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Experiments 4.3.2.1 Model validation 7 Before using RCM models to investigate the future climate scenario, it is necessary to evaluate how well models represent the present climate. There are different options to validate the appropriateness of a model (s) to simulate local climate. In this research two

in inland Devon. On 8/9 January 1982 conditions were especially severe in the Bristol area where dri s were locally 1 m deep. Another event, this time from convective showers, on 12 January 1987 produced snow depths of 35 cm (Falmouth), 39 cm (Penzance) and even 23 cm on the Scillies. Also, persistent

and predicted for 2023 relative to the preceding year, vs. the Niño3.4 index for April of the preceding year to March of the current year. The Niño3.4 index is the sea surface temperature (SST) anomaly in region 5°N to 5°S and 170°W to 120°W in the Pacific Ocean, de-trended to remove the effect

Ocean (Figure 3). Figure 3. Annual CO2 growth rate for years 1960 to 2023 and predicted for 2024 relative to the preceding year, vs. the Niño3.4 index for April of the preceding year to March of the current year. The Niño3.4 index is the sea surface temperature (SST) anomaly in region 5°N to 5°S

Workshop takes place, but s a result of COVID-19 restrictions, these were moved to virtual events since March 2020. Using Microsoft Teams, the UM Users virtual workshop consisted of live plenary sessions and breakouts groups spread over four half days covering key areas of the UM Partnership, namely

, coproduced and accessible weather and climate services to inform regional, national, sub-national and community level policy, planning and decisionmaking in Africa 12 plans and policies where weather and climate information is better used 875,000 HH using new or improved climate services s 22