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the door for low pressure systems to move in from the Atlantic. This change has already brought wetter conditions, and it’s this new setup that will influence our weather over the coming days. READ MORE: What is the jet stream and how does it affect our weather? Short-Term Outlook: Uncertainty

a number of brief hot spells, particularly in the south and east, followed by a return to cooler, wetter weather. The hottest day of the year so far occurred on 1 July, marking the peak of the most recent warm phase. Current conditions and short-term outlook As we move into early July, high pressure has

the storm. For more details see ESA - Arctic Weather Satellite’s first images capture Storm Boris. Credits:  Image: ESA August 2024 - Thunderstorms during Paris Olympics 1 August 2024 The Paris Olympics in late July to August 2024 began with wet and unsettled weather, featuring heavy rain

and eastern England being rather wet. For example, Kent saw 185% of its average rainfall while West Lothian saw just 59%. At least one weather station in Kent (East Malling) reported more than twice its normal rainfall. Storm Noa on 12 April 2023 was the second named storm of the 2022/2023 storm

unpredictable for a while now, the traditional seasons have changed, the wet season that was expected between February and March is no longer consistent. Livestock has been affected, with huge losses reported from the surrounding Kraals too. The animals do not fetch good prices at the market because

results, referred to as the “new” projections. The maps presented here cover all four seasons, whereas those in Harris et al (2022) were mainly restricted to winter and summer. Here, we show projected changes for the RCP4.5 scenario during 2040-2059 as well as covering RCP8.5 responses for 2070-2089

: Wet and windy into Autumn Author: Press Office 28 August 2025 As summer comes to an end, the UK is already experiencing a distinctly autumnal feel. The latest Met Office 10-Day Trend points to a period dominated by unsettled conditions, with low pressure systems bringing spells of rain, showers

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

to be much wetter over the lake (biases as large as 8 mm/day with respect to CPC- FEWS). The discrepancy between the amount of rain in the model and in observations is particularly pronounced in the late rainfall season (SON), but the bias is also present in the off-peak seasons. The bias is present

. This can ‘block’ the Atlantic low-pressure systems which are responsible for the relatively mild, wet and windy weather that often occurs in UK winters. This blocking pattern increases the chance of cold, dry weather in the UK and mild, wet and windy conditions for southern Europe. However, the impacts