Fergus C Emi, Brooks J Renée, Kaufmann Philip R, Herlihy Alan T, Pollard Amina I, Weber Marc H, Paulsen Steven G
National Research Council (Fergus, Herlihy), U.S. Environmental Protection Agency, Corvallis, Oregon, USA; Pacific Ecological Systems Division (Brooks, Kaufmann, Weber, Paulsen), U.S. Environmental Protection Agency, Corvallis, Oregon, USA; Office of Water (Pollard), U.S. Environmental Protection Agency, Washington, DC, USA.
J Am Water Resour Assoc. 2020 Jun 1;56(3):450-471. doi: 10.1111/1752-1688.12817.
Establishing baseline hydrologic characteristics for lakes in the U.S. is critical to evaluate changes to lake hydrology. We used the U.S. EPA National Lakes Assessment 2007 and 2012 surveys to assess hydrologic characteristics of a population of ~45,000 lakes in the conterminous U.S. based on probability samples of ~1,000 lakes/yr distributed across nine ecoregions. Lake hydrologic study variables include water-level drawdown (i.e., vertical decline and horizontal littoral exposure) and two water stable isotope-derived parameters: evaporation-to-inflow (E:I) and water residence time. We present 1) national and regional distributions of the study variables for both natural and man-made lakes and 2) differences in these characteristics between 2007 and 2012. In 2007, 59% of the population of U.S. lakes had or drawdown relative to water levels in ecoregional reference lakes with minimal human disturbances; while in 2012, only 20% of lakes were significantly drawn down beyond normal ranges. Water isotope-derived variables did not differ significantly between survey years in contrast to drawdown. Median E:I was 20% indicating that flow-through processes dominated lake water regimes. For 75% of U.S. lakes, water residence time was < 1 year and was longer in natural vs. man-made lakes. Our study provides baseline ranges to assess local and regional lake hydrologic status and inform management decisions in changing environmental conditions.
确定美国湖泊的基线水文特征对于评估湖泊水文变化至关重要。我们利用美国环保署2007年和2012年的全国湖泊评估调查,基于每年约1000个湖泊分布在九个生态区域的概率样本,评估美国本土约45000个湖泊的水文特征。湖泊水文研究变量包括水位下降(即垂直下降和水平湖滨暴露)以及两个由水稳定同位素得出的参数:蒸发与流入量之比(E:I)和水停留时间。我们展示了1)天然湖和人工湖研究变量的全国及区域分布,以及2)2007年至2012年这些特征的差异。2007年,相对于人类干扰最小的生态区域参考湖泊的水位,美国59%的湖泊出现了水位下降或有下降趋势;而在2012年,只有20%的湖泊水位显著下降至正常范围之外。与水位下降情况相反,水同位素得出的变量在不同调查年份之间没有显著差异。E:I中位数为20%,这表明湖泊水流状态以流通过程为主导。对于75%的美国湖泊,水停留时间小于1年,且天然湖的水停留时间长于人工湖。我们的研究提供了基线范围,以评估当地和区域湖泊的水文状况,并为在不断变化的环境条件下的管理决策提供参考。