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首页> 外文期刊>Journal of hydrometeorology >Fog Water Collection in a Subtropical Elfin Laurel Forest of the Garajonay National Park (Canary Islands): A Combined Approach Using Artificial Fog Catchers and a Physically Based Impaction Model
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Fog Water Collection in a Subtropical Elfin Laurel Forest of the Garajonay National Park (Canary Islands): A Combined Approach Using Artificial Fog Catchers and a Physically Based Impaction Model

机译:Garajonay国家公园(加那利群岛)的亚热带Elfin月桂树森林中的雾水收集:使用人工雾化捕手和基于物理的撞击模型的组合方法

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Fog precipitation has long been assumed as an additional water source in the relic laurel ecosystems of the Canary Islands, located at 500-1400 m MSL. However, to what extent fog water can contribute to the laurel forest water balance is not yet clear. Combining data from artificial fog catchers and a physically based impaction model, the authors evaluated the potential contribution of fog water captured by needle-leafed Erica arborea L. trees in a selected watershed of the Garajonay National Park (La Gomera Island) for a 2-yr period (February 2003-January 2005). Fog water collection was measured with artificial catchers at four micrometeorological stations placed at 1145, 1185, 1230, and 1270 m MSL. Average fog water collection was only significant at the highest measurement site (one order of magnitude greater than at lower altitudes), totaling 496 L m(-2) yr(-1) during the 2-yr period. The average fog water yield in the first and second annual periods ranged between 0.2-5.0 and 0.1-2.1 L m(-2) day(-1), respectively. Rainfall exhibited seasonality, distinguishing between rainy and dry seasons, while fog water collection was distributed more evenly throughout the year. Regarding fog water captured by the vegetation, the impaction model predicted a significant amount of fog water potentially collected by a single E. arborea tree, on the order of 1810-2090 L yr(-1). Taking tree population density into account, the yearly average water contribution to the soil surface by wind-driven fogs was 251-281 mm, whereas annual rainfall was 635 and 1088 mm, respectively. The hourly course of micrometeorological variables shows a 58% reduction in global radiation under foggy conditions and a concomitant 3 degrees-6 degrees C mean temperature decrease compared to fog-free periods. Thus, limiting evapotranspiration may also be a relevant effect of fog in this subtropical elfin cloud forest.
机译:长期以来,人们一直认为雾霾是加纳利群岛MSL 500-1400 m遗迹月桂树生态系统中的额外水源。然而,雾水在多大程度上有助于月桂树森林水平衡尚不清楚。结合人工除雾器的数据和基于物理的撞击模型,作者评估了在Garajonay国家公园(戈梅拉岛)选定流域中,针叶艾里卡arborea L.树木捕获的雾水的潜在贡献,其中2-年(2003年2月至2005年1月)。在四个微气象站(分别位于1145、1185、1230和1270 m MSL),用人工捕集器测量了雾水的收集量。平均雾水收集量仅在最高测量点处有意义(比低海拔处高一个数量级),在2年期间总计496 L m(-2)yr(-1)。第一年和第二年的平均雾水产量分别在0.2-5.0和0.1-2.1 L m(-2)day(-1)之间。降雨表现出季节性,区分雨季和旱季,而全年的雾水收集更为平均。关于植被捕获的雾水,影响模型预测单个树栖乔木(E. arborea)树木可能收集的大量雾水,约为1810-2090 L yr(-1)。考虑到树木的密度,风雾对土壤表层的年平均水分贡献为251-281 mm,而年降雨量分别为635和1088 mm。与无雾时期相比,微气象变量的每小时变化过程表明,在有雾条件下,全球辐射减少了58%,随之而来的是平均气温下降了3度至6摄氏度。因此,限制蒸散量也可能是该亚热带小精灵云雾林中雾的相关影响。

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