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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
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
cloud and visibility: Patchy cloud and fog above 500 or 600m overnight and during the morning but good visibility at times below the cloud. Visibility becoming generally poor as cloud and fog become extensive above 300m in the afternoon with patches down to valley level. Check our weather forecast
or 600m overnight and during the morning but good visibility at times below the cloud. Visibility becoming generally poor as cloud and fog become extensive above 300m in the afternoon with patches down to valley level. Check our weather forecast every day to get the most accurate and up to date
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
overnight and during the morning but good visibility at times below the cloud. Visibility becoming generally poor as cloud and fog become extensive above 300 or 400m during the afternoon with patches down to valley level in the west. Check our weather forecast every day to get the most accurate
22/30 SW 29/40 SW 30/43 SW 28/40 SW 300 19/29 SW 14/23 SW 16/22 SW 17/25 SW 16/24 SW 16/25 SW 21/32 SW 22/35 SW 21/32 SW Valley 11/26 W 9/22 W 9/22 SW 10/22 SW 11/22 SW 9/22 SW 13/29 SW 14/30 SW 14/29 SW Height (m) Temperature / Feels Like (°C) 00:00 03:00 06:00 09:00 12:00 15:00 18:00 21:00 00:00
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, condensing
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
500 or 600m overnight and during the morning but good visibility at times below the cloud. Visibility becoming generally poor as cloud and fog become extensive above 300 or 400m in the afternoon with patches down to valley level in the west. Check our weather forecast every day to get the most
