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• Annual to Decadal Climate Update FAQs

  Annual to Decadal Climate Update provides a synthesis of global annual and multi-year computer model predictions (forecasts) covering the next five years.

  of climate prediction. However, it is still unclear just how competently machine learning will predict events that have not yet been seen in the observational record. 8. How can I access the Annual to Decadal forecast data? To access the forecast data, send your request to wmolc-adcp@metoffice.gov.uk. This is raw data in netcdf format provided for research purposes for someone who has experience working with climate data.

• Sharing our weather and climate expertise

  We are a world authority on weather and climate science.

  Weather and climate stories are rarely out of the headlines, meaning that the views of our media-trained experts are frequently sought by media and others around the world. Covering so many topics affecting the world’s weather and climate means we have a lot to talk about. How you can follow us

• Transforming climate resilience in tea production

  The Tea-CUP project is changing how climate services are delivered by developing actionable information to address the challenges of climate change within the tea industry, informing adaptation measures and decision-making.

  , and climate change is posing significant challenges to the tea industry in China, the UK and beyond. In the Tea-CUP project (Co-developing Useful Predictions) scientists from the Met Office and China have been working with tea experts and local farmers in Yunnan Province to understand what seasonal

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

  in these islands are greater than 1500mm per year (Figure 4). Observed trends in regional climate for Southern Africa Observational records show that Southern Africa’s average annual surface temperatures increased by between 1°C and 1.5°C from 1961 to 2015. Minimum temperatures have increased more

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

  in these islands are greater than 1500mm per year (Figure 4). Observed trends in regional climate for Southern Africa Observational records show that Southern Africa’s average annual surface temperatures increased by between 1°C and 1.5°C from 1961 to 2015. Minimum temperatures have increased more

• climate-risk-report-for-sea---v6-final-april-2026.pdf

  as a result of human-induced climate change (Oliver et al., 2018). This marine heatwave persisted for 298 days, the longest on record for this region, with an average intensity of 2°C (Iskandar et al., 2021). Precipitation has generally increased by around 0.2- 0.5mm/day per decade, although this trend

• 2024: record-breaking watershed year for global climate

  2024 was the warmest year on record globally and the first year that was likely more than 1.5°C above pre-industrial levels: a stark reminder global temperatures are continuing to rise.

  exceeded the previous warmest year – 2016 - by 0.17°C, making 2024 and 2023 the warmest and second-warmest years on record.   A number of global climate centres will be releasing their 2024 average temperature figures today.  The latest figures highlight how the world is getting closer to breaching

• trd---climate-risk-report-for-csa---v4-final.pdf

  to lack of reliable observation records (Fallah et al., 2023). Central Asian countries such as Kyrgyzstan and Tajikistan have very complex topography which requires high resolution climate data (~30km) for regional trend attribution studies (Fallah et 16 al., 2023). Central Asian trend attribution

• 02278 great place to work - its who we are - AUG 23 UPDATE

  Ross Archivist We’re experts by nature. It’s who we are. What I do makes a difference... ...because my work at the National Meteorological Library & Archive supports climate scientists by preserving important historical records and valuable data. Extraordinary impact and benefit To make a difference

• paper2_recent_pause_in_global_warming.pdf

  this? First, periods of slowing down and pauses in surface warming are not unusual in the instrumental temperature record. Second, climate model simulations suggest that we can expect such a period of a decade or more to occur at least twice per century, due to internal variability alone. Third