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首页> 外文期刊>Hydrological Processes >Characterization of sudden and sustained base flow jump hydrologic behaviour in the humid seasonal tropics of the Panama Canal Watershed
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Characterization of sudden and sustained base flow jump hydrologic behaviour in the humid seasonal tropics of the Panama Canal Watershed

机译:巴拿马运河流域湿润的季节性热带地区突发性和持续性基流跳跃水文行为的特征

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摘要

Base flows are important for tropical regions with pronounced dry seasons, which are facing increasing water demands. Base flow generation, however, is one of the most challenging hydrological processes to characterize in the tropics. In many years during the May-December wet season in the Panama Canal Watershed (PCW), base flows in rivers abruptly increase. This increase persists until the start of the December-April dry season. Understanding this unusual base flow jump (BFJ) behaviour is critical to improve water provisioning in the seasonal tropics, especially during droughts and extended dry seasons. This study developed an integrated approach combining piecewise regression on cumulative average base flow and sensitivity analysis to calculate the timing and magnitude of BFJ. Rainfall, forest cover, mean land surface slope, catchment area, and estimated subsurface storage were tested as predictors for the occurrence and magnitude of the BFJs in seven subcatchments of the PCW. Sensitivity analysis on correlated predictors allowed ranking of predictor contributions due to isolated and cross-correlation effects. Correlations between observed BFJs and BFJs predicted by watershed and rainfall-related predictors were 0.92 and 0.65 for BFJ timing and magnitude, respectively. Forest cover was the second most significant predictor after cumulative rainfall for jump magnitude, owing to larger subsurface storage and groundwater recharge in forests than pastures. Catchments in the mountainous eastern PCW always generated larger jumps due to their higher rainfall and greater forest cover than the western PCW catchments. The cross-correlations between predictors contributed to more than 50% of the jump variances. The results demonstrate the importance of rainfall gradient and catchment characteristics in affecting the sudden and sustained BFJs, which can help inform land management decisions intended to enhance water supplies in the tropics. This study underscores the need for more research to further understand the hydrological processes involved in the BFJ phenomenon, including better BFJ models and field characterizations, to help improve tropical ecosystem services under a changing environment.
机译:基流对于干旱季节明显的热带地区非常重要,这些地区面临着不断增长的需水量。然而,基流产生是热带地区最具挑战性的水文过程之一。在5月至12月的巴拿马运河集水区(PCW)的雨季期间的许多年中,河流的底流量突然增加。这种增加一直持续到12月至4月旱季开始。了解这种异常的基流跳变(BFJ)行为对于改善热带地区的水供应至关重要,特别是在干旱和干旱季节。这项研究开发了一种综合方法,该方法结合了基于累积平均基本流量的分段回归和灵敏度分析来计算BFJ的时间和大小。测试了降雨,森林覆盖率,平均地表坡度,集水面积和估计的地下蓄水量,作为PCW七个子集水区BFJ发生和强度的预测指标。对相关预测变量的敏感性分析允许对由于分离和互相关效应而产生的预测变量贡献进行排名。流域和降雨相关预报器预测的观测到的BFJ和BFJ之间的相关性对于BFJ时机和震级分别为0.92和0.65。森林覆盖率是累积降雨之后跃升幅度第二大的预测因子,这是由于森林中的地下存储量和地下水补给量大于牧场。东部PCW山区的集水区总是比西部PCW集水区产生更大的跃迁,这是因为它们的降雨量更高且森林覆盖率更高。预测变量之间的互相关贡献了超过50%的跳跃差异。结果表明降雨梯度和集水特征对影响突发性和持续性BFJ的重要性,这可以帮助指导旨在加强热带地区水供应的土地管理决策。这项研究强调需要更多的研究来进一步了解BFJ现象所涉及的水文过程,包括更好的BFJ模型和田野特征,以帮助改善环境变化中的热带生态系统服务。

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