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Areas of expertise Dispersion for emergency response applications Radiological dispersion modelling My Publications - Leadbetter, S Current activities The main focus of Susan's work is on the application of the Met Office's Met Office Dispersion Model (NAME) to the accidental release of pollutants

. The only factors affecting ET O are weather parameters i.e., temperature, wind speed, relative humidity and sunshine hours. The FAO Penman- Monteith equation is suggested as the single method for determining ET O . ET o 900 0.408��R n � G� � � U 2 ( e mm / day� � T � 273 � � � (1 � 0.34U ) � 2 s � e

McSweeney et al. (2015). Maps show monsoon circulation in 850 hPa flow for JJA for observations from ERA40 and a selection of CMIP5 models. Categories from the assessment are given in brackets for the CMIP5 models: IP – implausible, SB – significant biases, B – biases, S – satisfactory They find

, D, McCarthy, MP, Kendon, M, Legg, T, Simpson, I. HadUK-Grid—A new UK dataset of gridded climate observations. Geosci Data J. 2019; 6: 151– 159. https://doi.org/10.1002/gdj3.78 Kendon, M., McCarthy, M., Jevrejeva, S., Matthews, A., Williams, J., Sparks, T., & West, F. (2023). State of the UK Climate

Press, Cambridge, United Kingdom and New York, NY, USA. van Vuuren, D.P., Edmonds, J., Kainuma, M.L.T., Riahi, K., Thomson, A., Matsui, T., Hurtt, G., Lamarque, J.-F., Meinshausen, M., Smith, S., Grainer, C., Rose, S., Hibbard, K.A., Nakicenovic, N., Krey, V., Kram, T. 2011. Representative

://doi.org/10.1007/s00382-022- 06403-0 Hollis, D, McCarthy, MP, Kendon, M, Legg, T, Simpson, I. HadUK-Grid—A new UK dataset of gridded climate observations. Geosci Data J. 2019; 6: 151– 159. https://doi.org/10.1002/gdj3.78 Kendon, M., McCarthy, M., Jevrejeva, S., Matthews, A., Williams, J., Sparks, T

in the projected loss of ice from the Antarctic ice sheet (Figure 2a). These revised projections show good agreement with independent work carried out at the Met Office for UKCP18 5 . 1 Daangendorf, S. et al (2019), Nature Climate Change: Persistent acceleration in global sea-level rise since

saw extremely high levels of tropical cyclone activity in the Western North Pacific. This was found to be mainly caused by sea surface warming in the eastern and central Pacific, with human influence largely increasing the odds of this event. Zhang et al 2016 Funk, C., Shukla, S., Hoell, A. and Livneh

The news comes as provisional figures from the Met Office show Autumn 2022 (September, October, November) was the third warmest on record for the UK, with an average mean temperature of 11.1C, topped only by 2011 and 2006’s Autumn figures, in a series which goes back to 1884.   In addition

– Fit Functions • Fit function for correlation coefficient ρ HV takes the form: with x = 1 - ρ HV . • Fit function of differential phase Φ DP takes the form: f x = a ⋅ s ⋅ x μ ⋅ e −λ with x = Φ DP - max Φ DP + 10° , where max Φ DP denotes distribution’s maximum, a is an amplitude factor, s a stretch