Vita su Marte
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Vita su Marte?
Risposta concisa: "forse". Ecco una brevissima rassegna dei vari comunicati, con diversi gradi di "ottimismo" ...
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Gli ultimi otto messaggi ricevuti dalla Federazione
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@ciccillo i computer sono nella stessa rete? Se sí, e se CUPS è configurato per condividere le stampanti, le vede anche l'altro computer automaticamente via Zeroconf / avahi
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@nachocarreras come se l'uranio non si importasse dalla.... Russia!
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@ugone non sapevo che capanna margherita non fosse in valle. Si impara sempre qualcosa!
Più facile metterne uno qui https://it.wikipedia.org/wiki/Bivacco_Luigi_Pascal
ma temo troppo freddo per le batterie di un nodo autosufficiente. @GustavinoBevilacqua
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As a software engineer and engineering manager, I am mildly concerned for my employability in the future. However, I've had a good career, with much more luck than I deserve. People in my profession have been notably pampered and paid extremely well. As automation turns its Sauron-like eye to my own industry, it's hard to say with a straight face that we have been unfairly treated. I also think that there are, and will be for the foreseeable future, a lot of options for people who like to code.
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@GustavinoBevilacqua mia nonna ogni giorno mi mandava dal prestinaio a prendere le michette (lei lo diceva in milanese)
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I think that using LLMs to create text, images, video or code is an empowering technology for a lot of people. I think especially with code, it gives people who don't code and who've never had control over their computing experience more agency in their life and work. I think that's a net positive result.
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@davep That's OK, you don't have to.
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I generally don't like LLM-generated images or video. I mostly don't like LLM-generated text -- it's usually flat, wordy, and full of business jargon. I don't use LLMs for either of these things.
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Apollo 17: Boulder on the MoonCredits: E. Cernan, Apollo 17, #NASA#nature #space #astrophotography
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Depositi e flussi legati all’impatto presso il cratere Jijiga#marte @astronomiaL’obiettivo di questa immagine è osservare come i modelli di flusso superficiale nell’area varino con la distanza dal cratere d’origine proposto.
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