M1 J41 Carrgate Interchange

For this output data, temperature is shown for 2 m above ground. The calculations take into account the terrain (elevation), but with lower resolution than in reality. Therefore the models cannot differentiate, for instance, the temperature on a mountain peak or on a city square scorched by the sun. The general rule is that the centres of large cities are 1 °C to 3 °C warmer than the surrounding area or natural landscapes. Significant temperature differences over a small area are primarily caused in the winter by an inversion. A short yet noticeable cooling can also occur after a local summer storm.

WebcamsWeather fronts

Share Settings Premium myVentusky About

Glasgow0 °CAberdeen London Dublin Birmingham Newcastle upon Tyne Cork Southampton Plymouth Belfast Bristol Liverpool Zaragoza Burgos A Coruña Porto Nantes Gijón Bordeaux Brest Vigo Bilbao Oslo Bergen Århus Stavanger Aalborg Hamburg Bruxelles - Brussel Köln Amsterdam Frankfurt am Main Bremen Hannover Reims Kassel Le Havre Groningen Norwich Nürnberg Paris Barcelona Milano Marseille Torino Stuttgart Genova Genève Montpellier Verona Perpignan Orléans Dijon Limoges Clermont-Ferrand Toulouse Nice Zürich Lyon Stockholm Göteborg Turku Berlin Warszawa Praha København Łódź Kraków Wrocław Poznań Leipzig Klaipėda Olsztyn Koszalin Rzeszów Калининград (Kaliningrad)Gdańsk Bydgoszcz Szczecin Dresden Brno Roma Budapest Wien Београд (Belgrade)München Zagreb Sarajevo Prishtina Oradea Linz Split Bari Ljubljana Venezia Graz Banja Luka Košice Pescara Rimini Salzburg Pécs Podgorica Timişoara Tirana M1 J41 Carrgate Interchange L H

°C5040302520151050−5−10−15−20−30−40

Ventusky: Weather Forecast Maps

Yesterday & Today

Nearest webcams