Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue
The new Earth Orientation Catalogue was recently derived, based mostly on the ARIHIP and Tycho-2 Catalogues that were combined with ground-based optical observations of latitude and Universal Time variations in the 20th century. The solution of Earth orientation parameters, based on this new star ca...
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| Цитувати: | Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue / J., Ron C. Vondrak // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 305-310. — Бібліогр.: 15 назв. — англ. |
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Vondrak, J. Ron, C. 2015-04-03T18:10:23Z 2015-04-03T18:10:23Z 2005 Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue / J., Ron C. Vondrak // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 305-310. — Бібліогр.: 15 назв. — англ. 0233-7665 https://nasplib.isofts.kiev.ua/handle/123456789/79664 The new Earth Orientation Catalogue was recently derived, based mostly on the ARIHIP and Tycho-2 Catalogues that were combined with ground-based optical observations of latitude and Universal Time variations in the 20th century. The solution of Earth orientation parameters, based on this new star catalogue and the new IAU model of precession-nutation, is presented. This study was supported by grant No. IAA3003205, awarded by the Grant Agency of the Academy of Sciences of the Czech Republic. en Головна астрономічна обсерваторія НАН України Кинематика и физика небесных тел MS4: Positional Astronomy and Global Geodynamics Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue Article published earlier |
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Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue |
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Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue Vondrak, J. Ron, C. MS4: Positional Astronomy and Global Geodynamics |
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Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue |
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Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue |
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Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue |
| title_full_unstemmed |
Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue |
| title_sort |
solution of earth orientation parameters in the frame of new earth orientation catalogue |
| author |
Vondrak, J. Ron, C. |
| author_facet |
Vondrak, J. Ron, C. |
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MS4: Positional Astronomy and Global Geodynamics |
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MS4: Positional Astronomy and Global Geodynamics |
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2005 |
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English |
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Кинематика и физика небесных тел |
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Головна астрономічна обсерваторія НАН України |
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Article |
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The new Earth Orientation Catalogue was recently derived, based mostly on the ARIHIP and Tycho-2 Catalogues that were combined with ground-based optical observations of latitude and Universal Time variations in the 20th century. The solution of Earth orientation parameters, based on this new star catalogue and the new IAU model of precession-nutation, is presented.
|
| issn |
0233-7665 |
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https://nasplib.isofts.kiev.ua/handle/123456789/79664 |
| citation_txt |
Solution of Earth orientation parameters in the frame of new Earth orientation Catalogue / J., Ron C. Vondrak // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 305-310. — Бібліогр.: 15 назв. — англ. |
| work_keys_str_mv |
AT vondrakj solutionofearthorientationparametersintheframeofnewearthorientationcatalogue AT ronc solutionofearthorientationparametersintheframeofnewearthorientationcatalogue |
| first_indexed |
2025-11-24T05:51:33Z |
| last_indexed |
2025-11-24T05:51:33Z |
| _version_ |
1850842886792282112 |
| fulltext |
SOLUTION OF EARTH ORIENTATION PARAMETERS
IN THE FRAME OF NEW EARTH ORIENTATION CATALOGUE
J. Vondrák, C. Ron
Astronomical Institute, Academy of Sciences of the Czech Republic
Bočńı II, 141 31 Prague 4, Czech Republic
e-mail: vondrak@ig.cas.cz
The new Earth Orientation Catalogue was recently derived, based mostly on the ARIHIP and
Tycho-2 Catalogues that were combined with ground-based optical observations of latitude and
Universal Time variations in the 20th century. The solution of Earth orientation parameters, based
on this new star catalogue and the new IAU model of precession-nutation, is presented.
INTRODUCTION
We produced, in the past years, several solutions of Earth Orientation Parameters (EOP) in the frame of
the Hipparcos Catalogue [2] that were based on optical astrometry observations of latitude / Universal Time
variations made at up to 33 observatories in the years 1899.7–1992.0. All of them were referred to the “old” IAU
1976 precession [5] and IAU 1980 nutation [14] models. Three solutions, that differed in number of instruments,
slightly different criteria for correcting positions / proper motions, and also in methods of merging observations
with different instruments into series, were made (where OA stands for Optical Astrometry):
• OA97 [12] that was based on observations made with 45 different instruments located at 31 observatories.
4.32 million individual observations in 48 series were used, and applied corrections to 11% of positions
and / or proper motions of the observed Hipparcos stars.
