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science programmes and other activities, provides the best possible services and advice to customers. To foster productive links with the global meteorological and climate community. In this video, hear from Professor Gideon Henderson, Professor of Earth Sciences at the University of Oxford and chair
in the UK to understand how information provided in the UK’s high-end (H++) sea-level rise scenario can be improved. She also has experience modelling carbon dioxide removal through ocean alkalinity enhancement and holds a Masters degree in Earth Sciences from the University of Oxford.
Team on Operational Weather Forecast Systems under the new INFCOM Commission. Before this, Ken joined the Met Office in 1984 with a degree in Physics from Oxford University. His first seven years were spent conducting experimental research on the dispersion of pollution in the turbulent boundary
-02 290 28 KT -02 6000ft 290 28 KT -09 290 28 KT -09 290 28 KT -08 Height (above ground level) / time (UTC) Oxford 1500 1800 2100 1000ft 280 22 KT +04 270 22 KT +03 260 24 KT +03 3000ft 280 22 KT -02 280 25 KT -03 280 28 KT -03 6000ft 290 23 KT -10 290 25 KT -10 280 26 KT -09 Height (above ground
(Grantham Institute, Imperial & University of Reading) and its membership is: • Professor Mat Collins (University of Exeter); • Professor Jim Hall (University of Oxford); • Dr Ed Hawkins (University of Reading); • Professor Gabi Hegerl (University of Edinburgh); • Dr Erik Kjellström (Rossby Centre
and the flooded towns included Evesham, Leamington Spa, Stratford-on-Avon, Bedford, Northampton and Huntingdon. Impacts In the river systems draining the 5,000 km area bounded by Bedford in the east, Evesham in the west, Peterborough in the north and Oxford in the south, the flood levels were
including dynamics, numerical methods and data assimilation. He was a main organiser along with John Ball and Sergei Kuksin of an EPSRC-funded workshop on the Mathematics of weather and climate prediction held at the Met Office in Spring 2009, in collaboration with the Oxford Centre for Nonlinear PDEs
and the Environment, University of Oxford, UK Dry-to-wet transition Two-tier approach: (1) climatologial envelope when the transition should occur (2) dry-to-wet transition in each year/season (1) Gradient (x100) Filtered precipitation Filtered Precipitation (60-points second order Butterworth filter
Contingencies Director. • Chief Scientist, Julia Slingo, noted the research on Solar Variability and the imminent publication of the paper, produced in collaboration with Reading and Oxford University. • JH talked about a good visit from Andrew Haldane, Bank Of England, including his appreciation
to the very wet weather. Over the course of a season, even influences from the other side of the globe can change the weather experienced in the UK. New study published Today, in a study published in the journal Environmental Research Letters, a team of Met Office and University of Oxford scientists
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