04 Apr '06 13:16>1 edit
Originally posted by sonhousePrior to 1956 the second was indeed defined in terms of the rotation of the Earth: it was 1/86,400 th of a mean solar day. Now, not every solar day is 86400 seconds long (they can be as short as 86378s or as long as 86429s), but the mean was calculated from nearly 150 years' data.
The seconds in a year are usually this: 86,400 (seconds in one day)
times 365.26 and that gives 31558464 seconds in a year. But is that the actual #? Can you get it down to milli or microseconds? I think it has been proven the earth speeds down and slows up a bit but how many days in a year? I can't believe its known only to 5 digit accuracy.
By 1956 it was recognised that the Earth's rotation was not a constant enough clock and so the second was re-defined in terms of the earth's rotation around the Sun:
1 second = 1/31,556,925.9747th of the tropical year for 1900 January 0 at 12 hours ephemeris time.
By 1967, however, the invention of the atomic clock meant that even this value was not accurate enough and the second was redfined to be:
1 second = the duration of 9,192,631,770 periods of the radiation corresponding to the transition between the two hyperfine levels of the ground state of the caesium-133 atom.
At this point the connection between time and astronomical events was broken. It is no longer meaningful to ask exactly how many seconds in a year, because each year will be different. There is no longer an exact ratio between seconds and days or seconds and years - the current mean solar day is 86,400.002 s for instance and increasing at 1.7 ms/century.
If you wanted to "time" a year say then the accuracy would not be limited by the clock used but rather the accuracy of your atronomical observation. If for instance you use "noon" as a datum; how accurately can you determine the time at which the Sun is at its highest elevation? I doubt that an accuracy better than 1/100th is possible.