Ellipsoid and Geoid
Ellipsoid:
- Imagine the Earth is shaped like a slightly squished ball. An ellipsoid is a smooth, math-based shape like this that we use to help map the Earth.
- Different ellipsoids fit the Earth in slightly different ways, like picking the best-fitting ball for different parts of the world.
Geoid:
- The geoid is like the shape of the sea level if it was extended all around the Earth, even under the land. It's a wavy, bumpy surface because gravity pulls differently in different places.
- We use the geoid to measure heights, like how tall a mountain is above sea level.
Datums
Datums:
- A datum is like a starting point or baseline for measuring places on Earth. Think of it as a fixed reference point from which we measure.
- There are two main types:
- Geodetic (Horizontal) Datums: These are like a grid we lay over the Earth to measure positions (latitude and longitude).
- Vertical Datums: These help us measure heights (elevations) above sea level.
Geodetic and Vertical
Geodetic:
- Geodetic refers to the system we use to measure exact positions on the Earth's surface. It includes latitude, longitude, and sometimes height.
- These measurements help us understand where things are located precisely on the globe.
Vertical:
- Vertical measurements tell us how high or low something is compared to sea level.
- This is useful for things like building roads, measuring mountain heights, and flood planning.
Global and Local
Global:
- Global systems cover the whole world. They provide a way to measure things consistently no matter where you are on Earth.
- Examples are the systems used by GPS satellites.
Local:
- Local systems are designed for specific regions or countries. They are very accurate in their area but might not work well globally.
- For example, a local system might be used just for North America or just for Great Britain.
In summary, these concepts help us map and measure the Earth accurately, whether we're looking at the whole world or just a small part of it.
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