Search results (1,217)

0.5ᵒC everywhere (with an average difference of 0.1ᵒC on a temperature increase of 2.5ᵒC for the British Isles as a whole). Fixing the graupel code error also significantly 2 impacts simulated present-day precipitation in winter, with the fixed-code run somewhat wetter although still not as wet

at the Met Office Your career Vacancies Rewards and benefits Equality, diversity and inclusion Equality, Diversity & Inclusion Progress Report 2022-23 Apprentices, graduates and placements Settings A change in the pollen season – but is it worse than normal? Author: Press Office 10 June 2022 The effects

associated with an intense storm system passing over the UK, or a notably hot or cold day. Climate hazards relate to exceptional conditions over periods of months to seasons such as the exceptional wet winter of 2013/14, or summer droughts and heatwaves spanning several weeks or even months

Scottish Highlands. The course of mean monthly rainfall for 1981 - 2010 for 4 sites is shown below. Whilst rainfall is generally welldistributed through the year, there is a seasonal pattern. The driest season is spring whilst in the wetter upland areas there is an autumn/winter maximum, when

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

the UK and they ‘block’ the passage of depressions. These anticyclones are most common in spring but can occur in all seasons — sometimes they can persist for a month or more and completely change the character of the weather. In summer, the blocking anticyclones can bring a prolonged spell of warm

-season sea surface temperatures in the tropical Atlantic and Pacific. The detailed methodology is described in Part 2. For this forecast the GloSea5 component comprised an aggregation of 42 GloSea5 predictions (ensemble members) initialised between 23 January and 12 February which cover the period

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

proxy observations (see ‘What do the projections show in recent climate?’ for more details). In the recent climate (1980-2000), the Global PPE-15 and Regional RCM-12 models agree well with the proxy observations in terms of duration and magnitude of the summer dry season, but show a delay in season

proxy observations (see ‘What do the projections show in recent climate?’ for more details). In the recent climate (1980-2000), the Global PPE-15 and Regional RCM-12 models agree well with the proxy observations in terms of duration and magnitude of the summer dry season, but show a delay in season