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hctn_sept2023rapidhadgemstudy_v1.1.pdf

://doi.org/10.1007/s00382-022- 06403-0 Hollis, D, McCarthy, MP, Kendon, M, Legg, T, Simpson, I. HadUK-Grid—A new UK dataset of gridded climate observations. Geosci Data J. 2019; 6: 151– 159. https://doi.org/10.1002/gdj3.78 Kendon, M., McCarthy, M., Jevrejeva, S., Matthews, A., Williams, J., Sparks, T

DePreSys: Met Office decadal prediction system

the decade. Updated decadal forecasts, along with verification of previous forecasts, are available from the Forecast web page. References Smith, D. M., S. Cusack, A. W. Colman, C. K. Folland, G. R. Harris and J. M. Murphy, 2007, Improved surface temperature prediction for the coming decade from

Radar systems

network was built up over a period from the mid 1970's to the 1990s, with the oldest radar at Hameldon Hill. To combat the risk of obsolescence, meet the future demands of higher resolution NWP, and operationally realise the benefits of dual polarisation technology on the UK network, the radar

Disc Log 185

an entirely separate building. A professional market rental valuation of the space has not been undertaken and is not required. The Union Office is included within the overall Business Rates assessment for Met Office HQ. Information concerning Business Rates is publically available via www.voa.gov.uk. 2. Cost estimated as standard office overheads for 0.75 fte staff member plus travel for staff case visits & H&S related meetings (less than £1k per annum).

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of the supplier(s)? Information released: The Met Office’s Annual Report 2012-13 (page 14) shows the electricity consumption for the HQ site. Please see the following link to the 2012-13 annual report: http://www.metoffice.gov.uk/learning/library/publications/corporate The Met Office uses EDF Energy

Dr Susan Leadbetter

Areas of expertise Dispersion for emergency response applications Radiological dispersion modelling My Publications - Leadbetter, S Current activities The main focus of Susan's work is on the application of the Met Office's Met Office Dispersion Model (NAME) to the accidental release of pollutants

ukcp18-how-to-choose-the-most-appropriate-projection.pdf

How to choose the most appropriate land projection New to climate projections? Looking for headline messages? Carrying out detailed analysis? See What do you want to do? on UKCP18 website See Key results on UKCP18 website Select strand(s) of land projections based on task Task Probabilistic Global

Weather Radar Data Quality Monitoring using Operational Observations

– Fit Functions • Fit function for correlation coefficient ρ HV takes the form: with x = 1 - ρ HV . • Fit function of differential phase Φ DP takes the form: f x = a ⋅ s ⋅ x μ ⋅ e −λ with x = Φ DP - max Φ DP + 10° , where max Φ DP denotes distribution’s maximum, a is an amplitude factor, s a stretch

srocc_sea_level_rise.pdf

in the projected loss of ice from the Antarctic ice sheet (Figure 2a). These revised projections show good agreement with independent work carried out at the Met Office for UKCP18 5 . 1 Daangendorf, S. et al (2019), Nature Climate Change: Persistent acceleration in global sea-level rise since

observed_changes_in_extremes_final_v1.0.pdf

saw extremely high levels of tropical cyclone activity in the Western North Pacific. This was found to be mainly caused by sea surface warming in the eastern and central Pacific, with human influence largely increasing the odds of this event. Zhang et al 2016 Funk, C., Shukla, S., Hoell, A. and Livneh

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