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Cake day: July 18th, 2020

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  • English used to be like other European languages too. We had thou/thee for singular, and you/ye for plural, and for respectful singular. Eventually, people began using it as respectful singular for everyone, and so it just became singular and plural, eclipsing thou/thee. Around this time, the you/ye accusative/nominative distinction was also lost, so now we just have you.

    If you’re curious, the you/ye distinction worked like this: “you” was used for the subject (the doer) of the sentence, and “ye” was used for the object (the done to). you/ye are analogous to I/me.

    “You come with me.” (plural you)

    “I come with ye.” (plural ye)

    As a result of the loss of thou, we also lost the conjugation of verbs related to it, like “art” instead of “are”, and “-st” or “-est” for other verbs (“goest”, “thinkst”, etc). It used to be that “are” was only for plural pronouns, but now both “you” and “they” can be singular.

    And if you’re curious about what happened to “-eth”, evidence suggests this was for a long time a typographic feature, and it was pronounced “-s” as it is today. It was used exactly like “-s”. “He thinketh” would have been pronounced “he thinks”.




  • Xavienth@lemmygrad.mltoProgrammer Humor@lemmy.mlcheckmate
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    7 days ago

    Adobe products often have no real equal. It sucks, but it’s the way it is. Gimp doesn’t come close to Photoshop, Inkscape is almost as good as Adobe Illustrator, and After Effects is the most capable video editing software I’ve ever used.

    It sucks that they try and lock you into proprietary file formats, like Substance Painter.






  • The difference in relative acceleration implied by the meme is on the order of tens of yoctometres (10⁻²³ m) per second per second.

    It’s a difference so small that it would be overshadowed by the fact that you’re holding one object femtometres (10⁻¹⁵ m) higher or lower than the other in the gravitational field.

    Additional sources of error to consider at this scale might be the heat radiation from the surroundings providing radiation pressure on the object, the sloshing of Earth’s core causing time-dependent variations in the gravitational field, the location-dependent variations in the Earth’s gravitational field, and the difference in centrifugal (yes, centrifugal in this reference frame) force due to latitude differences of one micrometre, and also due to natural variations in the rate of Earth’s rotation over time.