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Elucidating the climate and topographic controls on stable isotope composition of meteoric waters in Morocco, using station-based and spatially-interpolated data

机译:使用基于站和空间插值的数据,阐明摩洛哥陨石水稳定同位素组成的气候和地形控制

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Understanding the main controls on stable isotope variations in precipitation is fundamental for the interpretation of the hydrological cycle. However, spatio-temporal variations in delta O-18(p) are poorly known in Morocco. Herein, we explore the relative influence of meteorological variables, spatial and orographic (attitudinal) effects, atmospheric circulation and moisture sources on precipitation stable isotopes in Morocco. Precipitation events and two-years-long monthly records from 17 rain-gauge stations in Morocco are investigated and compared in this study to global gridded records of monthly and annual stable isotopes in precipitation. We highlight that the main spatial controls on precipitation stable isotopes are the topography and the distance from marine source. The most depleted mean annual isotopes are located in the High Atlas Mountains (delta O-18(p) = -9.56 parts per thousand and delta H-2(p) = -59.3 parts per thousand), while the most enriched isotope ratios exist in southwestern Morocco (delta O-18(p) = -2.35 parts per thousand and delta H-2(p) = -7.47 parts per thousand). The well-constrained relationship between delta O-18(p) and altitude describes a gradient of 0.11-0.18 parts per thousand, per 100 m. The seasonal variation is expressed by a general enrichment that reaches -4.8 parts per thousand during the dry season, related to the recycled vapor contained within the summer precipitation. Notwithstanding the scarcity of temperature and precipitation measurements, the amount effect is observed in multiple stations during several rain events and precipitation seems to have more influence on delta O-18(p) than temperature. Backward moisture trajectories indicate a distinct depletion in delta O-18(p) in extreme events originating from the Atlantic Ocean. The presence of a rain shadow effect is also revealed on the lee side of High Atlas Mountains, southeastern Morocco. (C) 2016 Elsevier B.V. All rights reserved.
机译:理解降水中稳定同位素变化的主要控制因素是解释水文循环的基础。但是,摩洛哥对O-18(p)的时空变化知之甚少。在这里,我们探讨了摩洛哥气象变量,空间和地形(垂直)效应,大气环流和水分源对降水稳定同位素的相对影响。调查了摩洛哥17个雨量计站的降水事件和为期两年的月度记录,并将其与全球每月和每年的稳定同位素降水栅格化记录进行了比较。我们着重指出,降水稳定同位素的主要空间控制是地形和距海洋源的距离。年度平均同位素最耗竭的地区是高阿特拉斯山脉(δO-18(p)= -9.56千分之几和δH-2(p)= -59.3千分之几),而最富集的同位素比率存在在摩洛哥西南部(δO-18(p)= -2.35千分之几和δH-2(p)= -7.47千分之几)。高度O-18(p)与海拔高度之间的约束关系很好,描述了每100 m千分之0.11-0.18的梯度。季节性变化以干燥季节达到-4.8千分之总富集来表示,这与夏季降水中所含的再循环蒸气有关。尽管缺乏温度和降水量的测量,但在几次降雨事件中,在多个观测站都观测到了数量效应,降水量似乎比温度对O-18(p)的影响更大。向后的水分运动轨迹表明,在源自大西洋的极端事件中,δO-18(p)明显减少。在摩洛哥东南部的阿特拉斯山脉的后风侧也发现有雨影效应。 (C)2016 Elsevier B.V.保留所有权利。

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