EarthRef.org Reference Database (ERR)
Development and Maintenance by the EarthRef.org Database Team

Detailed Reference Information
Rautenberg et al. 1997
Rautenberg, V., Plag, H., Burns, M., Stedman, G.E. and Jüttner, H. (1997). Tidally induced Sagnac signal in a ring laser. Geophysical Research Letters 24: doi: 10.1029/97GL00760. issn: 0094-8276.

The Earth rotation vector is an integral dynamical quantity of the Earth system, with Earth rotation variations depending on the overall dynamics of the Earth system at all time scales. New observations of Earth rotation variations with a precision better than 10-9 of the Earth rotation would contribute to the understanding of many geophysical phenomena. High precision short-term observations of the projection of the Earth rotation vector &OHgr;E on the area vector A of a ring laser are now possible. Tidally induced Sagnac effects are due to changes in the ring geometry (areal strain and perimeter variations), changes in the normal vector of the ring laser plane (tilt), and the vorticity of the Earth's tidal deformations. Here we estimate the latitude-dependent effect of the Earth's body tide deformations due to vorticity and tilt. At mid-latitudes, the vorticity Δ&OHgr; is of the order 8⋅10-8&OHgr;E, but because it is in the local horizontal plane, it is not detectable by a horizontal ring. The Sagnac effect due to tidal tilt for a horizontal ring at mid-latitudes is of the order of 4⋅10-8 of the Earth rotation effect. Thus, the tidal signal is of an order of magnitude where it may be used for validation of existing and future ring lasers.¿ 1997 American Geophysical Union

BACKGROUND DATA FILES

Abstract

Keywords
Geodesy and Gravity, Rotational variations, Geodesy and Gravity, Tides—Earth
Journal
Geophysical Research Letters
http://www.agu.org/journals/gl/
Publisher
American Geophysical Union
2000 Florida Avenue N.W.
Washington, D.C. 20009-1277
USA
1-202-462-6900
1-202-328-0566
service@agu.org
Click to clear formClick to return to previous pageClick to submit