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................................12 Climate change We’re causing it, so let’s tackle it...14 00.13 GMT: Just past midnight and local authority duty-officer Karen Johnson is roused from sleep by an important text. It’s the Flood Forecasting Centre in London confirming extreme rainfall in just two hours

on the ground, mounted on an aircraft or satellite-based, and can be used to observe the location and vertical profile of aerosols such as volcanic ash. A lidar measures backscattered light from atmospheric targets e.g. aerosols including volcanic ash and Saharan dust, water droplets and ice crystals, using

totals are based on the average value across each county. Lead author and Met Office climate scientist, Mike Kendon, said: “Our new analysis of these observations really shines a light on the fastest changing aspects of our weather as a consequence of climate change. Long term averages can be difficult

restrictions in coastal waters; such as in the Moray Firth and Firth of Forth during prevailing westerly wind conditions. The Pentland Firth is also resolved by multiple cells in the model, although the addition of current information would be needed in order to properly represent wave growth and dissipation

PWSCG (36) Meeting 10:30 – 16:00 Wednesday 27 th April 2016 BIS Conference Centre, 1 Victoria Street Minutes Wyn Williams (WW) Denise Harker (DH) Mike Gray (MG) Paul Riches (PR) Sarah Jackson (SJ) Alessia Morris (AM) John Irvine (JI) Colin Hord (CH) Nathan Travis (NT) Ben Fletcher (BF) Andy

in the first two weeks roughly 2°C below average. The cool start to the month was due to northerly and northwesterly winds bringing cold Arctic air across the UK. A low pressure centre developed over Scandinavia in the second week of June, pushing further cold air from the north across the UK. Frontal

The intensive testbed with its main hub in Zambia and centres in Mozambique and South Africa, hit the ground running on 30 January 2025.

and nowcasts – sent every two hours. The morning’s forecasts predicted some heavy rainfall for Kanyama. While the team at ZMD experienced two brief but heavy showers during the morning, the Kanyama community observers reported that they experienced only light rain. This led to a discussion about how

for Tuesday and Wednesday. Weather over past Coronations Data from the Met Office archive shows that past coronations back to Edward VII have been mixed when it comes to the weather. The Coronation of HM Queen Elizabeth II saw temperature highs of just 11.8°C on 2 June 1953 with some light rain through

mid-morning, spreading northeast through the day. Winds will be light at first but will widely become strong from the southwest, with gales, possibly severe, developing in many western coastal areas. After a cold start, with a widespread grass frost and local air frost, daytime temperatures

at times. Winds will be fresh to strong in the north and northwest early on, easing through the morning. Elsewhere, winds will remain light to moderate. Into the night, strong winds will return to the northwest, with a risk of coastal gales. Temperatures will be around or slightly above average