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, Bernie D, Bett PE, Bricheno L, Brown S, Calvert D, Clark RT, Eagle KE, Edwards T, Fosser G, Fung F, Gohar L, Good P, Gregory J, Harris GR, Howard T, Kaye N, Kendon EJ, Krijnen J, Maisey P, McDonald RE, McInnes RN, McSweeney CF, Mitchell JFB, Murphy JM, Palmer M, Roberts C, Rostron JW, Sexton DMH

. Corazza M, P. Bergamaschi, A. T. Vermeulen, T. Aalto, L. Haszpra, F. Meinhardt, S. O'Doherty, R. Thompson, J. Moncrieff, E. Popa, M. Steinbacher, A. Jordan, E. Dlugokencky, C. Brühl, M. Krol, and F. Dentener, Inverse modelling of European N2O emissions: Assimilating observations from different

in the tropical Pacific Niño3.4 region (120 ◦ –170 ◦ W, 5 ◦ N–5 ◦ S): >0.5 ◦ C, between -0.5 and +0.5 ◦ C, and <-0.5 ◦ C, respectively. Current conditions: Source: OSTIA SSTs in the tropical Pacific Niño3.4 3 NINO3.4 SST anomaly plume Met Office forecast from 1 May 2012 Monthly mean anomalies relative to NCEP

., … O’Doherty, S., et al.: Continued increase of CFC-113a (CCl3CF3) mixing ratios in the global atmosphere: emissions, occurrence and potential sources, Atmos. Chem. Phys., 18(7), 4737–4751, doi:10.5194/acp-18-4737-2018, 2018. Arnold, T., Manning, A., … O’Doherty, S., Inverse modelling of CF4 and NF3 emissions

to be tracked by the programme Step 1.2 Define your boundary partners: Next, for the selected dimension(s) of transformation your project is focusing on, define the key stakeholders your project engages or aims to influences to bring about change. The boundary partners are not necessarily only stakeholders

High Energy Radiation Impacts on Ground Level, Aircraft and Space Electronics The Need for an L5 Measurement Package 11-14 May 2015 L5 Consortium Meeting London K A Ryden Prof. C. S Dyer* University of Surrey (Space Centre) * Date and CSDRadConsultancy Ltd “Sic Itur Ad Astra.” © Copyright QinetiQ

Srinivasan, RIMES Dr D. S. Pai, Regional Climate Centre Pune - India Meteorology Department Sayed Reza Mousawi, Afghanistan Meteorological Department Quamrul Hassan, Bangladesh Meteorology Department Dr Indira Kadel, Department of Hydrology and Meteorology, Nepal Sohail Babar Cheema, Pakistan Meteorology

for at least 2 million years. The five warmest years in the UK series from 1884 include 2022, 2023, and 2020 and the ten warmest years have all occurred since 2003. 2023’s provisional mean temperature of 9.97°C puts it just behind 2022’s figure of 10.03°C and ahead of 2014’s 9.88°C. 2023 was also

. These research groups ran 12 climate models and performed over 300 experiments to assess the implications of 2020’s unusual emissions.  Figure 1. The map shows the average change in aerosols across the Earth system models. AOD refers to aerosol optical depth. Green shading shows regions with reduced