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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

no significant low cloud. Visibility mostly very good or excellent, except in any early valley mist and fog. 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 © Crown Copyright 2026. All Rights Reserved

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

snowdonia.pdf

hill tops above 800m: 90%, falling 40% in the evening. Low Cloud and visibility: Generally no significant low cloud, but cloud could develop around the summits during the evening. Visibility mostly very good or excellent, except in valley mist and fog, and summit cloud later. Check our weather

yorkshire_dales.pdf

% 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. Check our weather forecast every day to get the most accurate and up to date information https://www.metoffice.gov.uk/weather/specialist-forecasts

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

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

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

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

mourne_mountains.pdf

03:00 06:00 09:00 12:00 15:00 18:00 21:00 00:00 600 39/54 SW 40/55 SW 34/46 SW 27/36 W 27/37 W 29/40 W 31/42 W 37/51 W 38/53 NW 300 21/36 SW 22/38 SW 18/31 SW 15/25 W 16/27 W 18/29 W 18/30 W 22/36 W 23/38 NW Valley 17/35 SW 17/36 SW 14/29 SW 12/23 W 13/25 W 14/27 W 15/29 W 17/34 W 19/35 NW Height

brecon_beacons.pdf

(mph) Wind Direction (blowing from) 00:00 03:00 06:00 09:00 12:00 15:00 18:00 21:00 00:00 600 20/28 SW 21/30 SW 22/32 SW 24/35 SW 28/41 SW 29/44 SW 29/43 SW 27/41 W 25/38 W 300 13/26 SW 15/29 SW 16/29 SW 18/33 SW 20/38 SW 22/40 SW 20/38 SW 19/36 W 19/34 W Valley 10/22 SW 12/25 SW 13/26 SW 16/32 SW 18

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