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UKCP Case Study: Climate Change Impacts on Peak River Flows Authors: A.L. Kay 1 , A.C. Rudd 1 , M. Fry 1 , G. Nash 2 & S. Allen 3 1. UK Centre for Ecology & Hydrology (Wallingford) 2. UK Centre for Ecology & Hydrology (Edinburgh) 3. Environment Agency, UK Year of Production: 2021 Target Audience
, 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
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
Circulation Response to CO2 Forcing, Journal of Climate, DOI: 10.1175/JCLI-D-17-0323.1. Gohar G, Bernie D, Good P and Lowe JA, 2018. UKCP18 Derived Projections of Future Climate over the UK, Met Office. Lowe JA, Howard TP, Pardaens A, Tinker J, Holt J, Wakelin S, Milne G, Leake J, Wolf J, Horsburgh
) 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
-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
, 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
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
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