Greene Richard M, Lehrter John C, Hagy James D
U.S. Environmental Protection Agency, Office of Research and Development, National Health and Environmental Effects Research Laboratory, Gulf Ecology Division, 1 Sabine Island Drive, Gulf Breeze, Florida 32561, USA.
Ecol Appl. 2009 Jul;19(5):1161-75. doi: 10.1890/08-0035.1.
A new suite of multiple regression models was developed that describes relationships between the area of bottom water hypoxia along the northern Gulf of Mexico and Mississippi-Atchafalaya River nitrate concentration, total phosphorus (TP) concentration, and discharge. Model input variables were derived from two load estimation methods, the adjusted maximum likelihood estimation (AMLE) and the composite (COMP) method, developed by the U.S. Geological Survey. Variability in midsummer hypoxic area was described by models that incorporated May discharge, May nitrate, and February TP concentrations or their spring (discharge and nitrate) and winter (TP) averages. The regression models predicted the observed hypoxic area within +/-30%, yet model residuals showed an increasing trend with time. An additional model variable, Epoch, which allowed post-1993 observations to have a different intercept than earlier observations, suggested that hypoxic area has been 6450 km2 greater per unit discharge and nutrients since 1993. Model forecasts predicted that a dual 45% reduction in nitrate and TP concentration would likely reduce hypoxic area to approximately 5000 km2, the coastal goal established by the Mississippi River/Gulf of Mexico Watershed Nutrient Task Force. However, the COMP load estimation method, which is more accurate than the AMLE method, resulted in a smaller predicted hypoxia response to any given nutrient reduction than models based on the AMLE method. Monte Carlo simulations predicted that five years after an instantaneous 50% nitrate reduction or dual 45% nitrate and TP reduction it would be possible to resolve a significant reduction in hypoxic area. However, if nutrient reduction targets were achieved gradually (e.g., over 10 years), much more than a decade would be required before a significant downward trend in both nutrient concentrations and hypoxic area could be resolved against the large background of interannual variability. The multiple regression models and statistical approaches applied provide improved capabilities for evaluating dual nutrient management strategies to address Gulf hypoxia and a clearer perspective on the strengths and limitations of approaching the problem using regression models.
开发了一套新的多元回归模型,用于描述墨西哥湾北部底层水缺氧区域与密西西比 - 阿查法拉亚河硝酸盐浓度、总磷(TP)浓度及流量之间的关系。模型输入变量源自美国地质调查局开发的两种负荷估算方法,即调整后的最大似然估计(AMLE)法和综合(COMP)法。通过纳入五月流量、五月硝酸盐以及二月TP浓度或其春季(流量和硝酸盐)与冬季(TP)平均值的模型,描述了仲夏缺氧区域的变化情况。回归模型预测的缺氧区域与观测值的偏差在±30%以内,但模型残差随时间呈上升趋势。另一个模型变量“时期”(Epoch)使1993年后的观测值具有与早期观测值不同的截距,这表明自1993年以来,单位流量和养分条件下的缺氧区域增加了6450平方公里。模型预测表明,硝酸盐和TP浓度双双降低45%可能会使缺氧区域减少至约5000平方公里,这是密西西比河/墨西哥湾流域营养物特别工作组设定的沿海目标。然而,比AMLE方法更准确的COMP负荷估算方法,相较于基于AMLE方法的模型,对任何给定养分减少量所预测的缺氧响应更小。蒙特卡洛模拟预测,在硝酸盐瞬间减少50%或硝酸盐和TP双双减少45%五年后,有可能解决缺氧区域的显著减少问题。然而,如果养分减少目标是逐步实现的(例如,在10年内),在养分浓度和缺氧区域出现显著下降趋势之前,需要十多年时间才能在较大的年际变化背景下解决该问题。所应用的多元回归模型和统计方法为评估解决海湾缺氧问题的双重养分管理策略提供了更强的能力,并更清晰地展现了使用回归模型解决该问题的优势与局限性。