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首页> 外文期刊>Ecosystems >Quantifying the Hydroregime of a Temporary Pool Habitat: A Modelling Approach for Ephemeral Rock Pools in SE Botswana
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Quantifying the Hydroregime of a Temporary Pool Habitat: A Modelling Approach for Ephemeral Rock Pools in SE Botswana

机译:量化临时池栖息地的水文状况:博茨瓦纳东南部临时岩池的建模方法

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Ecological and evolutionary processes in temporary rock pools operate within constraints imposed by their hydrologic regimes. These shallow pools flood when seasonal rains accumulate on impermeable substrates. Despite the ecological importance of hydrologic conditions for these ecosystems, we typically lack tools and empirical data required to understand the implications of hydrologic variability and climate change for biotic populations and communities in these habitats. In this study, we developed a hydrologic model to simulate rock pool hydrologic regimes based on rainfall, evapotranspiration, and basin geometry. The model was used to investigate long-term patterns of seasonal and inter-annual variation in hydroregime. In addition, hydrologic conditions associated with potential climate change scenarios were simulated and evaluated with respect to the biological requirements of the anostracan Branchipodopsis wolfi. The model's output for daily inundation matched with field observations with an overall accuracy of 85% and correctly estimated complete hydroperiods with an overall accuracy of 70%. Simulations indicate large variation in individual hydroperiods (76-115%) as well as in the number of hydroperiods per year (19-23%). Furthermore, this study suggests that climate change may significantly alter the rock pool hydroregime. These findings confirm the hydrologic sensitivity of these ephemeral habitats to precipitation patterns, and their potential sensitivity to future climate change. Modelling indicates that the suitability of average inundation conditions for B. wolfi deteriorates significantly under future climate predictions. High levels of spatial and temporal variation in hydrologic conditions are dominant features of these habitats and an essential consideration for understanding population and community-level ecological processes.
机译:临时岩池中的生态和演化过程在其水文状况所施加的约束下运行。当季节性降雨积聚在不可渗透的基底上时,这些浅水池就会泛滥。尽管水文条件对这些生态系统具有生态重要性,但我们通常缺乏了解水文变异性和气候变化对这些栖息地中生物种群和社区的影响所需的工具和经验数据。在这项研究中,我们开发了一个水文模型,以基于降雨,蒸散量和盆地几何学来模拟岩池水文状况。该模型用于调查水文状况季节和年际变化的长期模式。此外,针对潜在的气候变化情景相关的水文条件进行了模拟和评估,以证明其为厌食的枝状拟南芥的生物学需求。该模型的每日淹没输出与实地观测相匹配,总体精度为85%,正确估计的完整水文周期的总体精度为70%。模拟表明单个水文周期(76-115%)以及每年水文周期数(19-23%)的较大差异。此外,这项研究表明,气候变化可能会显着改变岩池的水文状况。这些发现证实了这些短暂生境对降水模式的水文敏感性,以及它们对未来气候变化的潜在敏感性。建模表明,在未来的气候预测下,平均淹没条件对沃尔夫杆菌的适宜性会大大降低。水文条件的高度时空变化是这些生境的主要特征,也是理解人口和社区级生态过程的重要考虑因素。

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