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• mwr_2024_08_for_print.pdf

  , Northern Ireland and northern England. Following this the temperatures returned to around average for many and below average for northern areas. Scotland in particular saw cooler than average temperatures in the second half of the month. On the 22nd, the 12th named storm of the season arrived: Storm Lilian

• southern-africa-climate-risk-report-trd-final.pdf

  increase and the number of days exceeding 35°C (40°C) is projected to increase by 15-35 (0-5) days per year across the zone. • There is no decisive trend for whether Zone 5 will become wetter or drier, although there is evidence for a small delay to the start of the rainy season. Year-to-year

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

  increase and the number of days exceeding 35°C (40°C) is projected to increase by 15-35 (0-5) days per year across the zone. • There is no decisive trend for whether Zone 5 will become wetter or drier, although there is evidence for a small delay to the start of the rainy season. Year-to-year

• ukcp18-weather-types-factsheet-november-2025.pdf

  projections indicate that, on average, UK winter weather conditions are expected to become milder and for certain weather types, wetter. We focus here on the UK winter season when specific conditions are expected to have more significant impacts. • The UK experiences two dominant weather types

• ukcp18-weather-types-factsheet-november-2025pdf

  projections indicate that, on average, UK winter weather conditions are expected to become milder and for certain weather types, wetter. We focus here on the UK winter season when specific conditions are expected to have more significant impacts. • The UK experiences two dominant weather types

• mearns_2013_narccap.pdf

  of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation

• mearns_2013_narccappdf

  of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation

• Met Office supports Tonga to make history with first ever presented television weather broadcast

  Warning Systems in Tonga  Forecasting the weather in Tonga can be challenging at times due to its location and size. Located within an area of the south Pacific which is affected by tropical cyclones at certain times of the year, some extreme conditions can affect the islands. In the wet season

• williams15victoriabasinrcmperformance.pdf

  to be much wetter over the lake (biases as large as 8 mm/day with respect to CPC- FEWS). The discrepancy between the amount of rain in the model and in observations is particularly pronounced in the late rainfall season (SON), but the bias is also present in the off-peak seasons. The bias is present

• williams15victoriabasinrcmperformancepdf

  to be much wetter over the lake (biases as large as 8 mm/day with respect to CPC- FEWS). The discrepancy between the amount of rain in the model and in observations is particularly pronounced in the late rainfall season (SON), but the bias is also present in the off-peak seasons. The bias is present