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State-of-the-art underwater robots to play crucial role

into vital aspects that form the weather systems that affect us every day.” The NOC has partnered with the Met Office since the 1990’s, developing ocean models that underpin these developments in weather forecasting capability. The success over the last year has led the Met Office to recently

Microsoft Word - Seasonal Assessment_summer2023.docx

, one in July and none at all in August, with the highest summer temperature, a modest 32.2°C, falling far short of 2022’s 40.3°C. This was provisionally the eighth warmest summer for the UK in the series from 1884. Of the UK’s top-ten warmest summers, summer 2023 was the wettest. While the rainfall

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Mixed conditions on the way

The short-lived hot period in the south and east is being replaced by a westerly airflow for the UK, bringing showers and some longer spells of rain for some in the coming days and a return to nearer-average temperatures for the time of year. Which day(s) will be dry this week? Find out

Dispersion processes and parameterizations

. During the 1960's with the advent of computers the Met Office was at the forefront in developing the first simple dispersion computer models. However, it was the Chernobyl incident in 1986 that triggered the start of the development around the world of sophisticated atmospheric dispersion models

Ocean and ice model development

representation of these. Identifying leading order processes which may impact on future predictions of Arctic sea-ice cover. References Bordeau, G., B. Barnier, A-M, Treguier, T. Penduff, S. Gulev (2010), An ERA40-based atmospheric forcing for global ocean circulation models. Ocean Modelling, vol. 31, p88-104. Murray, R. J. (1996), Explicit generation of orthogonal grids for ocean models. Journal of Computational Physics, vol. 126, p251-273.

snow-and-low-temperatures-late-march-2013---met-office.pdf

severe for livestock. s of Air temperature at Lake Vyrnwy, Powys 15 March to 5 April 2013 Historical context The snow and low temperatures were unusual because they occurred so late in the year - in late March - and this was the most significant spell of snow and low temperatures at this time of year

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