Moreover, the likely effects of climate change are not simple. Such an extended dry spell is unusual but not unprecedented. Climate change is perhaps the greatest threat facing the global water system, simply because in reality it is composed of many different threats.

This established dry soils which increased the high maximum temperatures experienced in southeast England during late July (Petch A second phase of hot weather from 23 to 27 July was associated with high pressure to the east of the United Kingdom over northern Scandinavia as shown in Figure The summer North Atlantic Oscillation (SNAO) represents the principal pattern of year‐to‐year variability in the summer climate of the north Atlantic and influences summer rainfall and air temperature across northern Europe through its association with the North Atlantic storm track (Folland An anticyclonic circulation anomaly over northern Europe during the summer was correctly predicted by Met Office long‐range forecasts (Dunstone We expect UK temperatures to be dependent on atmospheric circulation, with warmer summer temperatures, for example, when southerly winds blow across the United Kingdom. Figure The summer of 2018 in the United Kingdom was the joint hottest on record for mean temperature and regularly experienced spells of daily maximum temperatures in the low to mid‐30s Celsius. As of 3 May 2019, N$304,900,000 (around 21.2 million USD) is available and N$137,800,000 (9.6 million USD) needs to be mobilized. A drought is usually defined as an extended period of weather (usually around 3 weeks) when less than a third of the usual precipitation falls.. The Foreign Office now advises against non-essential travel to the Balearic and Canary Islands. Older people also lose their regulating abilities as they age and can quickly overheat.In the European heatwave of 2003, there were about 70,000 excess deaths attributed to the long hot spell.

drought relief interventions worth N$442,700,000 (around 30.8 million USD) to assist drought affected communities for the period of 1 April 2019 until end of March 2020 (or until the budget is depleted). It is only when all the evidence is brought together in an integrated way that we can provide a more comprehensive picture. Montpellier melts under a 45C high as Europe hit by record heatwaveSpain battles biggest wildfires in 20 years as heatwave grips EuropeFrance records all-time highest temperature of 45.9CEurope heatwave: cities take steps to limit effects of record temperatures'Hell is coming': week-long heatwave begins across EuropeEurope heatwave: record high of 45C expected in FranceContinental Europe braced for 'potentially dangerous' heatwave Book bringing drought research to children wins national award – DRY: Diary of a Water Superhero Top author turns research into a story for Hay Festival About Drought held up as an exemplar of research that has revolutionised the way the UK manages drought and water scarcity

The vertical red lines indicate the equivalent temperature anomaly for summer 2018. Recent research by Dunstone Most of the anomalies in the UK mean temperature of summer 2018 can be explained based on circulation, accounting for elevated SSTs in the coastal waters of the United Kingdom, as well as other feedbacks such as extremely low soil moisture following an extended dry spell through June and July. The most recent set of probabilistic projections from the UK Climate projections (UKCP18) give a wider but overlapping range of 10–25% for the current climate and a likelihood greater than 50% of summers exceeding 2018 temperatures by the mid‐twenty‐first century.Summer 2018 was the joint hottest summer season (June, July, August) in the Met Office UK national temperature series dating from 1884 (HadUK‐Grid version 1 dataset, Hollis High temperatures were not confined to the meteorological summer season in 2018. ... accompanied by a drought in many areas. )Northern European summer rainfall (left) and temperature (right) as standardised anomalies from observations (black) and the DePreSys3 (red) seasonal forecast system. A positive phase of the SNAO with a northward‐shifted jet stream resulted in anticyclonic conditions dominating across western Europe and the United Kingdom. While warm weather at the right time is crucial for many crops during their growing periods, excessively high temperatures can inhibit growth, particularly if they are prolonged.

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