We really only have two measurements of time based on physical events: the time it takes the Earth to complete a revolution on its axis (the day) and the time it takes the Earth to complete a revolution around the sun (the year). The rest—minutes, weeks, months—are subdivisions to make our lives easier to keep track of (months were originally derived from the motion of the moon, but as anyone who watches moon cycles knows, they don't sync up).
Our day is exactly twenty-four hours long. Our year, on the other hand, is just shy of 365.25 days. In a regular calendar year, we simply ignore that quarter day and go about our business. If we were to do that forever, eventually our calendar would be so far behind that the seasons would appear in the wrong months. So to catch up to the difference, every four years we add the previous three years' quarters to the current year's quarter to make a whole day that we tack on to the shortest month—February 29th.
Now, remember I said our year was just shy of 365.25 days? It's actually 365.24, but we use 365 and a quarter because that's close enough to work over the course of four years. Over the course of a hundred years, though, that difference adds up. If we simplify the math, we find that after 100 years, because of that .01 days we've been ignoring, we come out nearly a day ahead. So every 100 years we skip the leap day to catch back up again.
And if that weren't enough for you (and you're still reading), there are even more digits following that .24 that keep it from working out to an even number that cause our calendar to wobble slightly off its track. Suffice to say, every 400 years, we add the day back in to readjust. After that, we throw up our hands and leave it to the astronomers to figure out.
Five amazing, clean technologies that will set us free, in this month's energy-focused issue. Also: how to build a better bomb detector, the robotic toys that are raising your children, a human catapult, the world's smallest arcade, and much more.