The temporal aspect of peak water level in a specific coastal Maine location is the central focus. This phenomenon occurs twice daily, but the precise timing shifts predictably due to the lunar cycle. Accurately predicting it requires understanding astronomical influences and local geographical factors. As an example, the greatest water level might occur at 7:15 AM on one day and shift to 8:00 AM the following day.
Knowledge of the timing of the maximal water level offers several practical advantages. Navigation for marine vessels is improved, allowing safer passage through harbors and channels. Coastal activities like beachcombing, kayaking, and tide pooling are enhanced, as the optimal time for these activities is highly dependent on the state of the tide. Understanding the pattern is also essential for coastal engineering projects and environmental monitoring, influencing designs and providing baseline data.
