Sea elevation
The perpendicular distance of a certain point of the earth from sea level.Sea elevation refers to the height or altitude of the sea surface relative to a specific reference point, usually the mean sea level (MSL). This term is often used in the context of measuring the surface of the ocean in relation to land, and it can be affected by factors like tides, ocean currents, and atmospheric pressure.
Key Aspects of Sea Elevation:
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Mean Sea Level (MSL):
- Mean Sea Level is the average level of the sea's surface over a long period of time, typically taken from tidal observations. It serves as a baseline for measuring land elevation or the elevation of the ocean's surface.
- Sea elevation is often measured relative to MSL, which represents the "zero" point for land elevations or ocean depths.
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Tidal Influence:
- Tides are caused by the gravitational pull of the moon and the sun on Earth’s oceans. As a result, sea elevation varies throughout the day, with the water level rising and falling in a regular cycle, known as the tidal range.
- These tidal variations can cause local sea elevation to fluctuate by several meters at certain coastal locations, depending on the geography and the position of the moon and sun.
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Sea Level Rise:
- Sea level rise refers to the long-term increase in sea elevation, typically due to climate change, which leads to polar ice melt and thermal expansion of water as temperatures rise.
- Monitoring sea elevation is crucial for understanding and predicting the impacts of rising sea levels on coastal areas, including flooding, erosion, and the loss of land.
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Geographical Variations:
- Sea elevation can vary slightly across different regions due to factors like ocean currents, water temperature, air pressure, and the Earth's gravitational anomalies. This means that sea level can be slightly higher or lower in different parts of the world at any given time.
- Geoid: The shape of the Earth that represents the global mean sea level, adjusted for variations in the Earth's gravity field, is known as the geoid. It is used as a reference for more precise measurements of sea elevation.
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Sea Elevation and Navigation:
- Accurate measurements of sea elevation are important for maritime navigation and coastal engineering. They ensure that shipping routes are safe and that structures like ports, dams, and sea walls are designed to withstand changes in sea level.
Conclusion:
Sea elevation refers to the height of the ocean's surface, typically measured relative to mean sea level. It is influenced by tidal changes, long-term variations such as sea level rise, and regional differences in ocean conditions. Monitoring and understanding sea elevation is essential for managing coastal environments, navigation, and addressing the challenges of climate change.
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