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records: The highest daily maximum temperature recorded in the UK and Wales for November was 22.4°C at Trawsgoed (Ceredigion) on 1 November 2015. England’s highest November daily maximum was 21.1°C, observed at several locations including Cambridge Botanic Gardens, Writtle (Essex), Tottenham (London

on radar came not from the skies, but from the ground, or rather, just above it. Back in July, swarms of flying ants were picked up on radar, appearing as strange, flashing echoes to the northwest of London. These were initially mistaken for showers, but closer inspection revealed their true identity

in heatwave territory. For a heatwave to be officially recognised, temperatures must exceed specific thresholds for three consecutive days. These thresholds vary by region: 28°C in London and the southeast, 27°C in parts of the Midlands, and 25°C across much of Wales, northern England, Scotland, and Northern

between Reading and London, with a peak near Guildford. A corridor from Bristol through Birmingham to Manchester. Parts of Essex and Suffolk. These hotspots are partly due to population density, more people means more chances for tornadoes to be observed and reported, but they also reflect genuine

the next 48 hours across UK Domestic Airspace, to support situational awareness and planning (including staffing). A tactical (0-3 hour) trajectory-style forecast, and supplementary Meteorologist-written commentary issued ahead of and during convective weather activity within the London Terminal

. Winds begin to change direction, potentially ushering in warmer air to London and the south-east, where temperatures could climb to 23 or even 25°C, depending on wind orientation. However, conditions remain much less pleasant across north-western parts of the UK. READ MORE: Hurricanes, typhoons

Wales and southwest England, and over 30°C in eastern England. Monday is expected to be the hottest day of this spell, with highs of 32-34°C possible in southeast England, including London and Cambridge. Scotland and Northern Ireland will also feel warmer than on Sunday as the warm air spreads further

for the seasonal mean temperature • Medians increases with rarity, because 1-in-100 year events are by construction higher than 1-in-20 or 1-in-50 year events • Uncertainty ranges in return level also increase slightly with return period Figure 1 A comparison of summer daily maximum temperature for a London

Office in January 2011. Prior to this she was Content Developer at the London Science Museum, contributing to the Atmosphere exhibition focused on the complex science behind climate change and our options for adaptation and mitigation responses.  Nicola also spent time in Australia working at Monash

as WAFC London and NOAA as WAFC Washington. In the 1990’s the WAFCs and their WAFS were mature enough that the regional area forecast centres were closed. Evolving technology Over the years, our services have continuously evolved to meet the changing needs of the aviation industry: 1990s: We developed