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Analysis of extreme summers and prior late winter/spring conditions in central Europe

机译:欧洲中欧极端夏季及前期冬季/春季条件分析

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Drought and heat waves during summer in mid-latitudes are a serious threat to human health and agriculture and have negative impacts on the infrastructure, such as problems in energy supply. The appearance of such extreme events is expected to increase with the progress of global warming. A better understanding of the development of extremely hot and dry summers and the identification of possible precursors could help improve existing seasonal forecasts in this regard, and could possibly lead to the development of early warning methods. The development of extremely hot and dry summer seasons in central Europe is attributed to a combined effect of the dominance of anticyclonic weather regimes and soil moisture–atmosphere interactions. The atmospheric circulation largely determines the amount of solar irradiation and the amount of precipitation in an area. These two variables are themselves major factors controlling the soil moisture. Thus, solar irradiation and precipitation are used as proxies to analyse extreme sunny and dry late winter/spring and summer seasons for the period 1958–2011 in Germany and adjacent areas. For this purpose, solar irradiation data from the European Center for Medium Range Weather Forecast 40-yr and interim re-analysis dataset, as well as remote sensing data are used. Precipitation data are taken from the Global Precipitation Climatology Project. To analyse the atmospheric circulation geopotential data at 850 hPa are also taken from the European Center for Medium Range Weather Forecast 40-yr and interim re-analysis datasets. For the years in which extreme summers in terms of high solar irradiation and low precipitation are identified, the previous late winter/spring conditions of solar irradiation and precipitation in Germany and adjacent areas are analysed. Results show that if the El Ni?o–Southern Oscillation (ENSO) is not very intensely developed, extremely high solar irradiation amounts, together with extremely low precipitation amounts during late winter/spring, might serve as precursor of extremely sunny and dry summer months to be expected.
机译:在中纬度地区夏季的干旱和热浪是对人类健康和农业的严重威胁,对基础设施产生负面影响,例如能源供应中的问题。预计这种极端事件的外观随着全球变暖的进展而增加。更好地了解发展极热和干燥夏季的发展,并且鉴定可能的前体可以有助于改善这方面的现有季节性预测,并且可能导致预警方法的发展。中欧极热和干旱的夏季的发展归因于反气旋天气制度和土壤水分 - 气氛相互作用的主导地位的综合影响。大气循环在很大程度上决定了太阳照射的量和区域中的沉淀量。这两个变量本身是控制土壤湿度的主要因素。因此,太阳照射和降水用作德国和邻近地区的1958 - 2011年期间分析极端阳光和干燥的冬季/春季和夏季的代理。为此目的,使用来自欧洲的中范围天气预报40 - YR和临时重新分析数据集的太阳能照射数据,以及遥感数据。降水数据取自全球降水气候学项目。为了分析850 HPA的大气循环地球势数据,也取自欧洲中等范围天气预报40 - YR和临时再分析数据集。在鉴定了高太阳照射和低降水方面,迄今为止德国太阳照射和沉淀的前期冬季/春季条件和邻近地区的极端夏季的几年。结果表明,如果EL NI?O-Southern振荡(ENSO)不是非常强烈地开发,极高的太阳照射量,冬季/春季期间的极低降水量在一起,可作为极其阳光充足和干燥夏季的前兆预期。

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