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首页> 外文期刊>Transactions of the ASABE >EFFECT OF ENSO-INDUCED CLIMATE VARIABILITY ON GROUNDWATER LEVELS IN THE LOWER APALACHICOLA-CHATTAHOOCHEE-FLINT RIVER BASIN
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EFFECT OF ENSO-INDUCED CLIMATE VARIABILITY ON GROUNDWATER LEVELS IN THE LOWER APALACHICOLA-CHATTAHOOCHEE-FLINT RIVER BASIN

机译:ENSO诱发的气候变化对下阿帕奇奇拉-查塔霍奇-弗林特河盆地地下水位的影响

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摘要

Rapid population growth, urban sprawl, and increased agricultural production in the Apalachicola-Chattahoochee-Flint (ACF) river basin are threatening the availability of freshwater resources and greatly affecting the supply of freshwater to Apalachicola Bay, which supports a struggling shellfish industry. As a result, Alabama, Georgia, and Florida have been fighting over the allocation of ACF river basin water for the past three decades. The water conflict heats up every time there is drought in the basin. In the Southeast US., droughts are mainly caused by the La Nina phase of the seasonal-to-interannual climate variability phenomenon known as the El Nino Southern Oscillation (ENSO). Understanding and quantifying the impact of ENSO-induced climate variability on precipitation, soil moisture, streamflows, and groundwater levels can provide valuable information for sustainable management of water resources in this region. This study was undertaken to quantify the impact of ENSO on groundwater levels in the lower ACF river basin, an area highly dependent on groundwater for agricultural water use. Twenty-one observation wells with 30 years of monthly groundwater level data were used to study the ENSO-groundwater level relationship. Wavelet analysis techniques were used to study the teleconnection between ENSO and groundwater levels, while Mann-Whitney tests were conducted to quantify the impact. The effect of prolonged La Nina events on groundwater levels and their corresponding recovery periods were also studied Results indicate a strong relationship between groundwater level fluctuations and ENSO. This relationship was found to be stronger during the recharge season (December-April) as compared to the non-recharge or agricultural irrigation season (May-November). The results obtained can be used to develop procedures for forecasting groundwater levels, which can then be used to better manage the groundwater resources of this region.
机译:Apalachicola-Chattahoochee-Flint(ACF)流域的快速人口增长,城市扩张和农业生产增加正威胁着淡水资源的供应,并极大地影响了向苦苦挣扎的贝类产业提供支持的Apalachicola湾的淡水供应。结果,在过去的三十年中,阿拉巴马州,佐治亚州和佛罗里达州一直在争夺ACF流域水的分配。每当流域发生干旱时,水冲突就会加剧。在美国东南部,干旱主要是由季节到年际的气候变化现象的拉尼娜期引起的,该现象被称为厄尔尼诺南方涛动(ENSO)。了解和量化ENSO引起的气候变化对降水,土壤湿度,水流和地下水位的影响,可以为该地区的水资源可持续管理提供有价值的信息。这项研究旨在量化ENSO对ACF下游流域地下水水位的影响,该地区高度依赖于地下水用于农业用水。使用二十个观测井以及每月30年的地下水位数据来研究ENSO与地下水位的关系。小波分析技术用于研究ENSO与地下水位之间的遥相关性,而曼恩·惠特尼(Mann-Whitney)测试用于量化影响。还研究了长时间的拉尼娜事件对地下水位及其相应恢复期的影响。结果表明,地下水位波动与ENSO有很强的关系。与非补给或农业灌溉季节(5月至11月)相比,补给季节(12月至4月)的这种关系更强。获得的结果可用于开发预测地下水位的程序,然后可用于更好地管理该地区的地下水资源。

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