by zloq » Fri Dec 23, 2011 11:04 am
Well you seem to agree with my main point - that the moment of solstice is not defined as an extreme declination of the sun, but as a specific longitude along the ecliptic. One reason to do that is the motion of the sun is fairly steady in longitude, whereas when it is near an extreme point its behavior is dictated by higher order effects that would be hard to include accurately. A good example is the time of earliest sunset - which many people think happens on the winter solstice. But precisely because the sun is fairly stationary in dec. at that time, its changing apparent longitudinal speed is the dominant effect to determine sunset time - and the earliest sunset occurs many days earlier. At the top of a peak of a curve, highly magnified, it is completely flat - so even a slight perturbation could induce tilt at the main peak that has a big magnifying effect in laterally shifting the new peak.
As Meeus describes, an error of 1" in the solar longitude induces a 24s change in the time of a solstice. So - even if higher order effects (mainly due to the changing ecliptic latitude of the sun, which never exceeds 1.2") cause a tiny, sub arc-second change in declination, it can result in a relatively huge shift in longitude where that peak occurs - and therefore a big shift in time. It's not the *magnitude* of the shift that counts, but its rate of change, which causes a tilt of the top of the peak and offsets the lateral position of the new peak. I think these are all motivations to avoid defining events in terms of an extreme value - because the resulting time will be very sensitive to higher order effects.
As for 0.15" being "immeasurably" small - in many applications it is huge. Meeus points out that solstice is defined based on the unperturbed sun (including the effects of aberration and nutation), which ignores effects below 0.01". That is the level of simplification that is allowed in the definition that produced the time cited in the APOD caption. He also points out that even at the equinox, by the definition in use, the sun can be as far as 1.2" off the equator. But since the ecliptic is at an angle relative to the equator at the equinox, this has little impact on the time it crosses the equator, in contrast to the solstice where the sun is moving parallel to the equator.
I think it's good to know how these terms are defined - especially when the numbers are cited. If you say the number is based on one thing, and then you ask the person who did the calculation, who responds, "That's not what I did" - I think that's not good. The true definition of astronomical solstice is counter-intuitive - so when people speak of that moment as being a point of extreme declination - I can only assume they have never been exposed to the details spelled out by Meeus and the Astronomical Almanac. I just prefer to go by what something is rather than what it isn't.
I personally would have said the sun reaches its extreme point on the day of the solstice - to get the main idea across - and then separately talk about the moment of solstice and how it's defined. I enjoy learning about how these terms are actually defined - especially when they are somewhat surprising - and when there are in fact good reasons for them to be defined that way.
zloq
Well you seem to agree with my main point - that the moment of solstice is not defined as an extreme declination of the sun, but as a specific longitude along the ecliptic. One reason to do that is the motion of the sun is fairly steady in longitude, whereas when it is near an extreme point its behavior is dictated by higher order effects that would be hard to include accurately. A good example is the time of earliest sunset - which many people think happens on the winter solstice. But precisely because the sun is fairly stationary in dec. at that time, its changing apparent longitudinal speed is the dominant effect to determine sunset time - and the earliest sunset occurs many days earlier. At the top of a peak of a curve, highly magnified, it is completely flat - so even a slight perturbation could induce tilt at the main peak that has a big magnifying effect in laterally shifting the new peak.
As Meeus describes, an error of 1" in the solar longitude induces a 24s change in the time of a solstice. So - even if higher order effects (mainly due to the changing ecliptic latitude of the sun, which never exceeds 1.2") cause a tiny, sub arc-second change in declination, it can result in a relatively huge shift in longitude where that peak occurs - and therefore a big shift in time. It's not the *magnitude* of the shift that counts, but its rate of change, which causes a tilt of the top of the peak and offsets the lateral position of the new peak. I think these are all motivations to avoid defining events in terms of an extreme value - because the resulting time will be very sensitive to higher order effects.
As for 0.15" being "immeasurably" small - in many applications it is huge. Meeus points out that solstice is defined based on the unperturbed sun (including the effects of aberration and nutation), which ignores effects below 0.01". That is the level of simplification that is allowed in the definition that produced the time cited in the APOD caption. He also points out that even at the equinox, by the definition in use, the sun can be as far as 1.2" off the equator. But since the ecliptic is at an angle relative to the equator at the equinox, this has little impact on the time it crosses the equator, in contrast to the solstice where the sun is moving parallel to the equator.
I think it's good to know how these terms are defined - especially when the numbers are cited. If you say the number is based on one thing, and then you ask the person who did the calculation, who responds, "That's not what I did" - I think that's not good. The true definition of astronomical solstice is counter-intuitive - so when people speak of that moment as being a point of extreme declination - I can only assume they have never been exposed to the details spelled out by Meeus and the Astronomical Almanac. I just prefer to go by what something is rather than what it isn't.
I personally would have said the sun reaches its extreme point on the day of the solstice - to get the main idea across - and then separately talk about the moment of solstice and how it's defined. I enjoy learning about how these terms are actually defined - especially when they are somewhat surprising - and when there are in fact good reasons for them to be defined that way.
zloq