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A wavelet perspective on variabilities of hydrological processes in conjunction with geomorphic analysis over the Pearl River basin in South China

机译:中国南方珠江流域水文过程变异的小波分析与地貌分析

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Basin response to precipitation variability by terrestrial hydrological processes may be manifested at different timescales and vary from one basin to another. A quantitative grasp of natural variability modulation is desirable for characterizing basin tendency or vulnerability on floods and droughts; quantification is not always straightforward, however. Using a macro-scale hydrological model, the Variable Infiltration Capacity (VIC) model, the hydrological time series (runoff, soil moisture, and evapotranspiration) were obtained for the 10 sub-basins over the Pearl River basin in South China for the period 1952-2000. A continuous wavelet transform was used to identify the characteristics of the temporal scales of basin-featured extreme events and related multiple-scale variabilities. By use of wavelet coherence analysis and rank correlation method, the cross correlations of monthly anomalies of hydrological processes were examined. The results showed that the runoff correlated most with, and the evapotranspiration had less response to, the precipitation variability. The analyzed results revealed that the attenuation effect of runoff in response to precipitation variability was mainly within the timescale of 2 yr in the Pearl River basin. The soil moisture variability can extend precipitation variation along with time scales. With understanding of the variability features of the terrestrial hydrological processes, this paper showed one geomorphic index, a basin form factor (FF), can represent the wavelet-based indices for high- and low-frequency responses to precipitation variability. It was found that, for a sub-basin with a higher FF value, precipitation variability can be represented more by runoff variability at less than 2-yr time scales; such a sub-basin is apt to have serious floods. With a lower FF value, a sub-basin has longer memory of soil moisture, leading to severe droughts during dry periods. This finding would be valuable to evaluate the tendency on occurrence of floods and droughts in the Pearl River basin, a humid region, which may be transferable to other basins in the globe. (C) 2016 Elsevier B.V. All rights reserved.
机译:流域对地面水文过程对降水变化的响应可能在不同的时间尺度上表现出来,并且在一个流域到另一个流域之间都不同。需要定量掌握自然变异性,以表征流域干旱或干旱趋势或脆弱性;但是,量化并不总是那么简单。利用宏观水文模型,可变入渗能力(VIC)模型,获得了中国南方珠江流域1952年期间10个子流域的水文时间序列(径流,土壤湿度和蒸散量) -2000。连续小波变换用于识别盆地特征性极端事件的时间尺度特征和相关的多尺度变化。利用小波相关分析和秩相关法,研究了水文过程月度异常的互相关性。结果表明,径流与降水变化最相关,而蒸散对降水变化的响应较小。分析结果表明,珠江流域径流对降水变化的衰减效应主要在2年以内。土壤湿度的变化可以随着时间尺度扩展降水变化。在了解了地面水文过程的变异性特征后,本文显示了一个地貌指数,即盆地形状因子(FF),可以代表基于小波的降水和低频响应指数。研究发现,对于一个FF值较高的子流域,降水变异性可以用少于2年的时间尺度上的径流变异性来表示。这样的一个流域容易遭受严重的洪灾。 FF值较低时,子流域对土壤水分的记忆时间更长,导致干旱时期严重干旱。这一发现对于评估珠江流域(一个潮湿的地区)发生水灾和干旱的趋势将是有价值的,珠江流域可能会转移到全球其他流域。 (C)2016 Elsevier B.V.保留所有权利。

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