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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
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
17/32 W 16/28 W 16/26 W 12/19 W 7/14 SW 9/16 S 16/27 SE Valley 17/36 W 15/32 W 15/31 W 15/27 W 14/26 W 10/19 W 6/13 SW 8/15 S 14/27 SE Height (m) Temperature / Feels Like (°C) 00:00 03:00 06:00 09:00 12:00 15:00 18:00 21:00 00:00 600 8/1 7/2 7/1 8/2 10/6 10/7 9/6 8/4 8/4 300 10/6 10/6 9/6 10/7 13/10
at the local level. Adaptation in practice Lower Otter Valley – Clinton Devon Estates The Lower Otter Valley is heavily modified by human hand. The main modification is an embankment that was built in the early 19th century, canalising the river and disconnecting it from its entire floodplain. Since
21:00 00:00 600 27/38 W 21/30 W 18/25 W 18/25 W 21/31 W 21/31 W 16/24 W 13/20 SW 13/18 SW 300 16/34 W 15/30 W 11/24 W 11/25 W 14/29 W 14/28 W 10/22 W 6/16 SW 7/16 SW Valley 14/31 W 10/25 W 7/19 W 11/23 W 15/29 W 14/28 W 9/20 W 4/14 SW 7/16 S Height (m) Temperature / Feels Like (°C) 00:00 03:00 06
22/30 W 23/30 SW 20/25 SW 30/37 S 600 31/42 W 29/38 W 24/33 W 22/30 W 19/27 W 17/25 W 15/21 SW 14/19 S 21/29 S 300 22/37 W 20/35 W 17/29 W 16/28 W 14/24 W 12/22 W 9/18 SW 8/15 S 13/23 S Valley 23/38 W 21/36 W 18/30 W 17/29 W 14/25 W 12/22 W 10/18 SW 9/16 S 13/24 S Height (m) Temperature / Feels Like
