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and climate consultancy Insights About us Who we are, what we do and organisational news. Who we are Who we are Our people Our values Our history Accuracy Innovation Impact How we are run How we are run The Met Office Board Our governance structure Public Weather Service Our Chief Executive

and climate consultancy Insights About us Who we are, what we do and organisational news. Who we are Who we are Our people Our values Our history Accuracy Innovation Impact How we are run How we are run The Met Office Board Our governance structure Public Weather Service Our Chief Executive

and climate consultancy Insights About us Who we are, what we do and organisational news. Who we are Who we are Our people Our values Our history Accuracy Innovation Impact How we are run How we are run The Met Office Board Our governance structure Public Weather Service Our Chief Executive

Space Weather Mission to L5 Setting the Operational Context Dr. Thomas Berger Director Space Weather Prediction Center National Weather Service What does “Operational” mean? National Weather Service standards - 24/7/365 staffing of forecasting office. - 99+% reliability of observing, processing

% in parts of north-east England. The daily total of 80.7 mm at Morpeth (Cockle Park) on 5th is the highest recorded there in a record that begins in 1897, the previous record being 77.9 mm on 26 October 1900. Rainfall 4-6 September 2008 with return periods and percent of monthly average Weather station

in rainfall and temperature will alter the distribution of some of West Africa’s flora and fauna, with limited opportunity for species to take hold in new geographies because of existing pressure on habitats and ecosystems. • Careful management of forests, national parks and marine protected areas

-moving frontal system maintained cloudy and cool weather on the 6th with isolated showers. The 7th was another showery day but with some sunshine in between, and then rain spread from the south-west during the following night, giving 20.0 mm at Cardiff Bute Park (South Glamorgan). The rain

effect can increase already high background temperatures. Cities generally have less green and blue spaces, compared to more suburban and rural areas, such as parks, forests, ponds and wetlands that act to cool their surroundings. Heat emissions from transport and air conditioning units add excess heat

can increase already high background temperatures. Cities generally have less green and blue spaces, compared to more suburban and rural areas, such as parks, forests, ponds and wetlands that act to cool their surroundings. Heat emissions from transport and air conditioning units add excess heat

increase already high background temperatures. Cities generally have less green and blue spaces, compared to more suburban and rural areas, such as parks, forests, ponds and wetlands that act to cool their surroundings. Heat emissions from transport and air conditioning units add excess heat