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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

and WP-MIP Machine Learning Emulation of Climate Change Projections for Southeast Asia 12:00 Discussion groups 13:00 Group photo 13:05 Lunch + Poster Session 2&3 14:00 Plenary debrief Ron McTaggart- Cowan Chen Chen ECCC CCRS Session 2b: AI/ML models and integration with seamless physical model

and WP-MIP Machine Learning Emulation of Climate Change Projections for Southeast Asia 12:00 Discussion groups 13:00 Group photo 13:05 Lunch + Poster Session 2&3 14:00 Plenary debrief Ron McTaggart- Cowan Chen Chen ECCC CCRS Session 2b: AI/ML models and integration with seamless physical model

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

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

: 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

. 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

in the south Asian summer monsoon and in parts of the extratropical North Atlantic Ocean, with wet biases over the Indonesian warm pool. In the Indian ocean sector, wet biases occur off the coast of Madagascar in DJF (in the region associated with the southern lobe of the Indian Ocean dipole (Behera

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