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首页> 外文期刊>Science of the total environment >Impact of global-scale hydroclimatic patterns on surface water-groundwater interactions in the climatically vulnerable Ganges river delta of the Sundarbans
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Impact of global-scale hydroclimatic patterns on surface water-groundwater interactions in the climatically vulnerable Ganges river delta of the Sundarbans

机译:全球型水皮模式对孙德巴人气候脆弱河三角洲地表水土水域互动的影响

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摘要

The global climate patterns like El Nino Southern Oscillation (ENSO) cycle and Indian Ocean Dipole (IOD) have impacts on surface water quality and groundwater recharge patterns. But the ENSO and IOD impacts on surface water-groundwater (SW-GW) interaction in terms of quality have not been studied. Therefore, the present study was conducted to delineate the impacts of ENSO and IOD on the SW-GW interaction process-induced groundwater quality of coastal aquifers of Sundarbans, by the application of isotopic signature, salinity content of ground-water and seawater in relation to rainfall variability. Study results revealed that the declining trend of rainfall potentially increases the seawater salinity. The rainfall pattern also positively correlates with the groundwater level (GWL) at a 5% level of significance observed from the wavelet analysis. The deficit in rainfall due to the El Nino is the possible reason for the declining GWL, which is giving rise to groundwater salinity. El Nino also affected the nearshore seawater salinity which was increased from 19 to 24 ppT. The study provides a surrogate understanding of the potential impact of El Nino in one of the most climatically vulnerable parts of the planet, while IOD impacts are not conclusive. In the scenario of depleted rainfall amount, groundwater abstraction practices need to be managed, otherwise, it could create a potential threat to the available drinking water resources in the present and future climate change scenarios.
机译:全球气候模式,如El Nino Southern振荡(ENSO)循环和印度洋偶极子(IOD)对地表水质和地下水充电模式产生了影响。但尚未研究对地面水地水域(SW-GW)相互作用的ENSO和IOD的影响。因此,通过应用同位素签名,地下水和海水的盐度含量,对本研究进行了解恩索和IOD对Sun-GW相互作用过程诱导的沿海含水层的沿海含水层的地下水质量。降雨变异性。研究结果表明,降雨趋势趋势可能会增加海水盐度。从小波分析中观察到的5%显着性的地下水位(GWL)也与地下水位(GWL)呈正相关。由于El Nino导致的降雨赤字是GWL下降的可能性,这导致地下水盐度。 El Nino也影响了近岸海水盐度,从19升增加到24个PPT。该研究提供了对厄尔尼诺在地球最受欢迎的脆弱部位之一的潜在影响的替代理解,而IOD的影响则不会得出决定性。在耗尽的降雨量的情况下,需要管理地下水抽象实践,否则,它可能会对当前和未来的气候变化情景中的可用饮用水资源产生潜在的威胁。

著录项

  • 来源
    《Science of the total environment》 |2021年第1期|149198.1-149198.10|共10页
  • 作者单位

    School of Environmental Science and Engineering Indian Institute of Technology Kharagpur 721 302 India;

    School of Environmental Science and Engineering Indian Institute of Technology Kharagpur 721 302 India Geology and Geophysics Indian Institute of Technology Kharagpur 721 302 India Applied Policy Advisory to Hydrogeosciences Group Indian Institute of Technology Kharagpur 721302 India;

    Geology and Geophysics Indian Institute of Technology Kharagpur 721 302 India;

    Geology and Geophysics Indian Institute of Technology Kharagpur 721 302 India;

    School of Environmental Science and Engineering Indian Institute of Technology Kharagpur 721 302 India;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Groundwater; Ganges river; Coastal aquifer; Sundarbans; Hydroclimate; Bay of Bengal;

    机译:地下水;恒河;沿海含水层;孙德尔巴斯;水池;孟加拉湾;

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