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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
). 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
, 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
and NHS inform. Dr Siama Latif, NHS 24’s Associate Medical Director said: “When the weather gets colder this can have an impact on everyone’s health and wellbeing, but especially those who could be considered vulnerable, such as the very young, the elderly, or those with long-term health conditions
the necessary data needed to support a range of energy modelling for sub-seasonal to climate timescales. This effort is specifically focused on understanding the energy needs for the 2030’s and beyond. Working with Ofgem, the Department for Energy Security and Net Zero (DESNZ), the Climate Change
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