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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

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

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

Consortium in Kenya’. Working draft, Exeter: Met Office. 2 Carter, S., Steynor, A., Vincent, K., Visman, E., and Waagsaether, K. (2019) ‘Co-production of African weather and climate services’. Manual, Cape Town: Future Climate for Africa and Weather and Climate Information Services for Africa (https

3 /s) to the North Atlantic (grey), and when freshwater ceases to be added after 20 (green) or 50 (red) years, showing two different final states. b) Temporary resilience as a function of the amount of additional freshwater. 13 How likely is such a threshold to be crossed? It is likely, based

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) receiving the most votes can then present

). 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

Climates. Available at: https://doi.org/10.1017/9781139016476 & Bohnenstengel, S. et al (2014) Available at: https://doi.org/10.1002/qj.2144 Page 1 of 9 HOW IS TEMPERATURE CHANGING ACROSS THE UK? CURRENT TRENDS * FUTURE TRENDS ** ANNUAL AVERAGE TEMPERATURE Since the 1961-1990 period annual average

Wales Midlands Hawarden Airport, Flintshire Pitsford, Northamptonshire 37.1 40.2 East Anglia Cambridge, NIAB 39.9 England SW Bude, Corwall 36.0 S Wales England SE & Central S Gogerddan, Ceredigion Heathrow and St James’s Park, London 35.8 40.2 19 July 2022 18 July 2022 19 July 2022 19 July 2022 18 July

and inclusive co-production for weather and climate services’. Exeter: Met Office. 5. Arrighi, J., Koelle, B., Besa, M.C., Spires, M., Kavonic, J., Scott, D., Kadihasanoglu, A., Bharwani, S. and Jack, C., 2016. Dialogue for decision-making: unpacking the ‘City Learning Lab’ approach. FRACTAL working