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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

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

Regional Climate Centres in Africa Consolidated Capacity Needs Assessments Supported by: - 2 - Preamble In the light of the enormous challenges climate variability and climate change pose to societies, there is an urgent need to enable African countries to provide the best possible climate services

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

Hadley Centre, FitzRoy Road, Exeter, Devon EX1 3PB, UK e-mail: [email protected] of the RCMs are often different than the driving GCMs and arguably more credible given the improved performance of the RCM. This also suggests that local climate forcing will be a significant driver

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

dry and sunny throughout the day. Temperatures will be highest in eastern and southeastern England, where values may reach 19-20°C. Elsewhere, particularly in the west and northwest, it will be cooler with highs generally between 15-18°C. Winds will be light for most, though a strengthening breeze

the morning, although some eastern coastal areas and parts of the far north may remain overcast throughout the day. Elsewhere, conditions will be dry with plenty of sunshine. Winds will be light to moderate for most, though they may be locally fresh along eastern coasts. Temperatures will again be warm