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0.1º Start dump UM 0.1º 0.1º Output Recon 0.0198º 0.0198º Start dump UM 0.0198º 0.198º Output 11 SEAMLESS GLOBAL MODELLING WORKSHOP JUNE 2025| HIGH-RESOLUTION ACCESS REGIONAL NESTING SUITE FOR RESEARCH PURPOSES We suggested a nest configuration similar to this one Domain NX NY δx (°) δt BC (min) δt(s
& 12 UTC runs are extended at a 3-hourly interval to T+120 Model run times 00 UTC, 06 UTC, 12 UTC & 18 UTC Resolution 0.087° N/S by 0.058° E/W (~6km) Format GRIB2 Domain Latitude: 65.8°N to 30.2°N, Longitude: 19.6°W to 41.7°E Delivery File transfer protocol (FTP) Met Office FitzRoy Road, Exeter
Weather warriors | Weather and climate stories Activity steps 04 Invite each group to present their action plans – this can be done in a variety of formats including a slide show, written report or role play. To add a competitive element, ask teams to vote for their favourite presentations. The group(s
and Use: • Collections will be moved safely and with reference to any potential H&S issues that may impact staff. • Risk assessments will be undertaken before moving particularly vulnerable collections. • All items to be transported will be suitably packaged. • Items will be handled under appropriate
from the tropical Pacific. Nature Geoscience, 12, 351–354, doi:10.1038/s41561-019-0333-7. Lindzen, R., and S. Nigam, 1987: On the role of sea surface temperature gradients in forcing low-level winds and convergence in the tropics. Journal of the Atmospheric Sciences, 44, 2418-2436, doi:10.1175/1520
). This gives a 20-50 year temporary resilience. (Fig 4) (13) The temporary resilience period would be lower if freshwater was added at a higher rate. The AMOC strength when adding freshwater of 0.3 Sv (1 Sv=10 6 m 3 /s) to the North Atlantic (grey), and when freshwater ceases to be added after 20
our accounts we will not automatically Follow you back, Like your page(s), add you as a Friend, or join your account. This is to discourage the use of direct messaging, avoid wasting resources on spam handling and so that you can easily identify other key partners that we think are relevant and who
, Lamarque J-F, Meinshausen M, Smith S, Grainer C, Rose S, Hibbard KA, Nakicenovic N, Krey V, Kram T. 2011: Representative concentration pathways: An overview. Climatic Change. doi:10.1007/s10584-011-0148-z Wanders, N., Van Lanen, H. A. J., and van Loon, A. F. (2010) Indicators for drought
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