Comments by "H. de Jong" (@h.dejong2531) on "" video.
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No, it's not Photoshop. the actual images are in infrared. So we have to apply a transformation to make the image visible at all. For a color image, they take 3 images, using different filters (different wavelength bands, the same way a photo consists of R, G and B channels).
After downloading, the imaging team assigns colors to each image and stacks them to make a color image. There is some artistic freedom in choosing which colors to use, but generally the longest wavelengths are mapped to red, medium to green and short to blue.
for redshifted objects, the team can choose filters that match (more or less) the redshifted red, green and blue, so the image you get back out is an accurate representation of what the object would look like in visible light for a nearby observer.
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We have millions of images of Earth. The Himawari and GOES images (and Meteosat, which uses a similar imaging system) provide images in 10k x 10k resolution, in 16 spectral bands. The spectral bands are optimized for meteorology, so you won't get an RGB image. They do have red and blue channels, not green IIRC.
There are other Earth observation satellites in GEO: NASA's Terra satellite makes full-disk images.
A little farther out at the L1 point, we have DSCOVR, with another excellent camera on board. https://www.youtube.com/watch?v=xPM2kITNtTs
For more detailed images, we have lower-altitude satellites like Landsat, SPOT, the Maxar constellation etc. These are in low orbit, so they can't take full-hemisphere images. Still, several of these image the entire Earth on a regular basis.
We have photos from several interplanetary missions, e.g. Voyager and Galileo, which made full-disk images on their way out. And of course the photos and film made by the Apollo missions.
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