14 November 2019.
It is the second time in three years that a state of emergency has been declared because of drought. Twenty‐four counties in the southeast have a threshold of 27°C, and a belt of 12 counties has a threshold of 26°C. Much of England and Wales received less than 65% of average rainfall from May 1975 to August 1976, with some parts of southern England receiving less than 55%. The UK Droughts & Water Scarcity research programme is a five-year interdisciplinary, £12 million+ NERC programme in collaboration with ESRC, EPSRC, BBSRC and AHRC. Climate change is perhaps the greatest threat facing the global water system, simply because in reality it is composed of many different threats. For example, heavy rain and cloudy weather across swathes of northern Europe, including the UK, are likely to become more common as a result of the buildup of carbon dioxide in the atmosphere causing the jet stream weather system to become fixed in position.However, this year’s weather is certainly in line with the predictions scientists have made of rising temperatures, more heatwaves and prolonged droughts interspersed with periods of heavy flooding in some areas.Heatwaves can have pleasant effects, with long sunny days encouraging people into parks and on to beaches, and they certainly bring a smile to the faces of ice-cream sellers.However, the body’s ability to regulate its own temperature is crucial; babies are less well able to regulate their temperature and must be kept in well-ventilated conditions. Livestock can also suffer in the heat and need extra care.Finally, one of the ironies of the climate emergency is that hot weather encourages greater use of air conditioning, which was cited recently by BP as a key factor in raising greenhouse gas emissions last year.But as Greenpeace has pointed out, the deaths in Europe are of a relatively small number compared with the “far bigger disasters already occurring in hotter, poorer countries in the global South”. We thank two anonymous reviewers for constructive feedback that improved the manuscript.Please check your email for instructions on resetting your password. By continuing to browse this site, you agree to its use of cookies as described in our Time Series Analysis in Meteorology and Climatology: An IntroductionThe Atmosphere and Ocean: A Physical Introduction, 3rd EditionQuarterly Journal of Royal Meteorological Society Special CollectionsI have read and accept the Wiley Online Library Terms and Conditions of UseDifferent ways of framing event attribution questions: the example of warm and wet winters in the United Kingdom similar to 2015/16A new HadGEM3‐A based system for attribution of weather and climate‐related extreme eventsForced and internal components of winter air temperature trends over North America during the past 50 Years: mechanisms and implicationsPredictability and drivers of the 2018 dry European SummerSkilful seasonal predictions of summer European rainfallThe summer North Atlantic oscillation: past, present, and futureProbabilistic projections of transient climate changeHadUK‐Grid – A new UK dataset of gridded climate observationsExtreme weather events in early summer 2018 connected by a recurrent hemispheric wave‐7 patternQuarterly mortality report, England: July to September 2018The dynamical influence of the Atlantic multidecadal oscillation on continental climateGlobal analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth centuryMultivariate prediction using imperfect climate models part I: outline of methodologyAttribution of extreme weather and climate‐related eventsHigh risk of unprecedented UK rainfall in the current climateRCP4.5: a pathway for stabilization of radiative forcing by 2100. However, the synoptic situation in the summer did not result in an extended spell of southerly or southeasterly air masses over the United Kingdom that would tend to result in an extended spell of exceptionally high temperature, such as that experienced in the summers of 1976, 1995, 2003, 2006 and 2019.
The polar region is heating more rapidly, reducing the temperature difference with lower latitudes. 27 July 2020. Drought is defined as a moisture deficit bad enough to have social, environmental or economic effects.
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