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• mogreps-uk-ps47-asdi-pdf-updates-2.0.pdf

  . 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 an approximate depth of the snow, m None None Hourly T+0 to T+126 15-minutely T+0h15m to T+126h Hourly T+1 to T+126 Hourly T+0 to T+126 although wet

• factsheet_16-world-climates_2023.pdf

  (Mediterranean, humid sub-tropical and maritime west coast) Temperate climate zones lie between the tropics and the polar circles. The changes in these regions between summer and winter are generally subtle, warm or cool, rather than extreme, burning hot or freezing cold. However, a temperate climate

• mogreps-uk-ps47-asdi-pdf-updates-20pdf

  . 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 an approximate depth of the snow, m None None Hourly T+0 to T+126 15-minutely T+0h15m to T+126h Hourly T+1 to T+126 Hourly T+0 to T+126 although wet

• ukcp-climate-drifts-report.pdf

  12, the evolving NH extratropical drift becomes large, lying between 1-2 °C during years 80-100 (equivalent to the UKCP18 baseline period of 1980-2000) and nearly reaching 4 °C by year 150, after which it reduces more slowly. In member 11, the drift is more modest (~ 0.5 °C) during years 80-100

• ukcp18-factsheet-using-rainfall-data-from-ukcp-v2.pdf

  with increasing return period over the southern UK (the observations typically lie within the 12-member ensemble spread, Figure 2). However, all models have biases compared to the real world, but they can still provide useful information. Over the northern regions, the CPM generally underestimates

• factsheet_16-world-climates_2023pdf

  (Mediterranean, humid sub-tropical and maritime west coast) Temperate climate zones lie between the tropics and the polar circles. The changes in these regions between summer and winter are generally subtle, warm or cool, rather than extreme, burning hot or freezing cold. However, a temperate climate

• arrcc_carissa_ws4_observational_datasets-v2.pdf

  troposphere shifts northwards during break and lies approximately above the lower monsoon trough. This seems to provide an effective process of removing ascending air in the lower monsoon trough causing exceptionally heavy rainfall over Assam and along the foot of the Himalayas. Specifically

• Report on remote training workshop - Sea-level science and the use of sea-level projections in Bangladesh

  of sea-level rise on low-lying coastal areas in South Asia by working with organisations in the region to improve the provision and use of sea-level projections. Reviews of the recent scientific literature on sea-level science information and services for Bangladesh (Harrison et al., 2020a

• global-10km-ps47-asdi-pdf-updates-2.0.pdf

  from T+150 to T+168 T+150 to T+168 relative_humidity_on_pressure_levels snow_depth_water_equivalent Fractional relative humidity (ratio of the partial pressure of water vapour to the equilibrium vapour pressure of water) on pressure levels. Liquid water equivalent (LWE) depth of the snow lying

• paper1_observing_changes_in_the_climate_system.pdf

  shows the approximate 95% confidence range for the HadCRUT4 data (the ‘true’ global average is expected to lie outside this range around only 5% of the time). (Source: Met Office) Year-to-year variations of global mean surface temperature are strongly affected by natural variations in the climate