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and vocabulary to describe the weather for over 40 years and it’s important that they are still relevant. It’s become apparent from recent studies that different regions interpret language and information uniquely. For example, in January we found that two-fifths of people living in London described

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

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

times in the same period.  RCP 8.5 is a pathway where greenhouse gas emissions keep accelerating. This is not inevitable, but a plausible scenario if we do not curb our emissions. An example of an intense rainfall event with 20mm/hr is London in July 2021, when 40mm of rain fell over three hours at Kew

IAP missions in China facing a changing world Guoxiong Wu Institute of Atmospheric Physics, Chinese Academy of Sciences, China The WCSSP Workshop, 23 rd Sep, 2019, London, UK Contents • IAP at a Glance • The Climate Challenge facing in China • Research related to the “Challenge” at IAP • Future

people, with 63% of those eligible saying they would check on neighbours or relatives. Wales is next with 60%, the Midlands reached 57%, Scotland 56%, southern England and eastern England each reached 52%. London had just 44% of those who were eligible stating that they would check on a vulnerable

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

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

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

High Energy Radiation Impacts on Ground Level, Aircraft and Space Electronics The Need for an L5 Measurement Package 11-14 May 2015 L5 Consortium Meeting London K A Ryden Prof. C. S Dyer* University of Surrey (Space Centre) * Date and CSDRadConsultancy Ltd “Sic Itur Ad Astra.” © Copyright QinetiQ