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of the management of climate risks, and develop and delivery climate services. Find out more about the publication.  UK Climate Resilience Final Conference - March 2023 The final conference of the programme took place in London on 8-9 March. This hybrid event was an opportunity to celebrate

expertise sited on the UoR campus. � � � � � � � � � � Guests from London Economics presented the pre-final draft of the report they had been working on with Kristina Costar (Principal Economist). The draft had calculated the Met Office delivered an18.7 times benefit per pound of public investment

Met Office Board Summary 30 November 2022 Held at Microsoft, Paddington, London • Rob Woodward (Chair) welcomed attendees and confirmed the meeting was quorate. He welcomed Damitha Adikaari (Director - Science & Innovation for Climate & Energy (SICE), BEIS) and Felicity Howe from the BEIS

A Brief Summary of L5 Mission Concepts Nat Gopalswamy NASA/GSFC L5 Consortium Meeting, London, May 11-14, 2015 Dst Mariner 2: Off & Above the Sun-Earth Line 1962/10/07 15:46 UT C P Sonett (1924 -2011) Mariner II IP shock followed by a Sudden Commencement 4.7 h later - confirmed Gold (1953

* 3 35.6 South Farnborough Hampshire 36.2 3 35.9 Reading (Whiteknights) Berkshire 35.5* 3 35.0 Hawarden Bridge Flintshire 35.2 2 33.0 Newport Shropshire 34.8 3 32.0 Sutton Bonington Nottinghamshire34.8 3 32.8 Nottingham (Watnall) Nottinghamshire34.6 3 33.8 Hampstead Greater London 34.6* 3 34.4

Towards a global sulphur dioxide forecast capability for aviation Witham, C.; Kristiansen, N.; Beckett, F.; Marenco, F. 2021 647 Investigating How the Choice of Stratospheric Meteorological Data Influences Volcanic Ash Forecasts Within the London VAAC Area of Responsibility Stebbing, N,; Beckett, F

. The all-time record in the UK is 38.5° C at Faversham on 10 August 2003.  The dry spell has been most prolonged in East Anglia and Southeast England. Most especially much of East Anglia and Cambridgeshire, extending through Essex into London and also around Bournemouth and Southampton.  Parts

and the Channel Islands. The main factor determining the distribution of temperature is nearness to the coast, particularly the west coast. Temperatures are lower inland than near the coast. In July, the warmest areas are around London, and the coolest are in parts of Scotland. Areas near the coast

maxima occur in the London area (23.5 °C) whilst the lowest occur in the Shetlands (15 °C). Maximum temperatures are normally 2 or 3 hours a er midday. Extreme maximum temperatures can occur in July or August. For example, on 3 August 1990 a temperature of 34.5 °C was recorded at Knutsford

Met Office to support occasional AIB reports where Met was likely an element and we feed that back into our services e.g. after the Vauxhall helicopter accident, a safety recommendation was that more Met was required over London, Met Office produced London CTA product as a direct result of this AIB