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• report-on-regional-sea-level-projections-for-south-asia---arrcc-report---external-1.pdf

  change scenarios. • The projection ranges are based on the 5th to 95th percentiles of the underlying model distributions. There may be a greater than 10% chance that the real-world response lies outside the 5th to 9th percentile range and this likelihood cannot be accurately quantified. Substantial

• ukv-parameters-may-2019.pdf

  ; 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

• mogreps-g-documentation-external-data.pdf

  - 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

• ukv-parameters-may-2019pdf

  ; 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

• trd---climate-risk-report-for-csa---v4-final-april-2026pdf

  , river basins 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

• trd---climate-risk-report-for-csa---v4-final.pdf

  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

• wcssp-programme-science-workshop-report---final-111219.pdf

  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

• ukv-2km-ps47-asdi-pdf-updates.pdf

  . Hourly T+0 to T+54 3-hourly T+57 to T+120 snow_depth_water_equivalent snowfall_accumulation-PT01H snowfall_accumulation-PT03H snowfall_rate Liquid water equivalent (LWE) depth of the snow lying on the surface (ground). Typically, water is 10 times as dense as snow so multiplying by 10 gives

• sigwx-interpretation-guide-v201pdf

  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

• sigwx-interpretation-guide-v2.01.pdf

  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