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Impact of climate variation and change on Mid-Atlantic Region hydrology and water resources

机译:气候变化和变化对大西洋中部地区水文学和水资源的影响

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摘要

The sensitivity of hydrology and water resources to climate variation and climate change is assessed for the Mid-Atlantic Region (MAR) of the United States. Observed streamflow, groundwater, and water-quality data are shown to vary in association with climate variation; Projections of future streamflow, groundwater, and water quality are made using models determined from these associations and are applied to 2 transient general circulation model (GCM) scenarios. Regional streamflow increases in one scenario, but decreases in the other; both scenarios result in changes in the seasonality of peak flows. Response of groundwater to climate change depends on the GCM scenario used. Canadian Climate Center (CCC) scenarios suggest recharge will occur earlier in the year, and that seasonal fluctuations in groundwater levels will be less extreme. Hadley Center scenarios suggest recharge will occur earlier in the medium term, but later in the long term, with seasonal fluctuations in general being more extreme. Both scenarios show that nutrient loads can be expected to increase in winter and spring because of the expected increase in streamflow. Projected decreases in streamflow and associated nutrient fluxes in July and August could ameliorate problems associated with estuarine stratification and eutrophication in late summer. These projections demonstrate that future hydrology and water resources will be influenced by climate change, but that uncertainty in accurately projecting that influence will continue until model scenarios improve. [References: 42]
机译:美国中大西洋地区(MAR)评估了水文学和水资源对气候变化和气候变化的敏感性。观测到的水流,地下水和水质数据显示与气候变化有关。使用从这些关联确定的模型对未来的流量,地下水和水质进行了预测,并将其应用于2个瞬态通用循环模型(GCM)方案。区域流量在一种情况下增加,但在另一种情况下减少;这两种情况都会导致高峰流量的季节性变化。地下水对气候变化的响应取决于所使用的GCM方案。加拿大气候中心(CCC)情景表明补给将在今年早些时候发生,并且地下水位的季节性波动不会那么严重。哈德利中心(Hadley Center)的场景表明,补给将在中期出现,但从长期来看会出现后期,总体而言,季节性波动更为严重。两种情况都表明,由于预期的水流量增加,冬季和春季的养分含量有望增加。预计7月和8月的水流量和相关养分通量减少,可能会缓解夏末与河口分层和富营养化有关的问题。这些预测表明,未来的水文学和水资源将受到气候变化的影响,但是准确预测这种影响的不确定性将持续到模型情景得到改善为止。 [参考:42]

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