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3'1' Coordinatesystems and time' Seeber 2'1'

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Zero-meridian for Bureau Internationale de l' Heure (BHI) determined so that ... Polbev gelse, 1994-1997, Fuld linie : middel pol bev gelse, 1900-1996. 7. Kap. ... – PowerPoint PPT presentation

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Title: 3'1' Coordinatesystems and time' Seeber 2'1'


1
3.1. Coordinate-systems and time. Seeber 2.1.
Z
NON INERTIAL SYSTEM
Mean-rotationaxis 1900.
Gravity-centre
Y- Rotates with the Earth
CTS Conventional Terrestrial System
Greenwich
X
2
CIS
  • Zero-meridian for Bureau Internationale de l
    Heure (BHI) determined so that star-catalogues
    agree in the mean with observations from
    astronomical observatories.
  • The connection to an Inertial System is
    determined using knowledge of the Z-axís (Polar
    motion), rotational velocity and the movement of
    the Earth Center.
  • We obtain an Quasi-Inertial system, CIS.
  • More correct to use the Sun or the centre of our
    galaxe !

3
Kap. 3 POLAR MOTION
  • Approximatively circular
  • Period 430 days (Chandler period)
  • Main reason Axis of Inertia does not co-inside
    with axis of rotation.
  • Rigid Earth 305 days Euler-period.

4
Ch. 3 POLBEVÆGELSEN
  • .

5
Kap. 3 POLAR MOVEMENT
  • Coordinates for the Polen and Rotational velocity
  • IERS (http//www.iers.org)
  • International Earth Rotation and Reference System
    service (IAG IAU)
  • http//aiuws.unibe.ch/code/erp_pp.gif
  • Metods
  • VLBI (Radio astronomi)
  • LLR (Laser ranging to the Moon)
  • SLR (Satellite Laser ranging)
  • GPS, DORIS

6
Kap. 3
  • Polbevægelse, 1994-1997, Fuld linie middel pol
    bevægelse, 1900-1996

7
Kap. 3. International Terrestrial Reference
System (ITRS)
  • Defined, realised and controlled by IERS ITRS
    Center. http//www.iers.org/iers/products/itrs/
  • Geocentric, mass-centre from total Earth
    inclusive oceans and atmosphere.
  • IERS Reference Pole (IRP) and Reference Meridian
    (IRM) konsist with BIH directions within /-
    0.005".

8
Kap. 3, ITRS.
  • Time-wise change of the orientations secured
    through 0-rotation-condition taking into account
    horizontal tectonic movements for the whole
    Earth.
  • ITRS realised from estimate of coordinates for
    set of station with observations of VLBI, LLR,
    GPS, SLR, and DORIS. See ftp//lareg.ensg.ign.fr/
    pub/itrf/old/itrf92.ssc

9
Kap. 3
  • Paris, 1 July 2003
    Bulletin C 26
  • INFORMATION ON UTC -
    TAI
  • NO positive leap second will be introduced at
    the end of December 2003.
  • The difference between UTC and the International
    Atomic Time TAI is
  • from 1999 January 1, 0h UTC, until further
    notice UTC-TAI -32 s
  • Leap seconds can be introduced in UTC at the end
    of the months of December or June, depending on
    the evolution of UT1-TAI. Bulletin C is mailed
    every six months, either to announce a time step
    in UTC, or to confirm that there will be no time
    step at the next possible date.
  • http//www.iers.org/iers/products/eop/leap_second.
    html

10
Kap. 3

11
Kap. 3 Variationer jord-rotationen.
12
Kap. 3
13
Ch. 3, Transformation CIS - CTS
  • Precession
  • Nutation
  • Rotation
  • Polar movement

SunMoon
14
Ch. 3, Precession.
  • Example t-t00.01 (2001-01-01)
  • .

15
Ch. 3, Nutation primarily related to the
Moon.
  • Movement takes place in Ecliptica

16
Ch. 3, Nutation
  • .

17
Ch. 3, Earth rotation and polar motion (ERP).
  • .

18
Ch. 3, Example for point on Equator.
  • Suppose ?0, xpyp 1 (30 m)
  • .

19
Ch. 3,
Exercise.
  • 2 May 1994
  • x0.18430.000000893,
  • y0.33090.0000014651
  • (x,y,z)(3513648.63m,778953.56m,5248202.81m)
  • Compute changes to coordinates.

20
Ch. 3, Time requirement
  • 1 cm at Equator is 210-5 s in rotation
  • 1 cm in satellite movement is 10-6 s
  • 1 cm in distance measurement is 310-11 s
  • We must measure better than these quantities.
  • Not absolute, but time-differences.

21
Ch. 3, Siderial time and UT. (see fig. 2.13).
  • Siderial time Hour-angle of vernal equinox in
    relationship to the observing instrument
  • LAST Local apparent siderial time true hour
    angle
  • GAST LAST for Greenwich
  • LMST Local hour angle of mean equinox
  • GMST LMST for Greenwich
  • GMST-GAST??cose
  • LMST-GMSTLAST-GAST?

xp
22
Ch. 3, UT
  • UT 12 hours Greenwich hourangle for the mean
    sun. Follows siderial time.
  • 1 mean siderial day 1 mean solar day
    -3m55.909s.
  • UT0B is time at observation point B, must be
    referred to conventional pole
  • UT1 UT0B ??P

23
Ch. 3, UT1, GMST and MJD
  • .

24
Ch. 3, Dynamic time
  • ET Ephemeis time (1952) to make equatins of
    motion OK.
  • TDB Barycentric time refers to the Sun
  • TDTTerrestrial time
  • From general relativity clock at the earth
    moving around the sun varies 0.0016 s due to
    change in potential of sun (Earth does not move
    with constant velocity).
  • TDBET on 1984-01-01

25
Ch. 3, GPS Time
  • GPS time UTC 1980-01-05
  • Determined from Clocks in GPS satellites
  • GPS time UTC n s-C0,
  • C0 about 300 ns

26
Ch. 3, Clocks and frequency standards.
  • With GPS we count cycles. Expect the fequency to
    be constant.

27
Ch. 3, Praxis, see Seeber, Fig. 2.15.
  • Precision quarts crystal temperature dependent,
    aging
  • Rubidium good stability, long term
  • Cesium stable both on short term and long term
    transportable, commercially available.
  • Hydrogen masers 10-15 stability in periods of
    102 to 105 s.
  • Pulsars period e.g. 1.6 ms.
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