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Recent trends in sediment load of the tropical (Peninsular) river basins of India

机译:印度热带(半岛)河流域沉积物负荷的最新趋势

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The tropical river basins of India are important because of the coastal ecosystem that they sustain and the densely populated economic zones that they serve. This study examines the recent trends in sediment load and also explores the influence of the climatic and human forcing mechanisms on the land-ocean fluvial systems. A large dataset comprised of the sediment time series of different timescale during the period 1986-87 to 2005-06 from 133 gauging stations spreading across tropical river basins of India was analyzed. Results indicate dramatic reductions in sediment load in the tropical river basins, which is beyond the fold of assignable natural variability. Around 88% (62%) of the total 133 gauging stations showed decline in sediment loads in the monsoon (non-monsoon) season. The significant downward trends outnumbered the corresponding upward trends in high proportions for both the seasons. Striking spatial coherence was observed among the significant trends, suggesting the presence of the cross-correlation among the sediment records. The regional trends, which account the spatial correlation, also indicated the widespread nature of the sediment declines. The rainfall, which is characterized by the non-significant decreasing trends and also frequent drought years, is the primary controller of the sediment loads for most of the river basins. It may be inferred that a little change in rainfall towards the deficit side leads to a significant reduction in sediment load. This is due to the diversion and storage of runoff to meet the manifold increases in water requirements for the agriculture and industry. Among the tropical rivers, the maximum reduction in sediment flux has taken place for the Normada River (-2.07 x 10~6 t/yr) due to the construction of dam. Although the sea level is rising, we speculate that the significant reduction in sediment loads may also have influenced the coastal erosion in recent years. The results of this study can be utilized for the sustainable management of the tropical river basins in the backdrop of a predicted erratic monsoon rainfall and the growing anthropogenic stresses.
机译:印度的热带流域之所以重要,是因为它们维持着沿海生态系统以及它们所服务的人口稠密的经济区。这项研究调查了沉积物负荷的最新趋势,并探讨了气候和人类强迫机制对陆地-海洋河流系统的影响。分析了一个大型数据集,该数据集由分布在印度热带河流域的133个测量站在1986-87年至2005-06年期间的不同时间尺度的沉积物时间序列组成。结果表明,热带河流域的泥沙负荷显着减少,这超出了可分配的自然变异性的范围。在总共133个测量站中,约有88%(62%)在季风(非季风)季节沉积物负荷下降。在两个季节中,显着的下降趋势超过了相应比例的上升趋势。在显着趋势之间观察到惊人的空间连贯性,表明沉积物记录之间存在互相关。考虑到空间相关性的区域趋势也表明了沉积物下降的广泛性质。降雨的特点是下降趋势不显着,而且干旱频繁,是大多数流域沉积物负荷的主要控制者。可以推断,降雨向赤字侧的微小变化会导致泥沙量的显着减少。这是由于径流的转移和存储,以满足农业和工业对水的大量需求。在热带河流中,由于修建了大坝,诺玛达河的沉积物通量最大程度减少(-2.07 x 10〜6 t / yr)。尽管海平面上升,但我们推测,近年来泥沙量的大幅减少也可能影响了海岸侵蚀。在预测的季风降雨不稳定和人为压力不断增加的背景下,本研究的结果可用于热带流域的可持续管理。

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