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compared to a baseline period of 1961-1990. We can see that temperatures have risen in all areas across the UK. We can also see that whilst some areas have become drier, more areas have become wetter. IMPACTS Cities and towns across the UK are already experiencing the impacts of climate change

areas have become drier, more areas have become wetter. IMPACTS Cities and towns across the UK are already experiencing the impacts of climate change. The negative impacts of climate change for urban areas may include: HEAT Increased energy demand for summer cooling SEA LEVEL RISE Increased risk

see that temperatures have risen in all areas across the UK. We can also see that whilst some areas have become drier, more areas have become wetter. IMPACTS Cities and towns across the UK are already experiencing the impacts of climate change. The negative impacts of climate change for urban areas

) and rainfall (right) from 1991-2020 compared to a baseline period of 1961-1990. We can see that temperatures have risen in all areas across the UK. We can also see that whilst some areas have become drier, more areas have become wetter. IMPACTS Cities and towns across the UK are already experiencing

in all areas across the UK. We can also see that whilst some areas have become drier, more areas have become wetter. IMPACTS Cities and towns across the UK are already experiencing the impacts of climate change. The negative impacts of climate change for urban areas may include: HEAT Increased energy

of the wet season in semiarid tropical climates of western Africa. Int J Climatol 21:1251– 1262 Sijikumar S, Roucou P, Fontaine B (2006) Monsoon onset over Sudan- Sahel: simulation by the regional scale model MM5. Geophys Res Lett 33: L03814. doi:10.1029/2005GL024819 Sivakumar MVK (1988) Predicting

Assessing the use and benefits of weather and climate information services in Pakistan Final report for the Asia Resilience to a changing climate programme August 2022 3 Authors University of Leeds Marta Bruno Soares Linas Svolkinas Hellen Msemo Natalie Suckall ICIMOD Mandira Shrestha Mani Nepal

. There was plenty of settled weather, with only limited amounts of rainfall, especially in the south. Only during the last week of the month was the weather truly unsettled, a period which included the first named storm of the season. The mean temperature was provisionally 0.5 °C above the 1981-2010 long-term

in percentages. The outlook uses 3 categories, linked to previous observed UK conditions, for possible UK temperature, precipitation and wind speed in the coming season: COLD, NEAR AVERAGE and MILD for temperature WET, NEAR AVERAGE and DRY for precipitation CALM, NEAR AVERAGE and WINDY for wind speed

in these seasons. In summer, convection caused by solar surface heating sometimes forms shower clouds and a large proportion of rain falls from showers and thunderstorms then. The additional heat from the London urban area can encourage such shower development in summer. A further factor that greatly affects