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phase precipitation being considered as a liquid water equivalent (lwe) value. It includes the contribution from the model convection scheme if this is invoked (true for Global models but not the UK models) as well as that from the model precipitation scheme. m s-1 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm]M

with the ice phase precipitation being considered as a liquid water equivalent (lwe) value. It includes the contribution from the model convection scheme if this is invoked (true for Global models but not the UK models) as well as that from the model precipitation scheme. m s-1 [YYYYMMDD]T[hhmm]Z-PT

in a fixed position around the station circle so that individual elements can be easily identified. D....D C H or C N s /h s /h s C m or C G(f’)f’f’ ff N s /h s /h s TT N FV’V’ or VV ww TdTd C L or C dd N s /h s h s or N h /h TwTw P wa P wa H wa H wa or PPP pppa or pppa W 1 W 2 D s v s Figure 11

of Change Step 1. Analyse the context & discuss the need(s) your project aims to address Following these steps will show how your project ‘unfolds’ to create the changes and impact it wants to support. By the end of these steps, you will have developed a ToC map and narrative (as shown in this 'How

and distributed by aviso, with support from cnes. http://www.aviso.altimetry.fr/duacs/, 2014. M. J. Best, M. Pryor, D. B. Clark, G. G. Rooney, R .L. H. Essery, C. B. Ménard, J. M. Edwards, M. A. Hendry, A. Porson, N. Gedney, L. M. Mercado, S. Sitch, E. Blyth, O. Boucher, P. M. Cox, C. S. B. Grimmond, and R. J

/wiser The views expressed in this publication are the sole responsibility of the author(s) and do not necessarily reflect the views of FCDO or the Met Office, UK. Images: I-stock; Robert Powell, Paul Watkiss. Citation. Watkiss, P. and Cimato, F. (2022). How to Note 1: Commissioning Socioeconomic Benefit

. These changes are calculated from the population data in the 'middle of the road' socio-economic scenario (SSP2), used throughout the poster. References Dankers, R., Arnell, N. W., Clark, D. B., Falloon, P. D., Fekete, B. M., Gosling, S. N., Heinke, J., Kim, H., Masaki, Y., Satoh, Y., Stacke, T., Wada, Y

and chloroform emissions, together with ozone and hydrogen deposition have been characterised, leading to the estimation of methane emission rates for each event. The mean methane emission flux was found to be 400 ± 90 ng m - 2 s -1 . A strong seasonal cycle was found in the methane emission fluxes

., Colle, B. A., Pfahl, S., Pinto, J. G., Quinting, J. F. & Seiler, C. (2019) The Future of Midlatitude Cyclones. Current Climate Change Reports, 5, 407-420. https://doi.org/10.1007/s40641-019-00149-4 Economou, T., Stephenson, D. B., Pinto, J. G., Shaffrey, L. C. & Zappa, G. (2015) Serial clustering

- - - Wet Bulb Freezing Level m AMSL Hourly to T+360 - - - Relative Humidity % Hourly to T+360 Three-hourly to T+360 - Local Midday / Midnight to Day 15 Mean Sea Level Pressure Pa Hourly to T+360 Three-hourly to T+360 - Local Midday / Midnight to Day 15 Wind Wind Speed m/s Hourly to T+360 Three-hourly