• OA99 [13] that was based on observations made with 47 instruments at 33 observatories. 4.45 million
observations in 39 series were used, and 20% of positions and/ or proper motions of the observed stars
were corrected.
• OA00 [7] that was based on observations made with 47 instruments at 33 observatories. 4.45 million
observations in 41 series were used, and 20% of star positions and / or proper motions were corrected.
The reason why these corrections (mostly for double and multiple star systems) had to be applied was threefold:
Firstly, the real motions of the observed objects are not linear – the reference point that was observed (either
a component or a photocenter) exhibits, in addition to the linear drift, also a small periodic motion.
Secondly, the Hipparcos mission was shorter than four years, i.e., usually much shorter that the orbital
periods. As a result, the linear proper motion derived from Hipparcos observations is rather a tangential
motion near the epoch of the Hipparcos mission (1991.25) than the mean motion over a longer time span
(decades) that is required for deriving Earth orientation parameters. So, even if the amplitude of the periodic
part is negligible, the extrapolated star’s position can have big error.
Thirdly, it was sometimes not quite clear which object was observed: a component of a double star or
its photocenter? This reference point was often different from the object listed in the Hipparcos Catalogue,
and sometimes even different for different types of instruments (visual, photographic, photoelectric). Usually,
the human eye proved to be a better detector than photography or photoelectric device, capable of distinguishing
much closer objects.
After these solutions were finished, several new star catalogues appeared as combination of Hipparcos /Tycho
positions with ground-based catalogues with a much longer observational history. The result is the catalogues
with much more reliable proper motions. The most important ones are Tycho-2 [3] (the combination of the Tycho
Catalogue with additional 144 ground-based astrometric catalogues), and ARIHIP [15] (selection of the best
stars from other combined catalogues FK6, GC+HIP, Tycho-2+HIP and Hipparcos itself). We decided to
make use of these catalogues, and to combine them further with the rich observational material collected in
Earth rotation programmes during the whole 20th century (latitude / Universal Time variations). The goal
c© J. Vondrák, C. Ron, 2004
305
is to get a better and more stable celestial reference frame for long-period Earth rotation studies [10]. Thus,
the idea of constructing the Earth Orientation Catalogue (EOC), containing all stars observed in Earth rotation
programmes, appeared. A more detailed description of the combined catalogues, including EOC, can be found
in [9]. Here follows an abbreviated outline of deriving the EOC.
CONSTRUCTION OF THE NEW EOC CATALOGUE
The idea is to use the observed data made by optical astrometry in Earth rotation programmes (instantaneous
latitude /Universal Time / altitude difference) to improve the catalogue positions and proper motions. We have
collected the data with 47 instruments located at 33 observatories, covering the interval 1899.7–2003.0. They
can be divided into three groups according to the observables that they provide:
1. 10 Photographic Zenith Tubes that measured simultaneously latitude and Universal Time (3 at Washing-
ton, DC; 2 at Richmond, Florida and Mizusawa, Japan; 1 at Mount Stromlo, Australia; Punta Indio,
Argentina; Ondřejov, Czech Republic).
2. 7 Photoelectric Transit Instruments that measured only Universal Time (3 at Pulkovo and 1 at Irkutsk,
Russia; Kharkiv and Mykolaiv, Ukraine; Wuhang, China).
3. 16 Visual Zenith-Telescopes and similar instruments that measured only latitude (7 Visual Zenith-Teles-
copes at International Latitude Service stations – Carloforte, Italy; Cincinnati, Ohio; Gaithersburg, Vir-
ginia; Kitab, Uzbekistan; Mizusawa, Japan; Tschardjui, Turkmenistan; Ukiah, California; 2 at Poltava,
Ukraine; 1 at Belgrade, Serbia; Blagoveshchensk, Irkutsk, and Pulkovo, Russia; Józefoslaw, Poland; Float-
ing Zenith Telescope at Mizusawa, Japan; Visual Zenith Tube at Tuorla-Turku, Finland).
4. 14 instruments for equal altitude method that measured the differences of stars’ altitude, i.e., the combina-
tion of latitude and Universal Time (Danjon astrolabes at Paris, France; Santiago de Chile; Shanghai and
Wuhang, China; Simeiz, Ukraine; 2 photoelectric astrolabes at Shaanxi, China; photoelectric astrolabes
at Beijing, Shanghai, Yunnan, China, and Grasse, France; circumzenithals at Bratislava, Slovakia; Prague
and Ondřejov, Czech Republic).
