Unveiling Significant Shoreline Changes in Lake Michigan After a Record-Setting Water Level Increase using High-Resolution Satellite Images

In this paper, high-resolution multispectral satellite images were used to uncover a remarkable shoreline transformation in Lake Michigan coastal areas, driven by a record-setting increase in the water level between 2013 and 2020. Shoreline change analyses were conducted for eleven different natural beaches around the lake, unveiling significant variations of shoreline retreat despite being affected by the same water level increase. The average observed shoreline retreats between 2013 and 2020 for the beaches ranged between 20 m and 62 m. When the passive inundation was excluded, the estimated morphological changes were found to differ significantly from site to site, with some locations experiencing minimal changes, while others encountered considerable morphological changes of up to 38m. The examination of the correlation between the morphological changes and ten hydrodynamic and morphological factors revealed strong correlations with the offshore slopes and beach width, with steeply sloping, wide beaches experiencing more erosion. Notably, wave power, longshore sediment transport divergence, and the number of storms exhibited moderate correlation with the observed morphological changes. The results of the shoreline changes and correlation analysis offer valuable insights into the varied effects of increased water levels on Lake Michigan beaches, including erosion and passive inundation, while shedding light on the key factors driving shoreline erosion in this context. These insights can help decision and policymakers in making informed choices regarding the protection and management of Lake Michigan coastal areas, particularly in anticipation of future incidents of water level increase