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and intense storm surges threaten livelihoods and local economies, with potential ripple effects throughout the region. This is because the ports of Djibouti, Berbera, Lamu, Mombasa, Zanzibar and Dar es Salaam serve the region’s landlocked countries, with the low-lying coasts of Djibouti, Kenya

climate change information benefits of 12.4:1 this lies at the topend of the studies quoted above. Whilst there are two studies exceeding 30:1, most of the studies identified lie in the range of 2: 1 to 14:1. Therefore, when comparing this study’s result it is necessary to consider whether

The distance of model time-series from the observations, outside of the baseline uncertainty, is a good measure of the quality of the current emission map and fully takes into account the allowable uncertainty at each observation time. Any modelled value that lies within the uncertainty

- PT03H Fractional relative humidity (ratio of the partial pressure of water vapour to the equilibrium vapour pressure of water) on pressure levels. Exchange of heat between the surface and the air by motion of air, also called turbulent heat flux. Liquid water equivalent (lwe) depth of the snow lying

. This reflects on the structure of the resulting grids, shown in Figure 6. Figure 3 shows the total emissions and uncertainty, concentrating on UK, Ireland, Benelux, NWEU and EU27. There is very little difference between the ExpY2a and ExpY1 solutions, both lie within the uncertainty of the bottom-up

; negative is downward. W m-2 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm] M-sensible_heat_flux_at_surface.nc Hourly (0-54) 3-hourly (51-120) Instantaneous snow depth water equivalent Liquid water equivalent (LWE) depth of the snow lying on the surface (ground). Typically water is 10 times as dense as snow so

are considered during the socio-economic analysis e.g., the source of the Amu Darya and Syr Darya rivers lies in Zone 2 (a climatologically distinct mountainous zone) whereas the discharge of these rivers is in Zone 1 (an arid desert climatological zone). In this case, it makes sense to conduct an upstream

measure of uncertainty. ✓ Improve understanding of importance of non-climatic factors (urban development, natural variability) on future climate changes. ✓ Understanding where benefits lie for resolution vs complexity vs ensembles. What’s the correct priority of these factors? ✓ Is high resolution

(and positive compared to negative) which enhances the higher sea-level projections at this point. This effect is not surprising, since Diamond Harbour and Hiron Point lie by or in inland waterways of the Ganges-Brahmaputra-Meghna Delta, a region susceptible to subsidencebased VLM on mm/yr timescales

to FL190. Figure 18: Icing call-out interpretation 3.8.4. In WAFC charts produced from the SWM BUFR data sets, icing areas that lie inside of the CB areas has been removed. This is to ensure that the forecast information remains clear for display systems that cannot use different line styles or colours