The inspection of all observations made with these instruments showed that there were 4418 different objects
observed (stars, double star components, photocenters). They were identified in different recent catalogues, and
their positions, proper motions, parallaxes, and radial velocities taken over from them. Not all of them were
found in the best one, ARIHIP, – we also had to use less precise Tycho-2, and the rest were found in the Hipparcos
and PPM Catalogues [1, 8]. ARIHIP uses three types of solution, with slightly different positions / proper
motions: single-star mode, short-term prediction mode and long-term prediction mode. To construct EOC, we
used a “classical” single-star mode. The statistics is as follows:
2995 objects were taken over from ARIHIP, 1248 from Tycho-2, 144 from Hipparcos, and 28 from PPM;
3 objects were found in none of the above catalogues, and therefore, their initial entries were taken over from
the catalogues used at the respective observatories. These entries formed the zero version of the catalogue,
so-called EOC-0.
The authors of ARIHIP introduced a classification of “astrometrical excellency” of each star – the number
of asterisks (the larger is the number, the more reliable the position / proper motion). The stars with no
asterisk are most probably double or multiple systems. There are 56% of such “non-excellent” stars in EOC-0
(including those originating from other catalogues than ARIHIP), so further improvement is still necessary and
possible. Taking into account the number of observations and number of different objects observed, each of
them was observed about a thousand times during long time interval, with precision of one observation of about
0.2′′. It means that proper motions can be determined with precision competing with recent catalogues, and
the combination with EOC-0 should bring a significant improvement.
The positions and proper motions were first improved by means of combining EOC-0 with the observations
made in local meridian (i.e., with only the first three groups of instruments shown above). This version,
containing only 3784 objects, was denominated EOC-1 and described in detail in [11].
In further improvement of the catalogue we used all available observations (i.e., made with all four groups
of instruments mentioned above) to determine relative positions of all stars with respect to those denoted as
astrometrically excellent. The strategy, assuming that the latitude /Universal Time is constant only during
a night, was chosen. Consequently, the method used was practically insensitive to any change of the terrestrial
coordinates of the instruments during the time. We proceeded by following these steps:
1. The instantaneous observables (i.e., latitude /Universal Time / altitude difference) were transformed from
original observations, using the entries from EOC-0 and the new model of precession-nutation IAU2000A [6].
306
2. The deviations of these observables from the mean value of the night (calculated for astrometrically
excellent stars only) were computed, and linear regression for these differences for the same star in different
epochs was made.
3. Stars with statistically significant deviations were checked for multiplicity, using the information contained
in the Hipparcos Catalogue. In positive case, the displacement of reference point from EOC-0 was esti-
mated, and the respective position in EOC-0 was corrected. In this case, the procedure above (item 2)
was repeated.
4. Combination of these deviations with EOC-0 was made. To this end, each entry of the star of the EOC-0
catalogue was represented by three virtual observations (of both right ascension and declination) in three
epochs covering one century: t1 = t◦−90, t2 = t◦, t3 = t◦+10, where t◦ is the mean epoch of the catalogue.
The values of these “observations” were implicitly set to zero. Their uncertainties were then calculated
from catalogue standard errors of the position σ◦ and proper motion σμ as
σ2
1 = 9000σ2
μ, σ2
2 = σ2
◦/
[
1 − (σ◦/σμ)2/900
]
, σ2
3 = 1000σ2
μ (1)
that would reproduce exactly the catalogue entry if subject to linear regression. These values were then
used to calculate the weights pi = (200/σi)2, if σi are given in milliarcseconds; all real observations
(deviations calculated above) were assigned the weights 1. Then the weighted linear regression through
all real and virtual observations was made to yield the combined position / proper motion. To this end,
we used the following observation equations for the three types of observations (latitude ϕ, Universal
Time UT, altitude h), respectively:
vϕ = Δδ + Δμδ(t− t◦) − δϕ,
vUT = Δα∗ + Δμ∗
α(t− t◦) − 15.041δUTcosϕ, (2)
vh = Δα∗ sin q + Δμ∗
α(t− t◦) sin q + Δδ cos q + Δμδ(t− t◦) cos q − δh.
