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Ten years water and energy surface balance from the CNR-ISAC micrometeorological station in Salento peninsula (southern Italy)

机译:萨伦托半岛(意大利南部)的CNR-ISAC微气象站实现了十年的水和能源表面平衡

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Data of surface-atmosphere energy and water transfer from a ten years(2003–2013) period of activity of the ISAC-Lecce micrometeorological station(href="http://www.basesperimentale.le.isac.cnr.it"target="_blank">http://www.basesperimentale.le.isac.cnr.it) have been analyzed: tothe authors' knowledge this is the first decadal data set ofsurface-atmosphere transfer in Salento peninsula. The surface energy budgetshows a tendency to a positive bias possibly due to several reasons thatrequire more investigations. Some suitable indices related to the surfacewater balance, such as the precipitation intensity, the aridity index andthe ground water infiltration fraction have been calculated. Possible trendsof these annual averages in the decadal period are considered, also takinginto account the statistical uncertainty associated to measurement errorsand missing data. The results indicate a significant increasing in theprecipitation intensity together with an experimental evidence of increasingof the ground water infiltration in the measurement area, that is inagreement with recent estimations for the whole Salento peninsula. On theother hand, recent studies show that seawater intrusion and salinization ofthe deep underground aquifer keep increasing in the same period.
机译:ISAC-Lecce微气象站活动十年(2003-2013)期间的地表大气能量和水转移数据(href =“ http://www.basesperimentale.le.isac.cnr.it”已经对target =“ _blank”> http://www.basesperimentale.le.isac.cnr.it 进行了分析:据作者所知,这是Salento半岛第一个年代际大气交换年代际数据集。表面能预算显示出正偏向的趋势,这可能是由于需要更多研究的几个原因所致。计算了一些与地表水平衡有关的指标,如降水强度,干旱指数和地下水入渗率。考虑了这些十年平均值的年度趋势,还考虑了与测量误差和数据丢失相关的统计不确定性。结果表明,降水强度显着增加,同时实验证据表明测量区域的地下水渗透增加,这与整个Salento半岛的最新估计相吻合。另一方面,最近的研究表明,在同一时期,深层地下含水层的海水入侵和盐碱化持续增加。

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