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Securing Biodiversity in Breckland - European Commission

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Mean m<strong>in</strong>imum daily air temperature (°C)YearFigure 18. Mean daily m<strong>in</strong>imum air temperature between 1949 and 2008 (n=60) at Santon Downhamweather stations <strong>in</strong> spr<strong>in</strong>g (+), summer (x), autumn (○) and w<strong>in</strong>ter (∆). Details of relationships between yearand air temperature are given <strong>in</strong> Table 17.Predicted Future Climatic Change <strong>in</strong> the <strong>Breckland</strong> RegionClimate changes <strong>in</strong> the East of England have been modelled by the UK Climate Predictions (UKCP09)based on various scenarios of emissions of greenhouse gases (Murphy et al. 2009)By the 2050s and under medium emissions scenario, the East of England is predicted to experience: Hotter summers. Summer mean temperatures are predicted to <strong>in</strong>crease by 2.5 °C with an<strong>in</strong>crease of 3.4°C <strong>in</strong> summer mean daily maximum temperatureDrier summers. Mean summer precipitation is predicted to decrease by 17% <strong>in</strong> summer meanprecipitation Milder w<strong>in</strong>ters. W<strong>in</strong>ter mean temperatures are predicted to <strong>in</strong>crease by 2.2 °C Wetter w<strong>in</strong>ters. W<strong>in</strong>ter mean precipitation is predicted to rise by 14%.The values given above are central estimates; more details of probabilities and climate changes areavailable at http://ukclimateprojections.defra.gov.uk.The UK Climate Impact Programme (UKCIP02) also predicted a significant decrease <strong>in</strong> soil moisturecontent.96

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