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FUTURE CHANGES IN THE OCCURRENCE OF EXTREME PRECIPITATION EVENTS IN EASTERN MEDITERRANEAN

机译:东地中海东部地区极端降水事件发生的未来变化

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It is widely known that precipitation extreme events can generate great impact on human activities and natural environment. Therefore, the analysis of extreme precipitation events in the present and future climate is of great importance. For Eastern Mediterranean, recent studies have shown an increasing tendency of the dry spell length during the last two decades while appears one of the most sensitive areas regarding the future precipitation extreme conditions. Therefore, further work is required in order to understand the distribution and causes of precipitation extremes in Eastern Mediterranean and be able to get general conclusions about their future occurrence and impact. The aim of this study is to estimate future potential changes in duration of extreme dry and wet spells and rainfall intensity in Eastern Mediterranean. For this purpose, daily precipitation amounts, as derived from the regional climate model of the UK Hadley Centre HadRM3P have been used for the present period 1960-1990 (control run) and the future period 2070-2100. The data are available on 0.44°x 0.44° latitude by longitude grid through the European project MICE (Modelling Impacts of Climate Extremes). Future data are based on the B2a IPCC emission scenario. For the identification of the precipitation extremes three climatic indices were employed: a) CWD (Maximum number of consecutive wet days), b) CDD (Maximum number of consecutive dry days) and c) SDII (quotient of precipitation amount of wet days and the number of wet days of the specified period). The indices were calculated for the present and future period, on a seasonal and annual basis. The validation of model results (control run) against the station data for the present period demonstrated that the two datasets agree quite well. Then, our analysis has shown a general tendency towards longer dry spells in all seasons, except autumn. In addition, extreme wet spells are shortened in the future during all seasons, except autumn where their length is increasing at almost all sites. Similarly, precipitation intensity found reduced for all seasons. However, the uncertainties in the future response of climate and its variability still remain, implying that these results should be handled with caution and further work must be conducted.
机译:众所周知,降水极端事件可能会对人类活动和自然环境产生很大影响。因此,在现在和未来的气候中对极端降水事件的分析具有重要意义。对于东地中海而言,最近的研究表明在过去二十年中的干法长度的趋势越来越大,而出现有关未来降水极端条件的最敏感的地区之一。因此,需要进一步的工作,以了解地中海东部降水极端的分布和原因,并能够获得对其未来的发生和影响的一般性结论。本研究的目的是估计东部地中海东部地区极端干湿法术和降雨强度的未来潜在变化。为此目的,从英国Hadley中心Hadrm3p的区域气候模型中衍生的每日降水量已被用于本期1960 - 1990年(控制运行)和未来2070-2100期间。通过欧洲项目小鼠(气候极端的建模影响),通过经度网格获得0.44°x 0.44°纬度。未来数据基于B2A IPCC发射方案。为了鉴定沉淀极端,使用三气候索引:a)CWD(连续最大潮湿的日子),b)CDD(连续干燥天数)和C)SDII(潮湿的沉淀量的商量)指定期间的潮湿天数)。以季节性和年度为基础为目前和未来期间计算指数。对当前期间的站数据进行模型结果(控制运行)的验证表明,两个数据集非常完全同意。然后,除了秋天,我们的分析显示了所有季节中较长的干燥法术趋势。此外,在所有季节期间,将来的季节缩短了极端湿法,除了几乎所有地点的长度在秋天越来越多的秋季。同样,为所有季节降低降水强度。但是,将来的气候响应和变异性仍然存在不确定性仍然存在,这意味着这些结果应谨慎处理,必须进行进一步的工作。

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