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of the major Kyoto gases (CO 2 , CH 4 , and N 2 O) and to run atmospheric observation sites at any proposed additional site/s across the UK. 4. To make high-quality real time measurements of the major Kyoto gases at any additional observation site(s), consistent with the requirements set out above. 5
in April and May as in a). 6 References 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. Harding. The Joint UK Land Environment
, 2019b) • Further information and guidance is available at the UK Climate Projections website. www.metoffice.gov.uk Pg 5 of 6 Source: Met Office © Crown Copyright 2019 References Brown S, Boorman P and Murphy J (2010). Interpretation and use of future snow projections from the 11-member Met Office
A B C D E F G H I J K L M N O P Q R S T U V W X Y Z A AC Altocumulus AD Aerodrome AGL Above ground level AIMMS Aircraft Integrated Meteorological Measurement System AMD Amend or amended AMSL Above mean sea level AOD Aerosol Optical Depth APR April
) was the most severe tropical cyclone to ever make landfall in the Philippines (right - NASA satellite image on November 7 th 2013). Maximum wind speeds peaked at 88m/s (197mph) and a storm surge produced wave heights reaching 5-6m above normal in some regions of Leyte. Yolanda caused widespread
Product user manual For Global Ocean level-1 data products from the Met Office Global Coupled Atmosphere-Land-Ocean-Ice system Contributors: J Roberts-Jones, M. Price, S. Moreton, R. King Date: December 2024 Ocean Products User Guide, Met Office Global Coupled Atmosphere-Land-Ocean-Ice system Date
Office North-West European Shelf forecasting system. Ocean Sci.,15(4), https://doi.org/10.5194/os-15-1133-2019. Graham, J. A., E. O’Dea, J. Holt, J. Polton, H.T. Hewitt, R. Furner, K. Guihou, A. Brereton, A. Arnold, S. Wakelin, J.M. Castillo Sanchez, C.G. Mayorga Adame (2018) AMM15: A new
- interaction region structure, leading shock - peak velocity, density, Alfvénicity of fast streams NOAA: warning when GOES electron fluxes at GEO exceed 10^3 e/(cm 2 s sr) Kilpua et al., GRL, 2015 Storm driver CME sheath CME ejecta + slow wind CME ejecta + fast wind interacKon region + faster
, L. M. Mercado, S. Sitch, E. Blyth, O. Boucher, P. M. Cox, C. S. B. Grimmond, and R. J. Harding. The Joint UK Land Environment Simulator (JULES), model description part 1: Energy and water fluxes. Geoscientific Model Development, 4(3):677–699, 2011. doi: 10.5194/gmd-4-677-2011. URL http://www.geosci
Offshore Technology Conference OTC-35733-MS A Spatiotemporal Machine Learning Framework for the Prediction of Metocean Conditions in the Gulf of Mexico: Application to Loop Current and Loop Current Eddy Forecasting E.C.C. Steele 1 , M.C.R. Juniper 1 , A.C. Pillai 2 , I.G.C. Ashton 2 , J. Chen 3 , S
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