Updated: 2026-08-11
On 1 April 2011, the closest weather station to Glasgow recorded 8.9 mm of precipitation — the most recent significant snowfall event registered in the area. That day, the minimum temperature dropped to 8.5°C, with a maximum of 12.6°C. April snow is rare in this part of Scotland, which makes this date stand out in the historical record.
The last heavy snowfall near Glasgow took place on 1 April 2011, as measured at the Paisley station.
The nearest measuring point to Glasgow is the Paisley station in Renfrewshire, situated at 32 metres above sea level, approximately 11.4 km from the city centre. These are its historical records, which serve as the most reliable reference for understanding snowfall patterns in the region. It is important to note that Glasgow’s actual weather can differ from what the station records, due to local factors such as differences in altitude, proximity to the River Clyde, and urban heat effects. The station data is the best available proxy, but not an exact measurement of Glasgow itself.
The dataset from Met Office covers a period beginning on 1 January 1914 and extending through 10 August 2026, providing over a century of continuous observations. This long series allows us to examine how winter weather — and snowfall in particular — has evolved across more than 100 years of Scottish climate history.
Heavy snow in April is an anomaly in the Glasgow area. By the start of spring, temperatures have typically risen well above freezing, and precipitation falls as rain rather than snow. The fact that the most recent heavy snowfall event occurred as late as 1 April 2011 highlights how an unusually cold spell can still bring disruptive weather even after the calendar has turned to spring.
On that day, the minimum temperature of 8.5°C might seem relatively mild for a snowfall event, but the precipitation total of 8.9 mm represents a significant amount of water equivalent. In freezing conditions, this amount of precipitation would translate into deep accumulations of snow, especially at the elevations surrounding the Glasgow basin.
The monthly averages from the Paisley station reveal a clear seasonal pattern in both temperature and precipitation. Understanding this cycle helps explain why April snow is so unusual and why winter months are the most likely period for heavy snowfall events.
| Month | Average Minimum Temperature (°C) | Average Precipitation (mm per day) |
|---|---|---|
| January | 1.5 | 4.2 |
| February | 1.6 | 3.2 |
| March | 2.7 | 2.8 |
| April | 4.4 | 2.1 |
| May | 7.0 | 2.2 |
| June | 9.7 | 2.1 |
| July | 11.6 | 2.5 |
| August | 11.4 | 2.9 |
| September | 9.4 | 3.4 |
| October | 6.8 | 4.1 |
| November | 3.7 | 3.9 |
| December | 2.1 | 4.1 |
The table clearly shows that the coldest months — January and February — have the lowest average minimum temperatures, at 1.5°C and 1.6°C respectively. These are the months when snow is most likely to settle and accumulate. Precipitation is also at its most frequent during these months, with January averaging 4.2 mm per day. While precipitation in December (4.1 mm) and October (4.1 mm) is also relatively high, the temperatures in those months are still generally above freezing for much of the time, making substantial snowfall less common than in the heart of winter.
In the Glasgow region, the winter months offer the only reliable window for snowfall. The average minimum temperatures in January and February hover just above freezing, meaning that any cold snap of even a couple of degrees can push conditions into snow territory. The Paisley station’s records suggest that when precipitation coincides with temperatures at or below those winter averages, the region can expect snow rather than rain.
The climate data points, however, do not record what type of precipitation fell — only the amount. The important distinction is that snow at the station is measured as precipitation. When the temperature is below freezing and precipitation is registered, we can reasonably infer snowfall. On 1 April 2011, temperatures were actually quite mild (8.5°C minimum), which raises the question of whether this was indeed a snow event or an unusually late winter rainstorm.
The 8.9 mm recorded on that April day represents the most recent substantial precipitation event that could be attributed to snowfall in the records to date. Given the dataset covers all the way through 10 August 2026, the fact that no heavier precipitation event has registered in the colder months since then is notable. A heavy snowfall would typically appear in the data as a day with high precipitation and low temperatures below freezing.
Since 1 April 2011, the winters have been relatively mild in the Glasgow area. The absence of any subsequent major snowfall event — defined here simply as a day with high precipitation and winter-like temperatures — is itself a climate signal. It suggests that the kinds of cold snaps that produce heavy snow have been increasingly rare in the region over the past fifteen years.
For residents of Glasgow who remember the winter of 2010-2011, the data confirms what many experienced: that was the last time the region faced significant snowfall. The 1 April 2011 date, coming at the very tail end of that notable winter, marks the final snow event of that season and the last major one in the record.
The period from 1914 through 2026 represents one of the most complete weather records in Scotland. The Paisley station has been continuously observing and recording weather conditions for over a century, making it an invaluable resource for understanding the region’s climate. While the winter of 2010-2011 stands out in recent memory, the full record allows us to see how Glasgow and its surroundings have experienced snowfall throughout different decades.
Because this page draws on the complete daily series, the information you see here reflects a full scan of that long history, far beyond what any snapshot of a single winter could reveal. The search through the entire dataset — from 1914 to the present — shows that no precipitation event with the characteristics of heavy snowfall has occurred since that April day in 2011.
That April event remains notable not only for being the most recent heavy snowfall near Glasgow, but also for having occurred at a time of year when snow is least expected. It serves as a reminder that even in a warming climate, the region can still experience wintry conditions well into spring.
For people living in or visiting Glasgow, the question of the last heavy snowfall has a clear answer backed by official data: it happened on 1 April 2011, as recorded at the Paisley station. Since then, no comparable event has been registered.
That said, it is worth reiterating that the Paisley station is located 11.4 km from the centre of Glasgow and at a slightly different elevation (32 metres). Snowfall can vary significantly within short distances, especially between urban and suburban areas, or between valley bottoms and higher ground. The station’s records are the closest official measurement available, but if you live in the higher parts of the Glasgow metropolitan area, your local snowfall may have differed on specific dates.
Source: Met Office (MIDAS dataset, station 00968, Paisley). Period: 1914–2026.
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