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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
-23 Weather: Dry with clear spells overnight, perhaps some mist or freezing fog in the valleys by dawn. Any mist or freezing fog clearing during the morning and staying dry and bright for much of the day, although some high level cloud at times. Some patchy light rain possible by evening. Chance
) intervals intervals intervals Precipitation probability 00% 00% 00% 00% 00% 00% <05% 20% Forecast for Monday 23 Mar 2026 2026-03-23 Weather: Dry with clear spells overnight, perhaps some mist or freezing fog in the valleys by dawn. Any mist or freezing fog clearing during the morning and staying dry
) intervals Precipitation probability 00% 00% 00% 00% 00% <05% 20% 30% Forecast for Monday 23 Mar 2026 2026-03-23 Weather: Dry with clear spells overnight, perhaps some mist or freezing fog in the valleys by dawn. Any mist or freezing fog clearing during the morning and staying dry and bright
) (night) intervals intervals Precipitation probability <05% 00% 00% 00% 00% <05% 20% 20% Forecast for Monday 23 Mar 2026 2026-03-23 Weather: Dry with clear spells overnight, perhaps some mist or freezing fog in the valleys by dawn. Any mist or freezing fog clearing during the morning and staying dry
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
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of the day, although some high level cloud at times. Some patchy light rain possible by evening. Chance of cloud-free hill tops above 600m: 90% or more Low Cloud and visibility: Generally no significant low cloud. Visibility mostly very good or excellent, except in any early valley mist and fog
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
