This article has been reviewed according to Science X's editorial process and policies. Editors have highlighted the following attributes while ensuring the content's credibility: When high or low tide occurs, the water does not necessarily rise and fall uniformly along the entire coastline. In fact, the height of the tide in a bay can vary by up to one meter (3 feet) from one location to another just a few kilometers away.
This is shown in a new study published by researchers from DTU Space in collaboration with colleagues from the University of Oxford and the Technical University of Munich (TUM), as well as the German space technology company OHB. Together, they have analyzed satellite images taken over a period of more than 40 years by the U.S. Typically, tides are measured using water level gauges located at specific sites or through satellite measurements of the sea surface.
Especially in sparsely populated areas, this leaves large areas without direct measurements of tidal height along the coast. The new method is instead based on satellite images of the coastline itself: "Typically, water level gauges are spaced 50 km (31 miles) apart or more, and measurements are then calculated from their values. With this method, we can instead use satellite images of the coastline to obtain a much more detailed picture of how tidal levels vary geographically along a given coastline," says Professor Ole Baltazar Andersen of DTU Space, a co-author of the study, which has been published in Communications Earth & Environment.
By tracking the boundary between land and water across thousands of satellite images and combining these data with information about the beach's slope, researchers can calculate changes in water level and thus tidal variations. This allows for far greater precision than previous methods, says Michael Hart-Davis, a researcher at DGFI-TUM and the lead author of the article: "Variations in the coastline have often been regarded as noise that needed to be removed from satellite data. Here, we show that this noise can instead be used as a signal to map tidal patterns on a very local scale," he says.
The extensive satellite data allow researchers to verify and improve existing tidal models, thereby contributing in the long term to more accurate local forecasts of high and low tides. "The interesting thing is that we can use this new knowledge to improve the models. In the long run, this could give us better local tidal forecasts, even along coastal stretches where we currently have very few measurements," says Andersen.
This could be particularly significant in areas where traditional water level gauges are few and far between. "In Denmark, we have many water level gauges and relatively small tidal variations, so here the method isn't quite as significant. But in Greenland, for example, it's completely different.
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