Warren Glenn J, Lesht Barry M, Barbiero Richard P
USEPA Great Lakes National Program Office, 77 W. Jackson Blvd., Chicago, IL 60604 USA.
CSRA LLC and Department of Earth and Environmental Sciences, University of Illinois at Chicago, 845 W. Taylor St., Chicago, IL 60607 USA.
J Great Lakes Res. 2018 Aug;44(4):563-572. doi: 10.1016/j.jglr.2017.11.011.
The nearshore zone, that region of water directly influenced by its proximity to the coast, has received increasing attention in recent years. The extent of the nearshore zone has been defined by some constant descriptive feature: e.g., a specific depth or a particular distance offshore. This type of definition does not allow for the dynamic nature of the relationship between the land and water and how it may be influenced by local, seasonal, or transient effects. Here satellite observations examined evaluate how the width of the nearshore zone in Lake Michigan varies with position along the coastline and with time. Satellite-derived estimates of chlorophyll concentration along seventy-one shore-normal transects spaced approximately 10 km apart around the lake were used to determine the width of the nearshore zone, defined as the point at which the estimated chlorophyll concentration close to the shore approaches the more-uniform offshore concentration. Of a total of 23,807 transects extracted from MODIS observations made between 2003 and 2013, we successfully fit a bi-linear model relating chlorophyll concentration to distance offshore to 15,996. We found that the width of the nearshore zone is variable, both seasonally and spatially. Although the overall median width of 4.5 km (mean width 5.3 km) closely corresponds to the 5 km value used in a number of Great Lakes studies including Lake Michigan, ten percent of the estimates are greater than 8.9 km, likely representing times of enhanced mixing and transport of nearshore waters into the offshore.
近岸带,即因靠近海岸而直接受其影响的水域区域,近年来受到了越来越多的关注。近岸带的范围由一些固定的描述性特征来界定:例如,特定的深度或离岸的特定距离。这种定义方式没有考虑到陆地与水域之间关系的动态性质,以及它可能如何受到局部、季节性或短暂影响。在此,通过卫星观测来评估密歇根湖近岸带的宽度如何随海岸线位置和时间而变化。利用沿湖周围约10公里间隔的71条垂直于海岸的样带的卫星衍生叶绿素浓度估计值,来确定近岸带的宽度,近岸带定义为靠近海岸的估计叶绿素浓度接近离岸更均匀浓度的点。在从2003年至2013年的中分辨率成像光谱仪(MODIS)观测中提取的总共23,807条样带中,我们成功地将叶绿素浓度与离岸距离的双线性模型拟合到了15,996条样带上。我们发现,近岸带的宽度在季节和空间上都是可变的。尽管4.5公里的总体中位数宽度(平均宽度5.3公里)与包括密歇根湖在内的许多大湖研究中使用的5公里值非常接近,但10%的估计值大于8.9公里,这可能代表着近岸水体增强混合并输送到离岸的时期。