Earth Observation path to imaging introduction tutorial - #6970
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Reuse the same threshold -> label -> count workflow on a Sentinel-2 water-index image to count Greenland supraglacial melt ponds, mirroring the cross-discipline 'Choose Your Own Adventure' pattern of the object-tracking-using-cell-profiler and process-image-bioimageio tutorials. Adds the CYOA Bioimaging/Earth split, the EO dataset (Zenodo 10.5281/zenodo.20960690), two EO result figures, the Earth observation tag, and OSCARS funding. Validated end-to-end on usegalaxy.eu (13 major melt lakes).
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Sorry it took a while, I'm looking into it now. |
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| > <comment-title> Counting melt ponds with a cell-counting workflow </comment-title> | ||
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| > In the Earth observation path, we reuse *the same* segment-and-count workflow that was built for counting of stained cell nuclei to count *supraglacial melt ponds* on the Greenland ice sheet. This is a cross-discipline experiment from the [OSCARS-FIESTA](https://oscars-project.eu/projects/fair-image-analysis-across-sciences) project. Why does it work? Melt ponds have a high ice-adapted water index, so in a water-index image they appear as *bright blobs on a darker background*, which is the same characteristic that is exploited for segmenting cell nuclei. The same threshold–label–count steps that count nuclei count melt ponds; only the *index* and the *interpretation of the threshold* are domain-specific. |
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The same threshold–label–count steps that count nuclei count melt ponds; only the index and the interpretation of the threshold are domain-specific.
I re-phrased the text above to improve clarity, but I'm not sure myself what the last 1-2 sentences actually mean. Can you please try to phrase them more clearly?
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| > <comment-title> How the satellite image was prepared </comment-title> | ||
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| > The image is a single-band ice-adapted normalised-difference water index, NDWI<sub>ice</sub> = (blue − red)/(blue + red) (Williamson et al. 2018, [doi:10.5194/tc-12-3045-2018](https://doi.org/10.5194/tc-12-3045-2018)), computed from a Sentinel-2 Level-2A scene (tile T22WEV, 2019-07-23) over the south-west Greenland ablation zone and rescaled to 16-bit so that melt ponds are bright. The preprocessing notebooks, the full Galaxy run provenance, the validation against an independently published lake map, and a citable archive are in the [OSCARS-FIESTA example repository](https://github.com/annefou/fiesta-galaxy-meltponds-eo). |
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Can you please use the {% cite ... %} syntax for the reference?
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| > <comment-title> How the satellite image was prepared </comment-title> | ||
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| > The image is a single-band ice-adapted normalised-difference water index, NDWI<sub>ice</sub> = (blue − red)/(blue + red) (Williamson et al. 2018, [doi:10.5194/tc-12-3045-2018](https://doi.org/10.5194/tc-12-3045-2018)), computed from a Sentinel-2 Level-2A scene (tile T22WEV, 2019-07-23) over the south-west Greenland ablation zone and rescaled to 16-bit so that melt ponds are bright. The preprocessing notebooks, the full Galaxy run provenance, the validation against an independently published lake map, and a citable archive are in the [OSCARS-FIESTA example repository](https://github.com/annefou/fiesta-galaxy-meltponds-eo). |
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This looks like a DOI which could be better served by using the built-in Citations mechanism. You can use https://doi2bib.org to convert your DOI into a .bib formatted entry, and add to your tutorial.md
| > The image is a single-band ice-adapted normalised-difference water index, NDWI<sub>ice</sub> = (blue − red)/(blue + red) (Williamson et al. 2018, [doi:10.5194/tc-12-3045-2018](https://doi.org/10.5194/tc-12-3045-2018)), computed from a Sentinel-2 Level-2A scene (tile T22WEV, 2019-07-23) over the south-west Greenland ablation zone and rescaled to 16-bit so that melt ponds are bright. The preprocessing notebooks, the full Galaxy run provenance, the validation against an independently published lake map, and a citable archive are in the [OSCARS-FIESTA example repository](https://github.com/annefou/fiesta-galaxy-meltponds-eo). | |
| > The image is a single-band ice-adapted normalised-difference water index, NDWI<sub>ice</sub> = (blue − red)/(blue + red) (Williamson et al. 2018{% cite ... %})), computed from a Sentinel-2 Level-2A scene (tile T22WEV, 2019-07-23) over the south-west Greenland ablation zone and rescaled to 16-bit so that melt ponds are bright. The preprocessing notebooks, the full Galaxy run provenance, the validation against an independently published lake map, and a citable archive are in the [OSCARS-FIESTA example repository](https://github.com/annefou/fiesta-galaxy-meltponds-eo). |
Add Earth Observation path to the introduction to imaging. I think it can help to promote the tutorials we created for image analysis and which contain Earth Observation Path.