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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

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

lake_district.pdf

conditions by early evening, but further rain expected overnight. Chance of cloud-free hill tops above 800m: 10%, best chance across the northern Fells early morning. Low cloud and visibility: Poor visibility is likely throughout the day with persistent cloud often down to the valleys, but around 600m

snowdonia.pdf

likely to be persistent above 400-500m, soon lowering towards the valleys, although cloud bases a few hundred metres higher in the northeast. Check our weather forecast every day to get the most accurate and up to date information https://www.metoffice.gov.uk/weather/specialist-forecasts/mountain

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.

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

yorkshire_dales.pdf

(mph) Wind Direction (blowing from) 06:00 09:00 12:00 15:00 18:00 21:00 00:00 600 15/21 S 19/27 S 18/25 S 16/24 S 16/23 S 14/20 S 17/24 S 300 6/16 S 8/19 S 11/24 S 10/21 S 9/19 S 8/18 S 10/22 S Valley 6/19 S 9/23 S 10/23 S 9/21 S 6/17 S 5/15 S 9/22 SE Height (m) Temperature / Feels Like (°C) 06:00

brecon_beacons.pdf

/30 S 22/28 S 23/31 S 19/25 S 18/24 S 300 12/27 S 12/26 S 13/27 S 13/26 S 13/27 S 8/18 S 9/20 S Valley 6/20 S 11/26 S 10/25 S 11/26 S 10/23 S 5/16 S 5/16 S Height (m) Temperature / Feels Like (°C) 06:00 09:00 12:00 15:00 18:00 21:00 00:00 600 8/3 8/4 9/5 9/5 10/6 9/6 8/5 300 10/7 10/8 11/9 11/9 11/9

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