Showing posts with label fictitious mean Sun. Show all posts
Showing posts with label fictitious mean Sun. Show all posts

Wednesday, November 2, 2016

How Did We Go From Astronomical To Atomic Time?



Me, standing astride the Greenwich meridian which separates the eastern and western hemispheres, in July, 1978.

A question that often comes up during astronomy lectures concerns astronomical time- keeping. Most educated people are at least aware that it's based on the motions of the Earth (rotation and revolution) with respect to the Sun.  For much of the past 150 years precision astronomical timekeeping has been carried out from the Royal Greenwich Observatory outside London. (See images above). This is also the venue through which the Prime Meridian (0 degrees longitude ) runs, separating the eastern and western hemispheres and which I had the honor of standing astride in July of 1978.  As we were informed by one specialist at the time, this is the location from which Greenwich Mean Time is measured and which clocks around the world have adopted.

First things first, A “time zone” is defined by taking the 360 degrees through which Earth rotates in one day, and dividing it by 24, since it requires 24 hours to make one revolution. Thus, one standard time zone would be generated via (360 deg/ 24 hr) = 15 deg/h or 15 degrees of longitude per hour - so be 15 degrees of longitude in expanse. Thus, time zones (calibrated per HOUR) were marked out by LONGITUDE differences.

Time zones don’t mean anything until referenced or calibrated to a fixed position-location, and that is the Greenwich Meridian, defined as 0 degrees longitude. All longitudes west of Greenwich mark time earlier – and all longitudes east of Greenwich mark times later. Thus, Berlin will always have a time later than London, and London will have a time later than New Orleans, just as Barbados will always have a time earlier than London and later than Miami.

The time difference is referenced to longitude difference for the various central meridians. For example, if London is at approximately 0 degrees longitude, and New Orleans is at 90 degrees west longitude, then New Orleans is earlier than London by (90 deg/ 15 deg/h) = 6 hours. If the time in London is noon local mean time, then it is 6 a.m. in New Orleans.

In order to solve the problem of different local mean times, Greenwich Mean Time or GMT was developed, so people could compare the same clock times around the world. GMT is based on a 24 hour clock defined at the Greenwich Meridian. So, for example, if one is listening to the BBC from New Orleans and the time given is 13h 30 m GMT, then that means it’s 1.30 p.m. LMT in London. Since New Orleans is 6 hours earlier, than that means it’s 7.30 a.m. local mean time in New Orleans.

Thus, knowing GMT, one can always work out the time at one’s location if one knows the longitude difference relative to Greenwich. (Note for the purposes here, I ‘m taking London as having the same longitude as Greenwich. It's actually off by a few thousand feet but negligible in terms of computations.)

In the above discussion the key thread is that timekeeping was a more or less sensible operation, meaning it could be related to an actual object (Sun) and its apparent motions as seen from Earth. The problem is that over the centuries that followed time keeping became ever more abstract and also more refined in the sense the increments got smaller (ultimately reaching the second defined as 1/86,400 th of the time from one noon to the next.

But this required the ultimate abstraction of the fictitious mean Sun.  What exactly is the fictitious mean Sun? What, for that matter, is the fictitious Sun? Basically, the former is that fictitious entity which is presumed to travel always at a uniform rate every hour and every day. This fictional creation enables us to fabricate "time zones" based on the fiction that the Earth turns uniformly through 360 degrees every 24 hours, hence through 15 degrees every hour.

By contrast, the fictitious Sun is not so regularized so its motion is erratic. This is also referenced to what we call "apparent solar time" or "sundial time".  Based on comparisons of the two, one can then compute what is called the "equation of time", see e.g.















The above concepts are, of course, idealizations. In truth, the Earth's rotation rate is not stable over time, hence the lengths of time - especially the second- will be affected. Every tide that strikes the beaches of the planet takes energy out of its spin, through the combined actions of Sun and Mon.

This is good to know because it set the stage for atomic time. Why atomic time? Well, because atoms are not affected by tides.  Thus it was near the middle of the last century physicists decided that the "second" needed revision. Indeed, the second was not the second at all (1/86, 400th of an Earth rotation) but instead was equivalent to 9.2 billion oscillations of a microwave beam when tuned to the frequency of a cesium atom. The clear advantage is that one no longer needed to look at the Sun to set clocks. Thus did Judah Levine announce at one global time conference:

"I have bad news for you, Britain. We are stealing the Greenwich meridian!"