Here Δα∗, Δμ∗
α stand for Δα cos δ, Δμα cos δ, and q is the parallactic angle of the star. First two of Eqs. (2)
are used for virtual observations of declination and right ascension with their weights, respectively, and
they are mixed with any of the three equations for real observations, according to their type.
An illustrative example of combining declination is shown in Fig. 1; the observations at all ILS stations
and the Floating Zenith Telescope at Mizusawa (MZL) are combined with Tycho-2 entry for star No. 36366,
represented by three virtual observations whose weights are also depicted in the figure.
year - 1900
)*
0 10 20 30 40 50 60 70 80 90 100
-2.5
-1.5
-0.5
0.5
1.5
2.5
ILS MZL
12
2377
111
Figure 1. Tycho-2 star No. 36366: observations at all ILS stations and Mizusawa FZT (MZL, crosses), virtual observa-
tions (open circles with weights) and combined position (full line)
The combination leads to the catalogue version EOC-2; the comparison of its standard errors (median
values) with the Hipparcos is given in Table 1. A substantial improvement, especially of proper motions, is
obvious.
307
Table 1. Comparison of accuracy of EOC-2 with Hipparcos
Catalogue No. Epα − 1900 σ∗
α σ∗
μα Epδ − 1900 σδ σμδ
[mas] [mas/yr] [mas] [mas/yr]
Hipparcos 117995 91.25 0.87 0.72 91.25 1.02 0.85
EOC-2 4418 91.16 0.70 0.47 91.03 0.60 0.35
NEW SOLUTION OF EOP IN THE FRAME OF EOC-2
The new solution of EOP consists in using virtually the same data as were used to improve the catalogue, but
we did not go beyond 1992.0, when the number of active observatories and number of observations decreased
substantially. The series of observations with 47 instruments were merged in cases when the instruments of
similar type worked at the same observatory. The steps between them were estimated and removed beforehand.
Namely, we merged the observations with the following instruments into a single series: the visual zenith-
telescope and FZT at Mizusawa, Japan; two PZT’s at Mizusawa, Japan; two zenith-telescopes at Poltava,
Ukraine; three photoelectric transit instruments at Pulkovo, Russia; two PZT’s at Richmond, Florida; two
PZT’s at Washington, DC. On the other hand, the visual zenith-telescope at Pulkovo, Russia was treated as
two different series, due to a long gap in the observations (and change of the instrument’s position) during
the second world war. The same holds for circumzenithal in Prague, Czech Republic, that was moved to
a distant location, and was treated as two different series. Thus, the total number of series used was 42.
We followed more or less the same procedures as in our preceding solutions, with two exceptions:
1. New IAU2000A model of precession-nutation was used, which led to much smaller values of celestial pole
offsets, and consequently
2. celestial pole offsets were represented by a constant plus linear trend for both coordinates, not by five-
day individual points as before, in order to decrease the number of estimated parameters, and to make
the solution more robust.
The results of the solution, so-called OA04, are depicted in Figures 2 (polar motion) and 3 (Universal Time,
only after 1956.0) for each five-day interval, where their mean errors σ are also shown. The latter are given in
x
F
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
0
0.1
0.2
0.3
0.4
0.5
0.6
y
F
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990
-0.4
-0.2
0.0
0.2
0.4
0.6
0.8
0
0.1
0.2
0.3
0.4
0.5
0.6
Figure 2. Polar motion of the solution OA04 (in arcseconds)
308
F
1955
1960
1965
1970
1975
1980
1985
1990
-0.200
-0.150
-0.100
-0.050 0
0.050
0.100
0.150
0.200
0 0.002
0.004
0.006
0.008
0.010
0.012
0.014
0.016
F
igure
3.
R
ed
u
ced
U
n
iv
ersa
l
T
im
e
va
ria
tio
n
s
o
f
th
e
so
lu
tio
n
O
A
0
4
(in
seco
n
d
s
o
f
tim
e)
enlarged
scales
–
tw
o
tim
es
larger
than
the
results
for
polar
m
otion,25-tim
es
larger
for
U
niversalT
im
e.
Instead
of
U
T
1–T
A
I,
the
reduced
values
U
T
1–T
A
X
(w
ith
long-periodic
part
rem
oved,
in
order
to
show
the
variations
in
m
ore
detail)
are
depicted.
