Genma Saotome, on 24 July 2016 - 04:28 PM, said:
Essentially I was appending my comments to your line of thinking and not trying to rebut you. I should not have quoted you. Sorry about that.
No problems
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What I was attempting to accomplish is to make a point about why the G-H projection is no good for train simming. You do understand why it is no good but not everyone does. For example, Goku asked what's wrong G-H?
The problem with Goode Homosline projection is that it is not a conformal projection, that is it does not show all areas in there true shapes, in fact only a fraction of the earth is produce at its correct shape. This is not a problem for Transverse Mercator, if it is restricted to around plus or minus 5 degrees from its reference meridian.
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Let me also mention that the SRTM data is obsolete here in the US, it's long since been replaced by data w/ better resolution. My first route was started in 2002 and much of it was built using 30m data, not 90m SRTM. In 2003! Why are we even messing with 90m resolution today when 10m -- or smaller -- is available?
There is still a lot of areas around the world where high res terrain info is still not availible, so theres a few of us that have to struggle on with such low res data as 3 second SRTM. While 1 second data (30 metres) is availible in Australia. its not availible in a form thats is in any easy to use for MSTS, it being supplied in the proprietry ARCinfo format. Also if one requests say a 4 degree square of data, its supplied in one enormouse file. For my own use I break these down into 1 degree squares and save them in Geotiff format. My terrain modelling program using this file format directly.
Post Script. In fact the whole of Australia is availible at 1 sec resolution, unfortunately for me (i am on dialup intenet access) is only readily downloadable in a gi-normouse 25 gigabyte zipped ARCinfo file (one can make special request just for a specifc area). Just unzipping files this size takes ages even on a fast system.
Lindsay