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hours. W m-2 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm]M-sensible_heat_ flux_at_surface_mean-PT06H.nc 6-hourly (150-168) Mean in previous 6 hours 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

in the previous 6 hours. W m-2 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm] M-sensible_heat_flux_at_surface_mean-PT06H.nc 6-hourly (150-168) Mean in previous 6 hours snow depth water equivalent Liquid water equivalent (LWE) depth of the snow lying on the surface (ground). Typically water is 10 times as dense

context. o Maps are used to identify topography, natural resource, population density, agricultural production, water availability and protected wildlife areas (e.g. FAO Aqua maps, WRI Aqueduct mapping tools) • Identification of where the region’s vulnerability to climate-related hazards lie in relation

capture the different seasonal cycles of temperature in the sub-regions although for some there is a greater spread in the simulations (e.g. Southern Africa in October), Model Q16 tends to be consistently the warmest model, and lies apart from the other models, and Q4 the coolest. The temperatures

être clarifiés pour éviter toute confusion: une stratégie est formée de tous ces éléments ▪ Le modèle est trop long et exige une formation complète, en plus du guide, pour être compris ▪ Les questions liées à l’analyse globale ne sont peut-être pas pertinentes, une révision pourrait s’imposer ▪ Les

height is important to fishermen for several reasons. High waves slow down the movement of boats through the water. Very high waves can also swamp the canoes, causing them to take on water faster than it can be bailed out. The canoes have a very low freeboard and an open interior. They lie particularly

and progresses northward (with higher values) to reach the northernmost position between 20° and 22°N (with a value of about 36 °C). The location of ITD, which indicates the northward boundary of the moist southwest monsoon flow, roughly lies over the temperature maximum, and the strength of the flow

monthly rainfall scenarios for six large regions in England and Wales and for the current climate. These were used to sample many more cases than are available from existing observational records, including several hundred extreme regional rainfall events that are meteorologically possible but lie

TECHNICAL SUPPORT BY THE SADIS PROVIDER End users of the SADIS are encouraged to contact the SADIS Provider in the event of problems. The SADIS Provider staff will assist where possible to resolve problems experienced by users if the fault lies within the SADIS. It may of course be the case

and will further enhance the capabilities of NMHS through provision of training from a range of experts from across the consortium. Through convening the national ASPIRE teams, this will also provide enable shared learning from across the project’s activities and identify where synergies lie in the needs