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Implications of Hydrologic Data Assimilation in Improving Suspended Sediment Load Estimation in Lake Tahoe, California

机译:加利福尼亚州太浩湖水文资料同化对提高悬沙含量估算的意义

摘要

Pursuant to the federal Clean Water Act (CWA), when a water body has been listed as impaired, Total Maximum Daily Loads (TMDLs) for the water quality constituents causing the impairment must be developed. A TMDL is the maximum daily mass flux of a pollutant that a waterbody can receive and still safely meet water quality standards. The development of a TMDL and demonstrating compliance with a TMDL requires pollutant load estimation. By definition, a pollutant load is the time integral product of flows and concentrations. Consequently, the accuracy of pollutant load estimation is highly dependent on the accuracy of runoff volume estimation. Runoff volume estimation requires the development of reasonable transfer functions to convert precipitation into runoff. In cold climates where a large proportion of precipitation falls as snow, the accumulation and ablation of snowpack must also be estimated. Sequential data assimilation techniques that stochastically combine field measurements and model results can significantly improve the prediction skill of snowmelt and runoff models while also providing estimates of prediction uncertainty. Using the National Weather Serviceu27s SNOW-17 and the Sacramento Soil Moisture Accounting (SAC-SMA) models, this study evaluates particle filter based data assimilation algorithms to predict seasonal snow water equivalent (SWE) and runoff within a small watershed in the Lake Tahoe Basin located in California. A non-linear regression model is then used that predicts suspended sediment concentrations (SSC) based on runoff rate and time of year. Runoff volumes and SSC are finally combined to provide an estimate of the average annual sediment load from the watershed with estimates of prediction uncertainty. For the period of simulation (10/1/1991 to 10/1/1996), the mean annual suspended sediment load is estimated to be 753 tonnes/yr with a 95% confidence interval about the mean of 626 to 956 tonnes/yr. The 95% prediction interval for any given year is estimated to range from approximately 86 to 2,940 tonnes/yr.
机译:根据联邦《清洁水法》(CWA),当水体被列为受损时,必须制定导致损害的水质成分的总最大日负荷量(TMDL)。 TMDL是水体可以接受并仍安全符合水质标准的污染物的最大每日质量通量。开发TMDL并证明其符合TMDL要求估算污染物负荷。根据定义,污染物负荷是流量和浓度的时间积分积。因此,污染物负荷估算的准确性高度依赖于径流量估算的准确性。径流量估算需要开发合理的传递函数,以将降水转化为径流量。在寒冷的气候中,大部分降水会随着雪降落,还必须估算积雪的积聚和消融。随机组合现场测量和模型结果的顺序数据同化技术可以显着提高融雪和径流模型的预测能力,同时还可以提供预测不确定性的估计。使用美国国家气象局的SNOW-17和萨克拉曼多土壤水分核算(SAC-SMA)模型,本研究评估了基于粒子过滤器的数据同化算法,以预测湖中小流域的季节性雪水当量(SWE)和径流塔霍盆地位于加利福尼亚州。然后使用非线性回归模型,该模型基于径流量和一年中的时间来预测悬浮沉积物浓度(SSC)。最后将径流量和SSC结合起来,以估算出该流域的年平均泥沙量,并估算出不确定性。在模拟期间(1991年1月1日至1996年10月1日),年平均悬浮泥沙负荷估计为753吨/年,95%的置信区间约为626至956吨/年。每年的95%预测间隔估计为每年约86吨至2,940吨。

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    Leisenring Marc;

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  • 年度 2011
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