stops, which a forecast cannot.
Set a rain alert on Jeffrey Hill or the town centre and RainViewer warns you before rain arrives, which settles whether to start the climb now or wait it out below. The 2-hour forecast in 5-minute slices shows the next gap, and saved locations track the fell and the valley together.
A walk up to Jeffrey Hill and an afternoon on Longridge's high street both depend on a dry gap, and RainViewer shows the next one.
Showers reach Longridge from the west and stall against the Pennines, so the timing shifts from one hour to the next.
Your forecast for Longridge says rain this afternoon. RainViewer's live hyperlocal radar shows the cell still climbing the fell above the town with the centre still dry, which decides whether the walk starts now.
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Two hours of 5-minute steps let you time the walk up to Jeffrey Hill to the minute.
Put an alert on Longridge Fell. RainViewer warns you minutes ahead, which settles whether to start the climb now or wait it out below.
Rain reaches Longridge most often from the west and south-west, off the Irish Sea, so the arrows tell you at a glance whether a cell is heading your way.
The 48-hour history shows what fell on Longridge Fell and the moorland above, which is the fastest way to judge ground conditions.
Save Longridge Fell, Jeffrey Hill and Longridge town centre and check all three in one look.