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- 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

considered as a liquid water equivalent (LWE) value. It includes the contribution from the model convection scheme if this is invoked. m s-1 n/a None n/a Hourly T+0 to T+132 3-hourly T+135 to T+246 pressure_at_convective_cloud_base Air pressure at the base of the lowest convective cloud

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

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

(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

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

, 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

, purchase or otherwise provide, and maintain instrumentation to obtain measurements 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