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Did you mean banbury's s s?
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 AS Altostratus ASR Altimeter setting region ATD
, 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
- 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
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
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
, 1047-1056, doi:10.1039/C4EM00650J. Cherchi, A., A. Alessandri, S. Masina, and A. Navarra, 2011: Effects of increased CO 2 levels on monsoon. Clim. Dynam., 37, 83-101, doi: 10.1007/s00382-010-0801-7. Climate Profile of India Report, 2010: Met Monograph No. Environment Meteorology-01/2010. [Available
, Brown S, Calvert D, Clark RT, Eagle KE, Edwards T, Fosser G, Fung F, Gohar L, Good P, Gregory J, Harris GR, Howard T, Kaye N, Kendon EJ, Krijnen J, Maisey P, McDonald RE, McInnes RN, McSweeney CF, Mitchell JFB, Murphy JM, Palmer M, Roberts C, Rostron JW, Sexton DMH, Thornton HE, Tinker J, Tucker S
radar reflectivity and differential reflectivity data for rain attenuation: A self-consistent method with constraints. IEEE transactions on geoscience and remote sensing, 39(9), 1906-1915. Diederich, M., Ryzhkov, A., Simmer, C., Zhang, P., & Trömel, S. (2015). Use of Specific Attenuation
(this is not required for the UK models as they do not run a convection scheme). m s-1 [YYYYMMDD]T[hhmm]Z-PT[nnnn]H[mm]M-rainfall_rate.nc 15 Minutes (15m-126) Instantaneous rainfall rate (max in 1 hour) Maximum instantaneous rate at which rain (as a depth) which has been produced by the model
of multi-site synthetic precipitation data, Journal of Hydrology 345(3-4):121-133, DOI: 10.1016/j.jhydrol.2007.06.035. Brown, S., Boorman, P., Mcdonald, R., and Murphy, J., (2009). Supplement to: Interpretation for use of surface wind speed projections from the 11-member Met Office Regional Climate
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