T
he
relation
betw
een
T
A
I
and
T
A
X
is
given
(in
seconds
of
tim
e)
by
the
form
ula
T
A
X
=
T
A
I+
2
.63−
0
.002047
t−
0
.236×
10 −
7t
2
+
0
.49×
10 −
1
2t
3−
0
.17
cos(2
π
t/6000)
+
0
.26
sin
(2
π
t/6000)−
1
.32
cos(2
π
t/9000)+
0
.16
sin
(2
π
t/9000),
(3)
w
here
t
=
M
JD
−
35300.
T
he
form
ula
w
as
selected
so
that
the
difference
U
T
1–T
A
X
never
exceeds
0.2
s
in
the
interval1956.0–1992.0.
T
he
resulting
celestialpole
offsets
(in
m
illiarcseconds)
are
given
as
Δ
ψ
sin
ε
=
−
5
.7±
0
.3
2
+
28
.5±
1
.0
8 T
,
Δ
ε
=
−
5
.5±
0
.3
2
+
6
.7±
1
.0
7 T
,
(4)
w
here
T
is
given
in
centuries
since
1956.0.
T
hese
values
represent
a
sum
of
a
bias
betw
een
IC
R
S
and
the
new
E
O
C
catalogue
w
ith
the
correction
of
the
new
IA
U
precession.
T
hey
are
very
sm
all,
and
are
quite
com
parable
w
ith
the
form
aluncertainties
of
the
link
betw
een
the
H
ipparcos
(to
w
hich
E
O
C
is
linked)
and
IC
R
S
(±
0
.6
m
as
at
the
epoch
1991.25
and
±
25
m
as/cyr
in
rotation,according
to
[4]).
C
O
N
C
L
U
S
IO
N
S
T
he
new
star
E
O
C
catalogue
(given
in
the
IC
R
S)
w
as
constructed,using
about
4.5
m
illion
individualobserva-
tions
oflatitude
/
U
niversalT
im
e
/
altitude
difference,in
com
bination
w
ith
recentcataloguessuch
as
the
A
R
IH
IP
or
T
ycho-2.
V
ersion
E
O
C
-2
of
the
catalogue,
in
w
hich
m
any
double
stars
w
ere
detected
and
their
posi-
tions/
proper
m
otions
referred
to
their
reference
points
(either
double
star
com
ponents
or
photocenters)
is
m
ore
accurate
and
stable
in
long-periodic
sense
than
the
original
catalogues
based
on
the
H
ipparcos
m
ission
(H
ipparcos,
T
ycho,
A
R
IH
IP
,
...
).
T
he
catalogue
is
used
in
the
new
solution
of
E
arth
orientation
param
eters
from
optical
astrom
etry
in
the
interval
1899.7–1992.0.
T
he
present
solution,
O
A
04,
has
a
better
precision
of
five-day
values
than
our
preceding
solutions
based
on
the
H
ipparcos,
w
hich
is
dem
onstrated
by
the
statistics
show
n
in
T
able
2.
T
able
2.
C
o
m
p
a
riso
n
o
f
so
m
e
ch
a
ra
cteristics
o
f
th
e
so
lu
tio
n
O
A
0
4
w
ith
O
A
0
0
S
o
lu
tio
n
n
o
b
s
n
p
a
r
a
m
σ◦
σ
x
σ
y
σ
U
T
1
[ ′′]
[m
a
s]
[m
a
s]
[m
s]
O
A
0
0
4
4
4
7
4
0
0
2
9
8
0
9
0
.1
8
8
2
0
.5
1
8
.3
0
.8
7
O
A
0
4
4
5
3
8
6
9
4
1
6
4
4
3
0
.1
9
0
1
7
.4
1
5
.7
0
.7
2
T
hanks
to
the
better
star
catalogue,m
ore
observations
(n
o
bs )
could
be
used
in
the
solution
O
A
04
than
before,
because
less
observations
w
ere
rejected
due
to
large
residuals.
T
he
num
ber
of
estim
ated
param
eters
(n
p
a
r
a
m
)
309
decreased, because a better precession-nutation model was used, and it became unnecessary to estimate five-
day values of celestial pole offsets. Thus, the solution is made more robust. Although the mean error of one
observation (σ◦) slightly increased, the median mean errors of the unknowns representing five-day values of pole
position and Universal Time (σx, σy, σUT1) decreased substantially, by almost 20%.
Acknowledgements. This study was supported by grant No. IAA3003205, awarded by the Grant Agency of
the Academy of Sciences of the Czech Republic.
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