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Is the bounding box/geometry always constant? #14
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Not 100% sure, that's why there's also a todo in the code. As far as I can tell from the examples that I have access to, yes it is always full disk. But the amount of examples that I have might not give me a full view on things. Probably to be confirmed by NOAA. Note to self: If it is always full disk, I should set the corresponding field from goes extension. Note: This is partially a duplicate of #9. |
There are a number of issues here:
The corresponding commit for these changes is at 4914207 if you'd like to have a look. |
Here's an example of the G17 Item that crosses the antimeridian: |
It's an ABI definition (there's some text on this page: https://www.goes-r.gov/spacesegment/abi.html) so I agree that it isn't appropriate to use for the GLM data.
Agreed. We have a utility in stactools that can either split or "normalize" an antimeridian-crossing geometry, since (as you correctly point out) different tools do better with different formats. I think splitting for now is fine, and we can refine later if we need to change.
I'll take an action to chase this down on my side, but for now let's ignore the cutout in this package and come back and update later if needed. |
NOAA can't provide anything that we could really use here so far.
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All items created by this package have the same bounding box (and therefore geometry):
goes-glm/src/stactools/goes_glm/stac.py
Line 191 in f96294f
Is this true? I know for GOES ABI data, there are different image scales (e.g. meso-scale, full disk, and CONUS). The GLM is a different instrument so probably works differently, but I just wanted to check that all GLM netCDF items should have a bounding box that encompasses the full disk.
Also, is it the same bounding box regardless of whether the data are from
-16
or-17
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