Scottish snow cover dependence on the North Atlantic Oscillation index

• Published in: Hydrology Research
• Main Authors: Michael Spencer, Richard Essery
• Format: Article in Journal/Newspaper
• Language: English
• Published: IWA Publishing 2016
• Subjects: climate; north atlantic oscillation; scotland; snow; River; lake; and water-supply engineering (General); TC401-506; Physical geography; GB3-5030; Snow River; North Atlantic; North Atlantic oscillation
• Online Access: https://doi.org/10.2166/nh.2016.085; https://doaj.org/article/4c4e5740892f4af9809dd300d45aada4

Forecasting seasonal snow cover is useful for planning resources and mitigating natural hazards. We present a link between the North Atlantic Oscillation (NAO) index and days of snow cover in Scotland between winters beginning from 1875 to 2013. Using broad (5 km resolution), national scale data sets like UK Climate Projections 2009 (UKCP09) to extract nationwide patterns, we support these findings using hillslope scale data from the Snow Survey of Great Britain (SSGB). Currently collected snow cover data are considered using remotely sensed satellite observations, from moderate-resolution imaging spectroradiometer; but the results are inconclusive due to cloud. The strongest correlations between the NAO index and snow cover are found in eastern and southern Scotland; these results are supported by both SSGB and UKCP09 data. Correlations between NAO index and snow cover are negative with the strongest relationships found for elevations below 750 m. Four SSGB sites (two in eastern Scotland, two in southern Scotland) were modelled linearly with resulting slopes between −6 and −16 days of snow cover per NAO index integer value. This is the first time the relationship between NAO index and snow cover duration has been quantified and mapped in Scotland.