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• state-of-the-uk-climate-2014-v3.pdf

  and excluding stations above 500 metres above sea level. 34 SNOW The winter months of 2014 were mostly dominated by a mild Atlantic weather type and consequently there were no major snowfalls during the year across the UK. The most significant snowfall occurred on 26 December 2014 with lying snow

• 20150730 LE Final Report v8 clean

  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

• east-africa-climate-risk-report-finalpdf

  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

• central-africa-climate-risk-report-trd-finalpdf

  with little choice but to settle in riskier places (Hallegatte, 2017; Dodman et al, 2022). Those include low-lying areas of the rapidly growing coastal cities of Pointe- Noir (R. Congo), Libreville (Gabon), Luanda and Lobito (Angola), Malabo (Equatorial Guinea) and Douala (Cameroon), threatened

• state-of-the-uk-climate-2014-v3pdf

  and excluding stations above 500 metres above sea level. 34 SNOW The winter months of 2014 were mostly dominated by a mild Atlantic weather type and consequently there were no major snowfalls during the year across the UK. The most significant snowfall occurred on 26 December 2014 with lying snow

• east-africa-climate-risk-report-final.pdf

  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

• central-africa-climate-risk-report-finalpdf

  retreat is a particular risk in Central Africa due to the profusion of low-lying sandy beaches; a 2018 study identified erosion hotspots in Gabon and Angola and two accretion hotspots in Angola/DRC (Luijendijk et al., 2018). 21 2022, Met Office Figure 3: Baseline climate for the Central Africa region

• Regional climate change trends and uncertainty analysis using extreme indices: A case study of Hamilton, Canada

  (83 members) along with its 10th and 90th percentiles (uncertainty bounds) in the projection time frame (1950–2098). For annual total precipitation and maximum 1-day precipitation, the two scenarios of RCP 4.5 and RCP 8.5 have very similar pattern and boundaries. Observed total precipitation lies

• 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