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• Climate information for international development

  Working in partnership with scientific institutions in developing countries to generate and communicate information on climate variability and change

  The Climate Information for International Development team is a diverse mix of scientific software engineers and scientists working to generate, analyse and communicate information to a range of customers. Activities include scientific analysis and training, model development, regional climate

• UK Climate Projections (UKCP18)

  The UK Climate Projections (UKCP18) provides a comprehensive set of climate model projections for the UK, showing how the climate is likely to change in the future.

  Please be aware we are introducing UK Climate Information (UKCI) - a new national climate service being developed to support climate adaptation decision-making across the UK. UKCP18 remains the recommended and validated national climate dataset, so users should continue to use its data, guidance

• Sea ice in the climate system

  Arctic sea ice is a sensitive indicator of climate change and changes to the sea ice cover can have potential implications for the Arctic region and beyond.

  Found in both the Arctic and Antarctic, sea ice regulates heat exchange between the ocean and atmosphere, supports polar ecosystems, and serves as a sensitive indicator of climate change. Sea ice forms in high-latitude regions where winter darkness and cold temperatures allow the ocean to freeze

• State of the Global Climate: 2017

  The annual state of the Climate report highlights 2017 as one of the top three warmest years on record.

  An international analysis of the global climate of 2017 has been published in the annual report, ‘State of the Climate in 2017’ released yesterday by the American Meteorological Society. The report highlights that 2017 is among the top three warmest years for global temperature since records began

• Winter and February climate statistics

  and Africa leading to the season’s highest temperature of 18.4 °C at Santon Downham (Suffolk) on 24 February. Dr Mark McCarthy is the head of the Met Office National Climate Information Centre. He said: “February 2021 has seen a wide temperature range resulting from the two predominant weather patterns

• Weather forecasts and climate data

  Here's your one-stop shop for weather and climate information

  syndicated email containing up to date forecast information for publication. Contact enquiries@metoffice.gov.uk   Social media  The Met Office continually posts up to date weather and climate information across a range of social media channels including Twitter,Facebook and Instagram.  Past weather

• state-of-the-uk-climate-2014-v3.pdf

  by the Joint UK DECC/Defra Met Office Hadley Centre Climate Programme (GA01101). 4 Executive Summary Land temperature l 2014 was the warmest year on record for the UK, England, Wales and Scotland in a series from 1910, and for Central England in a series from 1659. l 8 of the 10 warmest years

• paper3_implications_for_projections.pdf

  with the previous generation, although they simulate global patterns of climate and climate change with greater fidelity. Despite the recent pause in the global mean surface temperature rise, the upper ranges of TCR and ECS derived from extended observational records, and specifically including

• wiser-mena-scoping-study-external-v2.pdf

  region, there is either a National Meteorological Service (NMS) or a National Meteorological and Hydrological Service (NHMS). NMS or NMHSs are responsible for observing the weather and keeping climate records, forecasting the weather at various timescales and for developing and delivering forecast

• The Met Office Hadley Centre Climate Programme: Driving Climate Science for a Resilient Future

  study of the UK’s record-breaking annual temperature in 2022, where human-induced climate change made this event around 160 times more likely.  In December 2023, the Met Office annual global temperature forecast was published. Global average temperature rise is measured as the difference between 1850