Weather records dating back 140 years could help scientists better predict heavy snowfalls in Scotland, a study shows.
Analysis of the logged data has revealed how closely snowfall in Scotland is linked to a weather phenomenon in the Atlantic Ocean.
The finding could lead to improved forecasting that benefits local authorities and transport bodies, as well as businesses associated with snow sports.
The study is the first to show how large scale changes in air pressure in the North Atlantic can have a direct impact on where - and for how long - there will be snow in Scotland.
The phenomenon - measured by the North Atlantic Oscillation index, or NAO - was already known to influence weather conditions in northern Europe.
When NAO readings indicate high pressure, northern Europe tends to experience mild conditions owing to incoming warm, westerly winds.
Low index readings suggest cold air is likely to blow across the continent from the east, bringing with it more wintry conditions.
By comparing snowfall records which began in 1875 with NAO index readings over the same period, University researchers gauged the impact of pressure changes on snow cover.
Until now, the link between the two was poorly understood.
The study shows that - between 1875 and 2013 - low-lying regions of Scotland were more likely to be covered with snow when the NAO index was low. Conversely, when the index was high, areas below 750m were largely unaffected by snow.
The link was strongest in the south west, where most land is less than 750m high, and eastern areas, which are the most exposed to easterly air flows, the team says.
In inland areas where much of the land is higher, the link is not as pronounced as low temperatures mean snow can fall regardless of changes in North Atlantic air pressure.
The study, published in the journal Hydrology Research, was funded by Natural Environment Research Council.
As seasonal forecasts of the North Atlantic Oscillation continue to improve, earlier and more informed predictions of snowfall will be possible.