Earlier quoted context omitted.
It will be easier to boost the Earth’s spin back to a 86,400-second day than to fix all the code.
It's been suggested that perhaps one way to find evidence of extrasolar life, would be to find exoplanets whose years are integer multiples of their rotational periods, i.e. they've done what you describe just to eliminate leap years and make their calendars easier.
Timeline of the far future
101–110 of 272 posts
Re: Timeline of the far future
#102In my opinion, this is the greatest threat to humanity of continuing to pump CO2 into the atmosphere.
Re: Timeline of the far future
#103Earlier quoted context omitted.
It's been suggested that perhaps one way to find evidence of extrasolar life, would be to find exoplanets whose years are integer multiples of their rotational periods, i.e. they've done what you describe just to eliminate leap years and make their calendars easier.
But how do we know which base number system they're using!?
Re: Timeline of the far future
#104My all-time favorite wikipedia article, great to see it getting some attention. I find that along with providing great fodder for small-talk (among certain types), it causes me to experience a psychological effect analogous to the so-called "overview effect" experienced by astronauts. Attempting to conceive of one's place in cosmological time is great exercise.
Re: Timeline of the far future
#105Re: Timeline of the far future
#106Can someone explain: > 800 million Carbon dioxide levels fall to the point at which C4 photosynthesis is no longer possible.[57] Without plant life to recycle oxygen in the atmosphere, free oxygen and the ozone layer will disappear from the atmosphere. All multicellular life will die out.[58]
The general idea, I believe, is that the carbonate-silicate cycle will shift more toward carbonates over time. The Earth will warm substantially as the sun's luminosity increases over millions of years. Warmer conditions will accelerate the reaction of water and carbon dioxide with silicate minerals like magnesium and calcium silicates, shifting the equilibrium to favor more carbon-as-insoluble-carbonate and less carbon-as-available-CO2. Plant life will eventually go extinct from insufficient atmospheric CO2. I haven't spotted a discussion of oxygen loss in either citation 57 or 58. But "just" losing plant life would be enough to drive the extinction of most other multicellular life on Earth.
https://en.wikipedia.org/wiki/Carbonate%E2%80%93silicate_cyc...
Re: Timeline of the far future
#107Can someone explain: > 800 million Carbon dioxide levels fall to the point at which C4 photosynthesis is no longer possible.[57] Without plant life to recycle oxygen in the atmosphere, free oxygen and the ozone layer will disappear from the atmosphere. All multicellular life will die out.[58]
Re: Timeline of the far future
#108Wow, I'd love to be able to see that. Makes one sad about all the things they'll never get to experience.
Re: Timeline of the far future
#109Earlier quoted context omitted.
It will be easier to boost the Earth’s spin back to a 86,400-second day than to fix all the code.
It's been suggested that perhaps one way to find evidence of extrasolar life, would be to find exoplanets whose years are integer multiples of their rotational periods, i.e. they've done what you describe just to eliminate leap years and make their calendars easier.