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What do you want to achieve? Computation of topocentric parallax is based on the WGS84 ellipsoid. The mathematical horizon is 90 degrees from the zenith, regardless of whether you are in a geoid depression or on the highest mountain. Which results in archaeoastronomy do you think would change? Where are sub-arcseconds relevant? Atmospheric variance certainly creates more uncertainty. One crucial element is getting a correctly aligned horizon panorama. This is where I started in 2010... When you follow the User Guide, you can have that now. And much more. |
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I was looking at the JPL Horizons manual and it discussed the allowance for the ellipsoid elevation due to variations around the world.
I followed the instructions, went to the site offered to calculate the elevation and input coordinates for a number of random locations from Stellarium for comparison and found that some had negative elevation values. When looking at the total difference in elevations I found it could be as much as 80 metres.
What do I do? Adjust the given results for geoid elevation, for known height above MSL and enter that into the location within Stellarium? Or does Stellarium already include the geoid elevation variance in its given elevation levels? What about sites that are not in Stellarium’s list of observation locations?
I am wanting to experiment with archaeoastronomy on different locations but I imagine that large elevation differences may affect the results?
Very new to this so I hope someone can assist.
Cheers
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