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for their application. Further guidance on which UKCP product(s) to choose and how to use them in combination is available from Fung et al., (2018). Evaluation of additional time slices We have assessed the performance of the new UKCP Local Transient Projections in representing presentday temperature, precipitation

recommend reading the science report on the PPCE (Murphy et al, 2020) where you can find examples of and explanations for the results that we see (section 3). www.metoffice.gov.uk Pg 4 of 5 Source: Met Office © Crown Copyright 2020 This document can be cited as: Murphy JM, Brown S and Fung F (2020). UKCP

. ‘Time-mean sea-level projections update: Technical note’, Met Office. References Church, J. A., & White, N. J. (2011). Sea-Level Rise from the Late 19th to the Early 21st Century. Surveys in Geophysics, 32(4–5), 585–602. https://doi.org/10.1007/s10712-011-9119-1 Gregory, J. M., Griffies, S. M

at the start of September each year. Since storm naming was introduced in 2015 to improve the communication of severe weather events, the furthest through the list the group has got is to Storm Katie, which impacted the UK in March 2016. 2023/24’s storm naming season is now just one name away from equalling

atmospheric dimethyl sulfide (DMS) to modeled oceanic DMS concentrations and emissions, Atmos. Chem. Phys., 23, 15181–15196, https://doi.org/10.5194/acp-23-15181-2023 *Joge, S. D., et al., (2024), Dimethyl sulfide (DMS) climatologies, fluxes, and trends – Part Classification: 2: Sea–air fluxes

temperatures in the month.   January 2023 mean temperature. Dyce, in Aberdeenshire, had January 2023’s highest temperature with 15.8°C on 24 January, though partly thanks to the Foehn effect, it’s not uncommon for Scotland to see the highest temperature recorded in a winter month.   Drumnadrochit

other specialisms such as those within the social sciences.” Footnotes 1  Christidis, N., Donaldson, G.C. and Stott, P.A., 2010. Causes for the recent changes in cold-and heat-related mortality in England and Wales. Climatic Change, 102(3), pp.539-553.; Mitchell, D., Heaviside, C., Vardoulakis, S

Africa and Ukraine, Policy Report No. 3. (3). 4. Adamenko, T. (2017). Agricultural drought monitoring in Ukraine: Presentation during EvIDENz Workshop 2017. Ukrainian Hydrometeorological Centre. 5. Kovalets, I. V., Kivva, S. L., & Udovenko, O. I. (2015). Usage of the WRF/DHSVM model chain

, повноту або використання сторонніми сторонами його вмісту. Погляди та думки, викладені у звіті, не обов’язково передають або відображають погляди Met Office. Met Office, Фітцрой Роуд, Ексетер, Девон, Велика Британія, EX1 3PB Тел.: +44 330 135 0000 Рекомендоване цитування: Wilson, L., New, S., Daron, J

by the European Union. Views and opinions expressed are however those of the author(s) only and do not necessarily reflect those of the European Union or the Commission. Neither the European Union nor the granting authority can be held responsible for them.