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Importance of stream temperature to climate change impact on water quality

机译:溪流温度对气候变化的重要性对水质的影响

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The sensitivity of some aspects of water quality to climate change wasassessed in the Seine River (France) with the biogeochemical modelRIVERSTRAHLER, which describes the transformations and fluxes of C, N, P andSi between the main microbiological populations, the water column and thesediment, along the entire river network. Point and diffuse sources areprescribed, stream temperature undergoes a sinusoidal annual cycleconstrained by observations, and runoff is calculated by a physically-basedland surface model. The reference simulation, using meteorological forcingof 1986–1990 and point sources of 1991, compares very well withobservations. The climate change simulated by a general circulation modelunder the SRES emission scenario A2 was used to simulate the related changesin runoff and stream temperature. To this end, a statistical analysis wasundertaken of the relationships between the water and air temperatures inthe Seine watershed over 1993–1999, using 88 points that correctly sampledthe variability of the tributaries. Most of stream temperature variance wasexplained by the lagged moving average of air temperature, with parametersthat depended on Strahler stream order. As an interesting simplification,stream temperature changes could be approximated by air temperature changes.This modelling framework was used to analyse of the relative influence ofthe water warming and discharge reduction induced by climate change onbiogeochemical water quality in Paris and downstream. Discharge reductionincreased phytoplankton growth and oxygen deficits. Water warming decreaseddissolved oxygen, increased phytoplankton biomass during the growth period,and reduced it afterwards, when loss factors dominate. It was also shownthat these impacts were enhanced when point source inputs of nutrient andorganic carbon increased.
机译:在塞纳河(法国)中,使用生物地球化学模型RIVERSTRAHLER评估了水质某些方面对气候变化的敏感性,该模型描述了主要微生物种群,水柱和沉积物之间的C,N,P和Si的转化和通量,以及整个河网。规定了点源和扩散源,溪流温度经历了观测值限制的正弦年周期,并且径流是通过基于物理的地面模型来计算的。使用1986-1990年的气象强迫和1991年的点源进行的参考模拟与观测值进行了很好的比较。在SRES排放情景A2下,由一般环流模型模拟的气候变化被用来模拟径流和河流温度的相关变化。为此,对塞纳河流域1993年至1999年水温与气温之间的关系进行了统计分析,使用了88个点来正确采样了支流的变化。大部分气流温度的变化可以通过空气温度的滞后移动平均值来解释,其参数取决于Strahler气流的阶数。作为一个有趣的简化,可以用空气温度变化来近似溪流温度变化。该模型框架用于分析气候变化引起的水温升高和流量减少对巴黎及下游生物地球化学水质的相对影响。减少排放量增加了浮游植物的生长和缺氧。在损失因子占主导地位的情况下,水温降低了生长期的溶解氧,增加了浮游植物的生物量,之后又减少了。研究还表明,当营养和有机碳的点源输入增加时,这些影响会增强。

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