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in the recitals. SADIS API Licence Agreement Page 2 of 10 Issue:21/11/2023 “Your Application” “Your Data” “Your Users” means any software application(s), site(s) or other interface that You create, develop, own or operate to interact with the API or read, update or delete certain content from Your Users

in wind speeds is modest compared to interannual variability for the PPE-15. • no trend in the wind speed over the UK for the mean of the CMIP5-13. Wind speed anomaly, m s ¡1 3 2 1 0 −1 −2 −3 DJF PPE-15 CMIP5-13 (subset) 1900 1925 1950 1975 2000 2025 2050 2075 2100 Date Figure 1 Global projections

evidenced manner; or  · the response addresses all elements of the Requirement very well and includes innovative and/or other good quality ideas that meet the Met Office ‘s Requirements and provides good evidence of where such ideas have been used effectively in the past and why they will work well

and comprehensively evidenced manner; or  · the response addresses all elements of the Requirement very well and includes innovative and/or other good quality ideas that meet the Met Office ‘s Requirements and provides good evidence of where such ideas have been used effectively in the past and why

a scale-dependent dynamic Smagorinsky model at near-grey-zone resolutions, Journal of Applied Meteorology and Climatology, volume 57, pages 2197-2214, DOI:10.1175/JAMC-D-17-0318.1. [PDF]  Gu J.F., R. S. Plant, C. E. Holloway, T. R. Jones, A. Stirling, P. A. Clark, S. J. Woolnough, and T. L. Webb

precipitation being considered as a liquid water equivalent (lwe) value. It includes the contribution from the model convection scheme if this is invoked (true for Global models but not the UK models) as well as that from the model precipitation scheme. m s-1 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm] M

and flows in the tachocline will be resolved in longitude for the first time. • The resolution will be about 0.1 R s , resolving azimuthal variations up to about wavenumber m=30. Earth L 5 L5 Workshop R. A. Howard (NRL) The processes and sources of the solar wind remain ambiguous • Status: – To constrain

in the appropriate box in the matrix: R = River S = Surface Water G = Groundwater C = Coastal/ Tidal Fig 5: Flood risk matrix displayed on selection of a local authority Fig 6: Mobile view of flood risk matrix on selection of a local authority 4 When a local authority coloured green is selected, you

placed in the appropriate box in the matrix: R = River S = Surface Water G = Groundwater C = Coastal/ Tidal Fig 5: Flood risk matrix displayed on selection of a local authority Fig 6: Mobile view of flood risk matrix on selection of a local authority 4 When a local authority coloured green is selected

east of 160°E and north of 25°S) Other tropical cyclone warning centres Australian Bureau of Meteorology (seas around Australia, longitude 90-160°E) MetService, Wellington, New Zealand (South Pacific Ocean east of 160°E and south of 25°S) Joint Typhoon Warning Center, Pearl Harbor, Hawaii (all oceans