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to the west of the UK, a light southerly flow draws hot air from the near continent northward across the UK. Satellite image from NASA Terra satellite at 1053 GMT 1 July 2015. The area of cloud across south-east England dri ed north during the day; had this not been present temperatures may have climbed

Ireland.  "Even though the process of selecting the names was a fun and light-hearted task, ultimately, advising the public of the importance of being prepared for the upcoming storm season, and communicating safety messages for every forecast storm are our highest priorities. At the start

information. A good example was Storm Éowyn last January, when our website, met.ie received more than 3 million visits in 2 days. This all aids in protecting life and property across Ireland. Even though the process of selecting the names was a fun and light-hearted task, ultimately, advising the public

of providing a value in the 0 to 1 (or 0 to 100% range) the data is categorized into to icing intensities. A comparison of the old Icing Potential and new Icing Severity fields is shown below: WAFS Icing Potential, FL240 WAFS Icing Severity, FL240 WAW trace light moderate severe It can be seen that the new

settled conditions across much of the UK, with most areas enjoying dry weather and sunny spells. Temperatures will be close to the seasonal average, though it will feel pleasantly warm in the sunshine, especially where winds remain light. Eastern and southeastern England may see more in the way of cloud

Thursday will begin with residual showers and isolated thunderstorms lingering across the southeast, gradually clearing through the morning. Western areas will see scattered, mainly light showers developing later in the day. Across central and eastern Scotland, and possibly far northeast England

Thursday will begin with residual showers and isolated thunderstorms lingering across the southeast, gradually clearing through the morning. Western areas will see scattered, mainly light showers developing later in the day. Across central and eastern Scotland, and possibly far northeast England

. Radio waves emitted from a radar antenna travelled outwards at the speed of light, only bouncing back to the same antenna when they encountered an object. When the weather was clear, radar could quickly provide intelligence on the position of aircraft in the sky. When it was raining or snowing, echoes

in the atmosphere, typically between 80 and 300 kilometres above the Earth’s surface. To see them, clear, dark skies are essential. Even thin cloud can obscure the subtle colours and movements of the aurora, while thick cloud makes sightings impossible. Light pollution from urban areas further reduces

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