- Joined
- Jun 27, 2017
- Professional Status
- Certified General Appraiser
- State
- California
FYI. (Something good for California appraisers to know ...)
ME: Can the GIS coordinates of a location on earth change?
ChatGPT: "Yes, the GIS coordinates of a location on Earth can change due to several natural and human-made reasons. Here are the primary factors contributing to such changes:
ME: How do surveyors handle such changes?
ChatGPT: "Surveyors handle the changes in GIS coordinates due to natural phenomena and human activities by employing a variety of methods and technologies to ensure that their measurements remain accurate and up to date. Here are some of the primary approaches:
https://oceanservice.noaa.gov/education/tutorial_geodesy/
ME: Can the GIS coordinates of a location on earth change?
ChatGPT: "Yes, the GIS coordinates of a location on Earth can change due to several natural and human-made reasons. Here are the primary factors contributing to such changes:
- Plate Tectonics: The Earth's lithospheric plates are constantly moving, albeit very slowly. This movement can cause the coordinates of locations on these plates to change over time. For example, the Pacific Plate, on which part of California sits, moves northwestward relative to the North American Plate.
- Land Subsidence and Uplift: Certain processes such as groundwater extraction, mining, and natural compaction of sediment can cause land to subside, while geological processes like isostatic rebound can cause land to rise. These changes can alter the elevation and horizontal position of a location.
- Glacial Rebound: In regions previously covered by glaciers, the land is still rebounding from the weight of the ice that has melted since the last Ice Age. This process of isostatic adjustment can change both the elevation and latitude of locations.
- Earthquakes: Significant seismic activity can abruptly change the landscape, shifting the coordinates of affected areas. For example, the 2011 earthquake in Japan shifted the entire country's main island of Honshu by several meters to the east.
- Human Activities: Large-scale construction projects like dams or reclamation can physically alter the landscape, influencing the coordinates of locations. Additionally, changes in how coordinates are measured or defined by geodetic systems (such as updates to GPS technology or shifts from one datum to another) can also alter the recorded coordinates of a location.
ME: How do surveyors handle such changes?
ChatGPT: "Surveyors handle the changes in GIS coordinates due to natural phenomena and human activities by employing a variety of methods and technologies to ensure that their measurements remain accurate and up to date. Here are some of the primary approaches:
- Continual Monitoring and Re-Surveying: In areas known to be susceptible to significant changes (e.g., earthquake zones, subsiding cities), surveyors frequently re-survey to update the data. This ongoing monitoring helps in managing and anticipating significant shifts in the landscape.
- GPS and Satellite Technology: Modern surveying heavily relies on Global Positioning System (GPS) technology, which can provide precise and continual updates on location data. GPS, along with other satellite-based systems like GNSS (Global Navigation Satellite System), allows surveyors to detect and record even minor changes in position.
- Geodetic Datums: Surveyors use geodetic datums, which are reference systems that provide a frame of reference for measuring locations on Earth. As our understanding of the Earth’s shape and size improves, or as shifts in the Earth’s surface occur, these datums are periodically updated. Surveyors must adjust their measurements to align with the current datum to ensure accuracy.
- InSAR (Interferometric Synthetic Aperture Radar): This technology uses radar images from satellites to detect changes in the Earth’s surface. It’s particularly useful for monitoring slow, gradual movements, such as those caused by land subsidence or volcanic activity.
- LIDAR (Light Detection and Ranging): LIDAR uses light in the form of a pulsed laser to measure variable distances to the Earth. This technology provides high-resolution maps of the Earth's surface, which are essential for detecting changes over time.
- Robotic Total Stations: These are advanced surveying instruments that automatically track a moving prism and can operate continuously. They are often used in monitoring applications to detect and record real-time changes in the position of structures or landforms.
- Collaboration with Geologists and Engineers: Surveyors often collaborate with other professionals to understand the underlying causes of geographical changes, such as plate tectonics or groundwater extraction, which can inform more effective surveying strategies and adjustments.
https://oceanservice.noaa.gov/education/tutorial_geodesy/
At its most basic level of definition, the horizontal datum is a collection of specific points on the Earth that have been identified according to their precise northerly or southerly location (latitude) and easterly or westerly location (longitude).
At its most basic level of definition, the horizontal datum is a collection of specific points on the Earth that have been identified according to their precise northerly or southerly location (latitude) and easterly or westerly location (longitude).
oceanservice.noaa.gov
At its most basic level of definition, the horizontal datum is a collection of specific points on the Earth that have been identified according to their precise northerly or southerly location (latitude) and easterly or westerly location (longitude).
At its most basic level of definition, the horizontal datum is a collection of specific points on the Earth that have been identified according to their precise northerly or southerly location (latitude) and easterly or westerly location (longitude).
oceanservice.noaa.gov
The Vertical Datum: Global Positioning Tutorial
The vertical datum is a collection of specific points on the Earth with known heights either above or below mean sea level. Near coastal areas, mean sea level is determined with a tide gauge. In areas far away from the shore, mean sea level is determined by the shape of the geoid.
oceanservice.noaa.gov