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• New radar noise level estimator

  — this is an easy case, without significant contamination. This demonstrates that the new scheme is able to perform at least as well as the existing scheme in normal conditions, while showing better skill at rejecting outliers. A more interesting case In contrast to the above example, in the following case

• Met Office Pricing Policy

  economic activity on a value basis, at a price which is lawful, profitable and which the customer is willing to pay. 4.4. Standard prices and standard pricing structures are reviewed at least annually, at which time they may be updated and reissued. Longer-term contracts and related pricing are typically

• england-and-wales-drought-2010-to-2012---met-office.pdf

  , there were also significant droughts in 1990-92, 1995-97 and 2004-06. The 1975-76 drought was the most significant drought for at least the last 150 years in the UK, and is usually regarded as a 'benchmark' against which all other droughts are compared. Much of England and Wales received less than 65

• reinhard-k-h-schiemann-grenville-lister-rosalyn-hatcher-dan-hodson-bryan-lawrence-len-shaffrey-andrea-dittus-jon-robson-ben-harvey-kevin-hodges-oscar-martinez-alvarado-steve-woolnough-andrew-turnerpdf

  , a little weaker than in RAPID (Fig. 7c) Figure 7: a) AMOC at 26°N (Sv). Olive green: ensemble mean. Shading is the ensemble range. Red (blue) member with least (greatest) AMOC decline over 1980- 2014: -0.5 (-1.6) Sv/decade. Black line: Observed AMOC (RAPID). Black dots: Observed AMOC (Bryden et al., 2005

• information_brief_final_12-12-2016.pdf

  decisions with planning time horizons of at least 30 years – e.g. energy infrastructure investment decisions or deciding where to locate new housing developments. Used in conjunction with historical tropical cyclone risk information, decision makers can determine whether or not plans or policies may

• reinhard-k.-h.-schiemann-grenville-lister-rosalyn-hatcher-dan-hodson-bryan-lawrence-len-shaffrey-andrea-dittus-jon-robson-ben-harvey-kevin-hodges-oscar-martinez-alvarado-steve-woolnough-andrew-turner.pdf

  , a little weaker than in RAPID (Fig. 7c) Figure 7: a) AMOC at 26°N (Sv). Olive green: ensemble mean. Shading is the ensemble range. Red (blue) member with least (greatest) AMOC decline over 1980- 2014: -0.5 (-1.6) Sv/decade. Black line: Observed AMOC (RAPID). Black dots: Observed AMOC (Bryden et al., 2005

• Briefing on Arctic and Antarctic sea ice - June 2022

  have been relatively high in parts of the Central Arctic. However, uncertainty is substantial. Given the very mild weather during winter, at least part of the apparently higher ice thickness may be associated with the relatively muted ice melt of the preceding summer. Figure 6. Arctic sea ice

• ar12_all_v03.compressed.pdf

  the team that visited the site (top left) and the tower itself which is 230 m high (top right). The sampling inlet is at 222 m up the tower. The bottom half of the image shows the instrumentation set up inside the building next to the tall tower. The centre image shows sampling valves for the GC-FID

• ExCALIBUR Fusion Modelling System Science Plan

  gyrokinetic models are currently at or beyond the limit of current HPC capability in terms of scalability. Kinetic levels of complexity are nonetheless going to be necessary (at least locally) for modelling the burning plasma regime, due to the inherent uncertainty in the fluid codes. The plasma

• high-impact-low-likelihood-scenarios-for-the-uk-background-reportpdf

  High-impact lowlikelihood climate scenarios for the UK Background report N.W. Arnell 1 , E. Hawkins 2 , T.G. Shepherd 1 , I.D. Haigh 3 , B. Harvey 2 , L. Wilcox 2 , L. Shaffrey 2 & A.G. Turner 1,2 1 Department of Meteorology, University of Reading 2 National Centre for Atmospheric Sciences