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• global-coupled-ocean-level1-product-userguide.pdf

  ..................................................................................................8 III.2 List of variables ............................................................................................9 III.3 File names

• CSSP_city_pack_BELFAST

  Concentration Pathways (RCPs) used in climate modelss to describe possible futures based on assumptions about green house gas emissions. In RCP2.6 global emissions are strongly mitigated and reduced. Global temperature rise is kept below 2°C. In RCP8.5 global emissions grow unmitigated and global

• global-coupled-ocean-level1-product-userguidepdf

  ..................................................................................................8 III.2 List of variables ............................................................................................9 III.3 File names

• public-weather-service-customer-supplier-agreement-2025-30-websitepdf

  Customer Supplier Agreement For the provision of the UK Public Weather Service 2025-2030 Met Office Ref No: L7543 Date agreement comes into effect: 1 April 2025 SECTION 2: PWS PERFORMANCE MEASURES, DELIVERABLES, SERVICES AND REPORTING FOR 2025-30 Contents SECTION 2: PWS PERFORMANCE MEASURES

• annual_report_2022mo.pdf

  : Met Office Annual Report & Accounts Session: 2021/22 HC 741 ISBN: 978-1-5286-3480-9 Ordered by the House of Commons to be printed 20 October 2022 Correction: Page 4 – ISBN Text currently reads: 978-1-5286-2756-6 Text should read: 978-1-5286-3480-9 Date of correction: 24 October 2022 2 Performance

• annual_report_2022mopdf

  : Met Office Annual Report & Accounts Session: 2021/22 HC 741 ISBN: 978-1-5286-3480-9 Ordered by the House of Commons to be printed 20 October 2022 Correction: Page 4 – ISBN Text currently reads: 978-1-5286-2756-6 Text should read: 978-1-5286-3480-9 Date of correction: 24 October 2022 2 Performance

• benni-buchenau-mike-bell-john-edwards--to-what-extent-can-bjerknes-compensation-explain-a-weak-amoc-in-gc5-lfric.pdf

  Coupled Atmosphere only To What Extent Can Bjerknes Compensation Explain a Weak AMOC in GC5-LFRic? Benni Buchenau, Mike Bell and John Edwards (Met Office) 1. The Problem 2. Direct Driver: Too-Small Sea-Air Heat Fluxes from the Labrador Sea Figure 1: Time series of modelled North Atlantic AMOC

• Briefing on Arctic and Antarctic sea ice - June 2026

  was below average across all marginal seas of the Arctic Ocean, ice retreat having begun earlier than average in all areas (Figure 2). Figure 2. Arctic sea ice extent on 10th June 2026, with 1981-2010 average extent indicated in orange, and the regions referred to in the text labelled. Data are from

• benni-buchenau-mike-bell-john-edwards--to-what-extent-can-bjerknes-compensation-explain-a-weak-amoc-in-gc5-lfricpdf

  Coupled Atmosphere only To What Extent Can Bjerknes Compensation Explain a Weak AMOC in GC5-LFRic? Benni Buchenau, Mike Bell and John Edwards (Met Office) 1. The Problem 2. Direct Driver: Too-Small Sea-Air Heat Fluxes from the Labrador Sea Figure 1: Time series of modelled North Atlantic AMOC

• Briefing on Arctic and Antarctic sea ice - June 2019

  week following over two months of record or near-record lows (Figure 1).  Figure 1. Daily Arctic sea ice extent for 2019, compared with recent years and the 1981-2010 average with ± 1 and 2 standard deviation intervals indicated by the shaded areas. Data are from the National Snow and Ice Data Center