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six days ahead and red warnings closer to the event. Pre-emptive actions were reported on the rail network, including the closure of the East Coast Main Line between London and York on the 19th. Impacts to travel, particularly rail services, began to be reported more widely with speed restrictions
Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (Solomon et al). Cambridge University Press, Cambridge, United Kingdom and New York, NY, 93-217 IPCC, (2000): IPCC Special report: Emissions’ Scenarios, summary to policy makers: A special report of IPCC working
Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 1535 pp. IPCC, 2021: Summary for Policymakers. In: Climate Change 2021: The Physical
bulb for 3 months. • A typical flash of forked lightning lasts for about 0.2 seconds. • The temperature of lightning’s return stroke can reach 28,000°C. • Lightning does strike twice; the Empire State Building in New York has been struck by lightning as much as 48 times in one day, but they have
to 21st It grew colder over the next few days, with a lot of cloud. Eastern areas and the Vale of York had fog clearing to sunshine on the 16th, other areas staying cloudy, with patchy drizzly rain in a few spots. The 17th began frosty and foggy in parts of the north and east on the 17th, with some
/gritting-routes-bins/ Stockton-on-Tees Borough Council Stoke-on-Trent City Council Swindon Borough Council Telford & Wrekin Borough Council Thurrock Council Warrington Borough Council West Berkshire Council Wiltshire Council Windsor & Maidenhead Borough Council Wokingham Borough Council City of York
. After early fog for the Vale of York and parts of the east coast on the 4th, showers across many areas became progressively heavier and more frequent through the day, with thunderstorms over northern counties during the afternoon. Rain or showers affected northern and eastern areas early on the 5th
. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 1535 pp, doi:10.1017/CBO9781107415324. Knapp, K. R., M. C. Kruk, D. H. Levinson, H. J. Diamond, and C. J. Neumann, 2010: The International Best Track
, A. Nauels, Y. Xia, V. Bex, and P. Midgley, Eds., Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, URL Availableathttp://www.climatechange2013.org/, accessed 2018-03-08. Davie, J., E. Pope, and C. Kent, 2019: D2.1: Relationships between large-scale modes of natural climate
of the Intergovernmental Panel on Climate Change. http://dx.doi.org/10.1016/j.renene.2009.11.012, Cambridge, UK. and New York, NY. Honti, M., Scheidegger, A., Stamm, C., 2014. The importance of hydrological uncertainty assessment methods in climate change impact studies. Hydrol. Earth Syst. Sci. 18, 3301
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