At a height of 848 metres (2,782 ft), Great Dun Fell is the second-highest mountain in England's Pennines, lying two miles (three kilometres) south along the watershed from Cross Fell, its higher neighbour. Together with its smaller twin, Little Dun Fell, which reaches 842 m (2,762 ft),[1] it forms a stepping-stone for the Pennine Way on its long climb up from Dufton. It lies within the historic county boundaries of Westmorland, the ceremonial county of Cumbria, and the modern unitary authority area of Westmorland & Furness.
The construction of the radar station led to the repaving of a tarred road to the summit, which became Britain's highest road. This road is marked as private from just above the village of Knock, and is not open to public motor vehicles. However, it is a bridleway until shortly before the radar station, so it is open to walkers, cyclists and horseriders.[2]
Field station
The University of Manchester formerly had a permanent meteorologicalobservatory at the Great Dun Fell site. It has hosted a number of field experiments doing research into clouds and their interactions with pollution. As the summit is in cloud for two thirds of the year it is an ideal location for this type of research. The university still has the option to use the site for short-term measurement periods.[3]
Under the Köppen climate classification, Great Dun Fell has a subpolar oceanic climate (Cfc), closely bordering both a subarctic climate (Dfc) under the 0 °C (32 °F) isotherm and an alpine tundra climate (ET) due to a July mean of exactly 10 °C (50 °F). The Met Office station publishes only temperature and frost averages. The summers are cool due to elevation. Considering its elevation and a latitude of over 54 degrees, winters are relatively mild due to oceanic influences.[4]
Climate data for Great Dun Fell 847 m (2,779 ft), 1991-2020 averages, 2000–present records.[a]