Which brings us to the singular disadvantage of atomic time: It is no longer sensible in the way that solar time had been. While one could mark the passage of time from noon on one day to noon the next and multiply by 60 minutes per hour then by 60 seconds per minute - then take the reciprocal, how could one process - far less measure - 9.2 billion oscillations of a microwave beam when tuned to the frequency of a cesium atom?.

Never mind, the accuracy is needed given much of the world (especially in the financial- commercial arena) now requires sub-second accuracy. For example, for financial clients latency is crucial. This means the time elapsed between ordering a trade and when it actually happens. Even a two second delay in the flash trade sphere could mean millions lost for some high end users.  These typically make dozens or hundreds of trades per second so even a millisecond delay is critical.

Note again, atomic time is not a system that has or needs time zones. It works on Universal Coordinated Time, or effectively GMT applied to every location on Earth.  Since the accuracy of worldwide UT is governed by atomic clocks, there is no tolerance for such things as "leap seconds". For reference, a leap second was last added to electronic clocks at midnight universal time on Saturday, June 30, 2012, with atomic clocks reading 23 hours, 59 minutes and 60 seconds before then moving on to Greenwich Mean Time. (Other leap seconds were added in 2008, 2005 and 1998.)

The leap second is added in order to compensate for changes in Earth's rotation.  But the worry of the atomic time lords is that if we get a leap second wrong it could  lead to global financial catastrophe. For example, if Tokyo markets are out of synch with New York's for even a fraction of a second and thousands of trades are delayed. Or, more technically, let's say for a 2 second period it is not possible to distinguish UTs of 00:00:00 and 00:00: 00 the next time, i.e. after a leap second is added. Then the order of trades would be impossible to decipher.  As far as any financial regulators would be concerned, causality itself would be reversed.

But Britain's time managers say 'hogwash' to this. The Greenwich Observatory position was best stated by Peter Whibberley in 2013 after a failed conference in Geneva:: "Removing the leap second would not be a minor technical change, but rather a fundamental change. Ever since mechanical clocks were created we have always adjusted to model the rotation of the Earth."

But the atomic clock masters aren't buying it, and therein lies the conflict and the basis or failing to resolve the issue.

Former British science minister David Willets, however, is unrepentant about British intransigence. As he notes:

"If we just fixed time by the atomic clock it would, over centuries, diverge from time as measured by the rotation of the Earth. The Sun would then not be at its highest in the sky at noon. The (Prime) Meridian would no longer be at Greenwich but slowly heading towards Paris. Leap seconds allow us to keep the time of day linked to the rotation of the Earth even as it slows. The purists disapprove of this but we should not sever the link between time and the pattern of our lives on Earth."


I for one believe he makes a solid point. Already technological gizmos (see previous post) have majorly impacted social areas of our lives, wreaking havoc in many as they are unable to break free of the electronic social twitter tethers. Now add in disruptions of time perception, where one might look to see an estimate of the time - say by the Sun's altitude in the sky- and behold it is totally out of synch with one's quartz watch.   All this plays into the horrific picture painted by Morris Berman in his book, The Re-Enchantment of the World, portraying a grim time when humans have lost all connections to the natural world .

Do we really want this in the interest of efficiency? At least for the time being any changes regarding the leap second will be postponed until 2023 when the next time conference meets.






Sunday, July 1, 2012

Where Did That Extra Second Come From?

As most readers are probably aware, yesterday (Saturday) featured 86, 401 seconds rather than the usual 86, 400. One leap second was added to compensate for a slowing Earth rotation (actually - if factored in from 1972, 24 full seconds slower than at that time). A cutesy explanation (on ABC News) last night was that "just as humans slow down when they age so has the Earth." Well, yes...and no.

The actual physical reason has less to do with aging per se and more to do with what we call "tidal friction" resulting from the Moon's cumulative gravitational effects (part of which causes our spring and neap tides as well as regular tides on Earth). Over time those gravitational effects add up....and a leap second must be added to correct it.

Thus did the concept of Ephemeris time (ET) enter the picture and ET thereby became part of the lexicon of astronomers, and integrated within the specialized sub-discipline of astrometry. The job of astrometry is to keep careful quantitative track of any changes that would lead to time corrections, specially related to ET. This isn't so stirring an idea now, but a couple of centuries ago it was almost a given that the Earth's period of rotation about its axis was constant. (Apart from a slow secular increase due to tidal friction). 

Note that "secular changes" are essentially non-reversible, and hence proportional to time passed.

