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midlands_-climate-met-office.pdf

Midlands: climate The Midlands area includes the Cotswold Hills to the south, the Northamptonshire uplands to the east, the Peak District to the north and is bounded by the Welsh border to the west. It includes the Severn and Avon valleys, with their rivers flowing to the south, and the valley

peak_district.pdf

cloudy (night) Partly cloudy (night) Light rain Light rain showers Heavy rain showers Heavy rain showers Cloudy Partly cloudy (night) Precipitation probability 10% 10% 30% 30% 60% 60% 30% 10% Forecast for Tuesday 21 Oct 2025 2025-10-21 Weather: Clear spells and some valley fog in the early hours

lake_district.pdf

cloudy (night) Partly cloudy (night) Heavy rain showers (night) Heavy rain showers Heavy rain showers Heavy rain showers Cloudy Precipitation probability 10% 10% 40% 70% 70% 40% 20% 10% Forecast for Tuesday 21 Oct 2025 2025-10-21 Partly cloudy (night) Weather: Clear spells and some valley fog

wales_-climate-met-office.pdf

there is little wind, skies are clear, and there is a covering of snow; the lowest temperatures occur away from the moderating influence of the sea, on the floors of inland valleys into which cold air can drain. It was under such conditions that the temperature fell to -23.3 °C, the lowest ever

PowerPoint Presentation

service for Yangtze river valley Climate prediction service for Pacific Typhoon risk Research on engagement and uncertainty Prototype Climate Services Climate prediction service for Yangtze river valley Climate prediction service for Pacific Typhoon risk Research on engagement and uncertainty

mourne_mountains.pdf

80% in afternoon. Low cloud and visibility: Patchy fog in the valleys and on the summits overnight. Cloud will become extensive during the morning with bases 400 to 600m, then lifting and breaking through the afternoon. Away from cloud, mainly good visibility, occasionally poor in showers. Check our

Mist, fog, and haze: What's the difference?

ability to hold moisture decreases, leading to condensation and fog. Radiation fog typically dissipates soon after sunrise as the ground warms, except in high elevation areas where the sun has little influence . Valley fog: Valley fog forms when cold, dense air settles into the lower parts of a valley

Dr Bernard Claxton

at Bridlington, valley flow in South Wales, the Pennines and the Clun Valley, fog in southwest France and surface moisture exchange in northern Spain. Bernard is both a Chartered Physicist and Member of the Institute of Physics, and a Fellow of the Royal Meteorological Society.

yorkshire_dales.pdf

/10 E 4/8 NE 4/6 NW 3/9 W Valley 5/11 E 6/13 E 7/13 E 6/9 E 3/6 NE 1/3 NE 1/4 W Height (m) Temperature / Feels Like (°C) 06:00 09:00 12:00 15:00 18:00 21:00 00:00 600 8/6 8/6 9/6 9/7 9/8 8/8 8/7 300 9/8 11/10 11/10 12/11 10/10 10/10 9/8 Valley 10/9 12/11 13/12 13/12 12/11 11/11 9/9 Freezing Level

PowerPoint Presentation

to the maritime influence. Showers – In spring and summer heavy showers developing further southwest along the Lagan Valley can give Belfast frequent heavy downpours or thunderstorms. Belfast sits at the eastern end of the Lagan Valley surrounded by high ground to the north and south. Winter time inversions

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