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the decade. Updated decadal forecasts, along with verification of previous forecasts, are available from the Forecast web page. References Smith, D. M., S. Cusack, A. W. Colman, C. K. Folland, G. R. Harris and J. M. Murphy, 2007, Improved surface temperature prediction for the coming decade from

an entirely separate building. A professional market rental valuation of the space has not been undertaken and is not required. The Union Office is included within the overall Business Rates assessment for Met Office HQ. Information concerning Business Rates is publically available via www.voa.gov.uk. 2. Cost estimated as standard office overheads for 0.75 fte staff member plus travel for staff case visits & H&S related meetings (less than £1k per annum).

. 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

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

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

for the global latitude-longitude grid used in Numerical Weather Prediction [Buckeridge & Scheichl, 2010]. The key idea is to use conditional coarsening in the N-S direction while increasing the mesh spacing uniformly in the E-W direction.  The Figure below shows an example of a semi-coarsened mesh. Using

the WISER brand, please email us. Current WISER Opportunities The Met Office is currently seeking consultancy support for the scoping phase of the WISER programme. WISER MEL Consultant The Met Office is seeking to appoint a Consultant(s) with necessary international development and MEL experience

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