Meanwhile, the value of ET at a given instant is reckoned by extremely accurate observations of sudden variations in the longtiudes of Sun, Moon and planets which of course emanate from variations in Earth's rate of rotation. Hence, if I detect a rather sudden "jump" in the Sun's (heliographic) longitude - say during lengthy observations of a sunspot group, I can tie that in to variation in Earth's rotation. (Generally, however, such changes wouldn't occur that fast.)

To get into the nitty gritty, Simon Newcomb (1895) originally provided us with the detailed expression for the longitude of the Sun (cf. 'Spherical and Practical Astronomy Applied to Geodesy', p. 168):

L= 279 deg 41'48."04 + 129, 602, 768."13 t_e  + 1."089 t_e^2

where t_e is the length of the tropical century from the standard epoch. (Recall the 'tropical year' is the time taken by the fictitious Sun to make one passage between the mean Vernal equinox. Hence, a tropical century refers to 100 such passages.)

Now, differentiating the preceding with respect to time t_e,  the instantaneous rate of change of L per second of ET is obtained, viz.

dL/ dt_e  = 0."0410686389744 + 6."9017 x 10^-10t_e

The last factor featuring the 10 raised to the negative 10 power is an important marker. It allows us to estimate the frequency at which time corrections, say to Earth's rotation, need to be made. Thus, the equation shows us that to define Ephemeris time correctly to 1 part in 10^10 (or one part in ten billion) observations of the Moon are required over at least 5 years.

Another quantity that makes its way into such computations is the Right Ascension of the fictitious mean Sun;

RA = 18 h 38 m 45.s 836  = 8, 640, 184.s 542 t_e  =0.s 0929 t_e^2

What exactly is the fictitious mean Sun? What, for that matter, is the fictitious Sun (referenced earlier in connection with the tropical year, and century)? Basically, the former is that fictitious entity which is presumed to travel always at a uniform rate every hour and every day. This fictional creation enables us to fabricate "time zones" based on the fiction that the Earth turns uniformly through 360 degrees every 24 hours, hence through 15 degrees every hour. Hence, we set out longitude markers to reference the mean time for all locations, say within 15 degrees of longitude.

Hence, in regular standard time (not 'daylight saving') one has the time zone for the Greenwich meridian registering say 12 noon, then at a longitude of 15 deg W. the time is one hour earlier, and at 30 W two hours earlier, and so forth. All locations within the time zone agree (with few exceptions) to keep the same time.

By contrast, the fictititous Sun is not so regularized so its motion is erratic. This is also referenced to what we call "apparent solar time" or "sundial time".  Based on comparisons of the two, one can then compute what is called the "equation of time", see e.g.

http://brane-space.blogspot.com/2011/07/tackling-simple-astronmoyh-problems.html

Now, if we reckon Ephemeris time into the context of the "fictitious Suns" we will be using two key hour angles: h (the hour angle of the fictitious mean Sun) and h' (the ephemeris hour angle of the fictitious mean Sun. Based on this, Ephemeris time (ET) would be expressed:

ET = h + 12h

While the equation of time (EQN T) is:

EQN T =   h"   -  h'

where h" is the hour angle of the fictititous Sun.(Those who'd like to review hour angles and how to work them out can consult two earlier blogs:

http://brane-space.blogspot.com/2011/03/more-spherical-astronomy.html

and

http://brane-space.blogspot.com/2011/03/solutions-to-spherical-astronomy.html

I will also give here, without derivation (though I welcome energized readers attempting it using material from prior blogs) the relation between the corrected time delta T, Ephemeris time and Universal Time (UT):

delta T = ET - UT

Generally, delta T is computed - or at least used to be before the era of atomic clocks - through inverse interpolation in the ephemeris of the Sun, Moon & planets...and deducting the recorded UT time of observation. (Note: An 'Ephemeris' is a manual giving all the changing positions correlated with times, dates for celestial objects).

In the modern atomic clock -time epoch, things are (fortunately!) much more streamlined and we have powerful Cray and other supercomputers to boot. Basically, one associates the atomic time (AT) and Ephemeris time (ET) via the generic expression:

AT - ET = a + bt  + ct^2

where t denotes the time from the epoch when AT = ET + a

Hence, the coefficient 'a' determines the epoch of atomic time in relation to Ephemeris time. The coefficient 'b' is the division ratio adopted for the atomic resonator (as we know, different atomic clocks, e.g. cesium , quartz etc. have different frequencies, hence differing resonator rates). Finally, coefficient c is a cosmic constant which value may be 0 or more likely on the order of 0.s001 per year.

As we can see from the above considerations, for the most recent leap second correction:

ET - UT = 1 s  =  AT  - ET

Just be glad you only have to savor that extra second of time, not figure out when exactly you have to add it!