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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
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
but valley temperatures struggling to rise above freezing. During the afternoon, a few light snow showers may affect the east of the Park for a time. Some uncertainty in the extent of these with most places likely to avoid them. Any showers soon clear away then a dry and clear evening. Chance
and scattered snow showers through the morning. These showers becoming lighter and more isolated through the afternoon and evening leaving mainly dry conditions with good sunny then clear spells. Feeling bitterly cold even down to valley level. Chance of cloud-free hill tops above 700m: 60% early morning
: Dry and clear to end the night then a sunny morning but valley temperatures struggling to rise above freezing. From late morning and during the afternoon, a few snow showers are expected to spread east. Some uncertainty in the extent of these with northern and eastern fells possibly avoiding them
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
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.
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
(blowing from) 06:00 09:00 12:00 15:00 18:00 21:00 00:00 900 22/26 NW 18/21 NW 16/20 NW 23/29 NW 26/32 NW 24/29 NW 24/30 NW 600 14/18 NW 8/11 NW 10/13 NW 15/21 NW 18/23 W 14/19 NW 13/17 NW 300 8/14 NW 3/7 W 4/8 W 9/17 NW 11/21 W 8/15 NW 7/16 NW Valley 9/14 NW 4/8 W 5/8 W 10/18 NW 12/22 W 9/16 NW 9/18
