Gezeitenmaß

Gezeitenmaß refers to the measurement of tides. It is a crucial aspect of oceanography and maritime navigation. Tides are the regular rise and fall of the sea level caused by the gravitational forces of the Moon and the Sun. The measurement of these changes is essential for understanding tidal patterns, predicting future tide levels, and ensuring safe passage for ships.

Historically, gezeitenmaß was conducted using simple tide poles or markers that indicated the water level at different times. As technology advanced, more sophisticated instruments like tide gauges were developed. These gauges can be mechanical or electronic, continuously recording the height of the tide. Modern gezeitenmaß often involves satellite altimetry, which uses radar to measure the distance from a satellite to the ocean surface, providing a global overview of sea level variations, including tidal effects.

The data collected through gezeitenmaß is used for various purposes. It helps in determining mean sea level, identifying extreme high and low tides, and calculating tidal ranges. This information is vital for port authorities to manage shipping schedules, for coastal engineers to design infrastructure, and for researchers studying the impact of climate change on sea levels. Understanding and accurately measuring gezeitenmaß contributes to both scientific knowledge and practical applications in coastal and marine environments.