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• Week ahead forecast: Wet weather continues, but signs of change for Christmas

  , with the potential for drier and less mild weather. Let’s take a closer look at what to expect day by day, and how the broader weather patterns are shaping up for the festive season. A wet start to December The first half of December has been exceptionally wet in many areas, with some locations

• wiser0065-scipea-impact-article_hydropower-0618.pdf

  Powering up the forecasts East Africa has distinct wet and dry seasons, and accurately predicting the onset of its rains is vital for farms and businesses. Yet hydropower is equally reliant on accurate and timely forecasts – as an important climate partnership project recently demonstrated

• ukcp-cmip5-downscaling-report.pdf

  member of RCM-PPE that gives lower PSS values though). This is consistent with the large (and significant) cold and wet biases seen in the north of the UK in this model in this season (Figures 16 and 18). The nested CPM-MRI reduces the contribution to the total rainfall from days with high rainfall

• ukcp-cmip5-downscaling-reportpdf

  member of RCM-PPE that gives lower PSS values though). This is consistent with the large (and significant) cold and wet biases seen in the north of the UK in this model in this season (Figures 16 and 18). The nested CPM-MRI reduces the contribution to the total rainfall from days with high rainfall

• north-west-england--isle-of-man_-climate-met-office.pdf

  that falls in these seasons. In summer, convection caused by solar surface heating sometimes forms shower clouds and a large proportion of rain falls from showers and thunderstorms then. A further factor that greatly affects the rainfall distribution is altitude. Moist air that is forced to ascend hills

• north-west-england--isle-of-man_-climate-met-officepdf

  that falls in these seasons. In summer, convection caused by solar surface heating sometimes forms shower clouds and a large proportion of rain falls from showers and thunderstorms then. A further factor that greatly affects the rainfall distribution is altitude. Moist air that is forced to ascend hills

• richard-jones---k-scale-year-long-global-um-simulations-for-dyamond-3-at-convection-permitting-resolutionpdf

  RAL3.3 S Amer Africa SE Asia “DYAMOND3” Takasuka et al (2024); Grey-scale = incomplete and not yet available Regional evaluation of resolution and physics dependencies Increasing model resolution 5/3 scaling Parametrised convection GPM Explicit convection Claudio Sanchez Results from earlier DYAMOND

• richard-jones---k-scale-year-long-global-um-simulations-for-dyamond-3-at-convection-permitting-resolution.pdf

  RAL3.3 S Amer Africa SE Asia “DYAMOND3” Takasuka et al (2024); Grey-scale = incomplete and not yet available Regional evaluation of resolution and physics dependencies Increasing model resolution 5/3 scaling Parametrised convection GPM Explicit convection Claudio Sanchez Results from earlier DYAMOND

• climate_outlook_user_guide_0520.pdf

  is gained. A climate of a particular place is often described in seasonal periods (e.g. summer/ winter or rainy/ dry season) over the cycle of the year. The climate can also naturally vary between different years due to the process of Earth system cycles, especially those associated with large

• northern-scotland_-climate-met-office.pdf

  distribution to air frost. However, those places into which cold air can drain are particularly prone to frost. Examples include Altnaharra (Highland) with an average of 73 air frosts per year. In Northern Scotland the frost-free season is o en as little as 3 months, as shown by the average