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首页> 外文期刊>Hydrology and Earth System Sciences >Interannual hydroclimatic variability and its influence on winter nutrient loadings over the Southeast United States
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Interannual hydroclimatic variability and its influence on winter nutrient loadings over the Southeast United States

机译:美国东南部的年际水文气候变化及其对冬季养分含量的影响

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摘要

It is well established in the hydroclimatic literature that the interannual variability in seasonal streamflow could be partially explained using climatic precursors such as tropical sea surface temperature (SST) conditions. Similarly, it is widely known that streamflow is the most important predictor in estimating nutrient loadings and the associated concentration. The intent of this study is to bridge these two findings so that nutrient loadings could be predicted using season-ahead climate forecasts forced with forecasted SSTs. By selecting 18 relatively undeveloped basins in the Southeast US (SEUS), we relate winter (January-February-March, JFM) precipitation forecasts that influence the JFM streamflow over the basin to develop winter forecasts of nutrient loadings. For this purpose, we consider two different types of low-dimensional statistical models to predict 3-month ahead nutrient loadings based on retrospective climate forecasts. Split sample validation of the predictive models shows that 18-45% of interannual variability in observed winter nutrient loadings could be predicted even before the beginning of the season for at least 8 stations. Stations that have very high coefficient of determination (> 0.8) in predicting the observed water quality network (WQN) loadings during JFM exhibit significant skill in predicting seasonal total nitrogen (TN) loadings using climate forecasts. Incorporating antecedent flow conditions (December flow) as an additional predictor did not increase the explained variance in these stations, but substantially reduced the root-mean-square error (RMSE) in the predicted loadings. Relating the dominant mode of winter nutrient loadings over 18 stations clearly illustrates the association with El Ni?o Southern Oscillation (ENSO) conditions. Potential utility of these season-ahead nutrient predictions in developing proactive and adaptive nutrient management strategies is also discussed.
机译:在水文气候文献中已经很好地确定,可以使用气候前兆(例如热带海面温度(SST)条件)部分解释季节性水流的年际变化。同样,众所周知,在估算养分含量和相关浓度时,流量是最重要的预测指标。这项研究的目的是弥合这两个发现,以便可以使用由预报的SST强迫的提前季节气候预报来预测养分含量。通过选择美国东南部(SEUS)相对较不发达的18个盆地,我们将影响该盆地JFM流量的冬季(1月至2月至3月,JFM)降水预报与养分含量的冬季预测联系起来。为此,我们考虑两种不同类型的低维统计模型,以基于回顾性气候预测来预测未来3个月的养分含量。预测模型的拆分样本验证表明,即使在季节开始之前,至少有8个站点,也可以预测观测到的冬季养分含量中18-45%的年际变化。在JFM期间预测观测到的水质网络(WQN)负荷时具有非常高的确定系数(> 0.8)的气象站显示出使用气候预测来预测季节性总氮(TN)负荷的显着技能。将先前的流量条件(12月流​​量)作为附加的预测变量并不会增加这些站中的解释方差,但会大大减少预测载荷中的均方根误差(RMSE)。与18个站点的冬季养分负荷的主要模式相关联,清楚地说明了与厄尔尼诺南方涛动(ENSO)条件的关联。还讨论了这些提前进行的养分预测在制定主动和适应性养分管理策略中的潜在用途。

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