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and climate consultancy Insights About us Who we are, what we do and organisational news. Who we are Who we are Our people Our values Our history Accuracy Innovation Impact How we are run How we are run The Met Office Board Our governance structure Public Weather Service Our Chief Executive

-8.2 °C Pershore (Worces.) -9.0 °C Lincoln (Lincolnshire) 2010 1981 25 Dec 31 Dec Wales -7.8 °C* Llysdinam (Powys) -5.5 °C Moel Cynnedd (Powys) 2010 1978 Altnaharra 21 Dec Fyvie Castle 29 Dec Scotland -13.8 °C -15.9 °C (Highland) 2010 (Aberdeenshire) 1995 Northern Edenfel (County 23 Dec Boom Hall

Abbey 1961-1975 MET/15/112/ Portavogie 1964 MET/15/113/ Portrush 1959-1967 MET/15/114/ Reagh Island 1960-1971 MET/15/115/ Roscor 1962-1972 MET/15/116/ Rosetta 1963-1974 MET/15/117/ Rowallane 1963-1964 MET/15/118/ Somerset Forest 1961-1972 MET/15/119/ Stormont Castle 1950-1980 MET/15/120/ Violet Hill

frequent over the north and west. Very warm and sunny weather spread from the south on the 25th and 26th, with a high of 29.1°C at Floors Castle (Roxburghshire) on the 25th, but on the 26th central and western areas had more cloud, with rain for the far north-west and Western Isles. The 27th

on the 24th, which was a cooler cloudier day in the west, but a warm and sunny one further east. Sunny and hot weather became established widely on the 25th with maxima of 31.6 °C at Edinburgh Gogarbank and Floors Castle (Roxburghshire). Thunderstorms again broke out in the evening, mainly

, with 10.1 hours of sunshine at Kinloss (Morayshire) and a high of 22.3 °C at Floors Castle (Roxburghshire). The night of the 10th/11th was very warm and the temperature did not drop below 14.8 °C at Aultbea (Ross & Cromarty). The 11th started dry and bright in many areas but an area of heavy rain

. Most places were dry, sunny and warm between the 19th and 22nd with a high of 24.8 °C at Floors Castle (Roxburghshire) on the 20th, but the 21st was generally cloudier; the north-west however was cloudier and some rain spread into the far north-west on the 19th, persisting on the 20th and 21st

and climate consultancy Insights About us Who we are, what we do and organisational news. Who we are Who we are Our people Our values Our history Accuracy Innovation Impact How we are run How we are run The Met Office Board Our governance structure Public Weather Service Our Chief Executive

and climate consultancy Insights About us Who we are, what we do and organisational news. Who we are Who we are Our people Our values Our history Accuracy Innovation Impact How we are run How we are run The Met Office Board Our governance structure Public Weather Service Our Chief Executive

, Indian Ocean Dipole, Atlantic Multi-decadal Variability).   Furthermore the density and hence thermal capacity of the oceans is around 1000 times that of the atmosphere. As a result, water moves much more slowly in the oceans (i.e. currents) than the air does in the atmosphere (i.e. winds). Combined