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This relationship is apparently non\u2010linear indicating that snow cover duration is especially sensitive to a defined mean temperature range. Secondly, that snow cover can be rather variable from year to year, or over multi\u2010year phases. This variability has been related to the frequency of synoptic\u2010scale atmospheric circulation patterns including the North Atlantic Oscillation. These two features are used to contextualise recent and likely future trends in snow cover. It is suggested that there may be different patterns of variability in some mountain areas compared to the adjacent lowlands. This is associated with combined effects of temperature and precipitation during exposure to different air masses. Suggestions are made for improving snow cover observations to further investigate these issues.<\/jats:p>","DOI":"10.1002\/wea.3625","type":"journal-article","created":{"date-parts":[[2020,1,9]],"date-time":"2020-01-09T19:30:36Z","timestamp":1578598236000},"page":"61-66","update-policy":"http:\/\/dx.doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":2,"title":["Snow cover variability in Great Britain during a changing climate"],"prefix":"10.1002","volume":"75","author":[{"given":"Iain","family":"Brown","sequence":"first","affiliation":[{"name":"Department of Geography and Environmental Science University of Dundee  Dundee UK"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"311","published-online":{"date-parts":[[2020,1,9]]},"reference":[{"key":"e_1_2_9_2_1","doi-asserted-by":"publisher","DOI":"10.1002\/wea.2731"},{"key":"e_1_2_9_3_1","doi-asserted-by":"publisher","DOI":"10.1007\/s10584-016-1637-x"},{"key":"e_1_2_9_4_1","doi-asserted-by":"publisher","DOI":"10.1038\/s41558-018-0318-3"},{"key":"e_1_2_9_5_1","doi-asserted-by":"publisher","DOI":"10.1002\/joc.6090"},{"key":"e_1_2_9_6_1","doi-asserted-by":"publisher","DOI":"10.1175\/2008JCLI2665.1"},{"key":"e_1_2_9_7_1","doi-asserted-by":"publisher","DOI":"10.1002\/wea.3367"},{"key":"e_1_2_9_8_1","doi-asserted-by":"publisher","DOI":"10.1002\/wea.3474"},{"key":"e_1_2_9_9_1","doi-asserted-by":"publisher","DOI":"10.1002\/wea.2503"},{"key":"e_1_2_9_10_1","doi-asserted-by":"publisher","DOI":"10.1029\/2018GL079799"},{"key":"e_1_2_9_11_1","doi-asserted-by":"publisher","DOI":"10.1002\/wea.3469"},{"key":"e_1_2_9_12_1","doi-asserted-by":"publisher","DOI":"10.1002\/joc.1472"},{"key":"e_1_2_9_13_1","doi-asserted-by":"publisher","DOI":"10.1080\/00369229318736875"},{"key":"e_1_2_9_14_1","doi-asserted-by":"publisher","DOI":"10.1080\/00369220118737130"},{"key":"e_1_2_9_15_1","doi-asserted-by":"publisher","DOI":"10.1002\/j.1477-8696.1978.tb04689.x"},{"key":"e_1_2_9_16_1","doi-asserted-by":"publisher","DOI":"10.1256\/wea.47.04"},{"key":"e_1_2_9_17_1","doi-asserted-by":"publisher","DOI":"10.1177\/0309133316650617"},{"key":"e_1_2_9_18_1","doi-asserted-by":"publisher","DOI":"10.1002\/wea.3390"},{"key":"e_1_2_9_19_1","doi-asserted-by":"publisher","DOI":"10.1002\/qj.49706527803"},{"key":"e_1_2_9_20_1","volume-title":"Climate and the British Scene","author":"Manley G","year":"1952"},{"key":"e_1_2_9_21_1","first-page":"619","article-title":"Scottish snow cover dependence on the North Atlantic Oscillation index","volume":"47","author":"Spencer M","year":"2016","journal-title":"Hydrol. 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