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years, however (Fung et al., 2018). Projected changes in future rainfall vary depending on which season you are looking at, with summers likely to become significantly drier while winters become wetter, along with an increase in the frequency and intensity of extreme temperature and rainfall events

: “The Easter period will bring a variety of Spring weather from sunshine and showers, to more prolonged cloudy and wet conditions, along with some snow in the north: chiefly over the hills. So, there will be opportunities to get outside and enjoy the weekend, and you can use the rainfall radar

on from a largely wet June, northern England and the Midlands have now received more than the season’s usual rainfall, with August still to go. Tim Legg, of the Met Office’s National Climate Information Centre, said: “With an all-time temperature record it would be easy to assume that this summer

that falls 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. A further factor that greatly affects the rainfall distribution is altitude. Moist air that is forced to ascend hills

to be drier and cooler seasons wetter. This also means that any correlations found between crop yields and either of these variables are not mutually exclusive, and so multivariate correlation will be explored in Section 3.5. Figure 4: Scatter plot of WFDEI JAS season total precipitation against

distribution to air frost. However, those places into which cold air can drain are particularly prone to frost. Examples include Altnaharra (Highland) with an average of 73 air frosts per year. In Northern Scotland the frost-free season is o en as little as 3 months, as shown by the average

All four seasons have fallen in the top ten in a series which began in 1884 and the 10 warmest years have all occurred since 2003.   As well as setting a new 139-year annual mean temperature record, 2022 will also be remembered for several other significant weather events.  Exceptionally warm start

1, is produced by combining output from the Met Office GloSea5 dynamical forecast system with statistical predictions based on pre-season sea surface temperatures (SSTs) in the tropical Atlantic and Pacific. The methodology is described in Part 2. The GloSea5 contribution to this forecast for FMAM

Powering up the forecasts East Africa has distinct wet and dry seasons, and accurately predicting the onset of its rains is vital for farms and businesses. Yet hydropower is equally reliant on accurate and timely forecasts – as an important climate partnership project recently demonstrated

Powering up the forecasts East Africa has distinct wet and dry seasons, and accurately predicting the onset of its rains is vital for farms and businesses. Yet hydropower is equally reliant on accurate and timely forecasts – as an important climate partnership project recently demonstrated