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Storm Ewan was named by Met Éireann, the Irish Met service, as the fifth named storm of the season on Saturday night. Storm Ewan brought strong winds to southern areas of Ireland on Sunday 26 February

and hill snow in some areas. Chief Meteorologist Andy Page said: “Polar Maritime air is becoming established across the UK with colder conditions expected for the next few days, but nothing unusual for late winter. The week will be characterised by wet and windy spells across the southern half of the UK

the SSP5-RCP8.5 scenario (Gutiérrez et al., 2021; Figure 2). In general, decreases in precipitation and increases in temperature and evaporation are expected to intensify drought severity and duration over the region. Wet season rain storms are also projected to become more intense, as a warmer

for understanding climate variability in East Asia on timescales of seasons to decades and to assist in collaborative attribution studies of extreme events. Model development is at the core of CSSP China. Longer-term goals include joint development of high-resolution models for the East Asian

) was the second storm of the 2017-2018 winter season, following Storm Aileen on 12 to 13 September. The strongest winds were around Irish Sea coasts, particularly west Wales, with gusts of 60 to 70 Kt or higher in exposed coastal locations. Impacts The most severe impacts were across the Republic of Ireland

regions being cooler and wetter and the northern areas being hotter and drier as they get closer to the Sahel. Observations from 1981-2010 show a moderate increasing trend in temperature compared to other regions of the world, but as the region has a narrow climatic temperature range both interannually

All tropical cyclones in the northern hemisphere season in 2014 are listed below including details of their start and end dates and maximum sustained wind (MSW). Qualitative comments are included on the performance of the Met Offi

Click on the name of the tropical cyclone to see a chart of the observed track and forecast tracks from the Met Office global model. Verification statistics on each tropical cyclone are available upon request from [email protected]. At the end of the season a verification report on the performance

to less frequent, more extreme rainfall and therefore the seasonal mean may decrease while daily extreme values may stay similar to the baseline or increase. • See UKCP Probabilistic Extremes report and factsheet for more details. • Widespread wet bias in Europe and UK region in winter. Biases vary

, but with the north and east generally brighter relative to average than the south and west. Rainfall was very close to average overall, but with regional variations, most parts of Scotland being drier than average, but southern and eastern England being rather wet. For example, Kent saw 185% of its average

The Great British weather presents different challenges in different seasons. It's not just winter weather which can wreak havoc on the roads - even rain at any time of the year can be dangerous - in fact 9 out of 10 weather-related deaths and serious injuries on the roads take place in the rain

is not sufficient to assess model projections. Direct investigation of the mechanisms for future precipitation change is also important, and existing efforts in this area have generated valuable hypothesis about the potential drivers of wet and dry responses [e.g., Biasutti et al., 2008, 2009; Monerie et al