Page 12 of 276
Did you mean banbury's s s s s s s?
(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
Nuclear Power Plant Accident - Annex III, 4 February 2013 Draxler, R., Arnold, D., Chino, M., Galmarini, S., Hort, M., Jones, A., … Wotawa, G. (2015). World Meteorological Organization’s model simulations of the radionuclide dispersion and deposition from the Fukushima Daiichi nuclear power plant
-35.625 o W, 3.75 o S-8.75 o S and is marked by the blue rectangle in Figure 1. Quintile category forecasts have been issued for this (or a very similar) region since 1987. Forecast probabilities for quintile categories of mean rainfall for SNEBR are shown in the table below. The near-normal and above
) on initiation. Can we perturb the soil moisture in a realistic way in some case(s) to investigate this? Analysis of climate runs inc. UKCP 2.2km ensemble, 2.2km over Europe and 4.5km over Africa. Event composites for different weather regimes. Analyse profiles of events and rainfall distributions
, 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
, GIC, etc. (29ea.) Aviation Power SWx Operations – observation network GIC Monitor (x3) TEC & Scintillation Monitor (x5) Singapyung Sintaebaek Daejeon Gwangju Dongjeju SWx Operations – satellite tracking facilities ‣ACE Tracking Antenna � global tracking network for RTSW � 13-meter dish antenna (S
the period 1996-2009. 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 Simulator
this signal has a particularly large spatial extent and a magnitude of >1.6 hPa s �1 in the ensemble mean by the 2080s/2090s. In north central Sahel both ensembles show smaller upward anomalies (approximately 0.8 hPa s �1 ) corresponding to the wet signal in Figure 1. These changes are amplified
, Institut Pierre Simon Laplace (IPSL) S. Flavoni: Sorbonne Universités, LOCEAN Laboratory, Institut Pierre Simon Laplace (IPSL) L. Hermanson: Met Office Hadley Centre N. Keenlyside: University of Bergen and Bjerknes Centre for Climate Research, Nansen Environmental and Remote Sensing Center
Climatic Change (2013) 120:965–975 DOI 10.1007/s10584-013-0831-3 LETTER Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) L. O. Mearns & S. Sain & L. R. Leung & M. S. Bukovsky & S. McGinnis & S. Biner & D. Caya & R. W. Arritt & W. Gutowski & E
Previous