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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

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

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

, Bernie D, Bett PE, Bricheno L, Brown S, Calvert D, Clark RT, Eagle KE, Edwards T, Fosser G, Fung F, Gohar L, Good P, Gregory J, Harris GR, Howard T, Kaye N, Kendon EJ, Krijnen J, Maisey P, McDonald RE, McInnes RN, McSweeney CF, Mitchell JFB, Murphy JM, Palmer M, Roberts C, Rostron JW, Sexton DMH

to as InTEM (Inversion Technique for Emission Modelling). ©Crown Copyright 2010 3 1.1 Publications Derwent, R.G., Simmonds, P.G., O’Doherty, S., Grant, A., Yates, E.L., Manning, A.J., Utembe, S.R., Jenkin, M.E., Shallcross, D.E. ‘Seasonal cycles in short-lived hydrocarbons and halocarbons in baseline

. Corazza M, P. Bergamaschi, A. T. Vermeulen, T. Aalto, L. Haszpra, F. Meinhardt, S. O'Doherty, R. Thompson, J. Moncrieff, E. Popa, M. Steinbacher, A. Jordan, E. Dlugokencky, C. Brühl, M. Krol, and F. Dentener, Inverse modelling of European N2O emissions: Assimilating observations from different

in the tropical Pacific Niño3.4 region (120 ◦ –170 ◦ W, 5 ◦ N–5 ◦ S): >0.5 ◦ C, between -0.5 and +0.5 ◦ C, and <-0.5 ◦ C, respectively. Current conditions: Source: OSTIA SSTs in the tropical Pacific Niño3.4 3 NINO3.4 SST anomaly plume Met Office forecast from 1 May 2012 Monthly mean anomalies relative to NCEP

(s) Averaging Freq. Level(s) Leadtimes WAV*hi primary_swell_wave_from_direction instant hourly surface T-48 => T+143 WAV*hi primary_swell_wave_mean_period instant hourly surface T-48 => T+143 WAV*hi primary_swell_wave_significant_height instant hourly surface T-48 => T+143 WAV*hi

situation as it evolves. Which Unitary Authority area(s) a warning applies to At the bottom of the email, there will be a list of Regions and Local Authorities affected by the warning. It is not currently possible to select warnings for just one Unitary Authority. It is only possible to receive all