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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

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

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

January 1979 and -18.2 °C at Lacock, Wiltshire on 13 December 1981. On the latter date, -11.8 °C was recorded at Heathrow (Greater London), whilst at St James's Park (Central London) the temperature fell no lower than -7.0 °C. July is the warmest month, with mean daily maximum temperatures in the London

-Soar where a caravan park had to be evacuated. Colder air then returned and the following week saw some severe overnight frosts (-18.9C at Altnaharra, northern Scotland on the 11th) and further snow showers. More widespread snow affected parts of southwest England on the 8th, resulting in an amber

: A maximum temperature of 22.9 °C was recorded at Thornes Park (West Yorkshire) on the 8th. A minimum temperature of -3.6 °C was recorded at Redesdale Camp (Northumberland) on the 16th. In the 24 hours ending at 0900 UTC on the 28th, 222.6 mm of rain fell at Honister Pass (Cumbria). A wind gust

a dry start, rain spread slowly from the west during the 4th, becoming widespread and occasionally heavy through the afternoon, Crai Reservoir (Powys) recording 87.8 mm. It was a mild night into the 5th, Cardiff Bute Park not falling below 16.4 °C, then there was widespread rain all morning, heavy