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          More by Press Office Mist, fog, and haze: What's the difference? Eight interesting facts about Autumn Fact checking climate information Met Office week ahead: Wet, windy but with hints of change Hurricanes, typhoons and tornadoes: What’s the difference? Why do we have seasons? How changing

the difference? Eight interesting facts about Autumn Fact checking climate information Met Office week ahead: Wet, windy but with hints of change Hurricanes, typhoons and tornadoes: What’s the difference? Why do we have seasons? How changing weather patterns are affecting UK wildlife Ocean forecasting

climate information Met Office week ahead: Wet, windy but with hints of change Hurricanes, typhoons and tornadoes: What’s the difference? Why do we have seasons? How changing weather patterns are affecting UK wildlife Ocean forecasting at the Met Office: What are ocean models? Met Office weather extremes

ahead: Wet, windy but with hints of change Hurricanes, typhoons and tornadoes: What’s the difference? Why do we have seasons? How changing weather patterns are affecting UK wildlife Ocean forecasting at the Met Office: What are ocean models? Met Office weather extremes: What are August's current

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

Modelling and WP-MIP - Ron McTaggart-Cowan Machine Learning Emulation of Climate Change Projections for Southeast Asia - Chen Chen Session 2b: AI/ML models and integration with seamless physical model development An AI/ML approach to NWP products using remote sensing data - Amar Jyothi Characterising

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

-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

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