1997Chinese Journal of GeophysicsRequires access

STUDIES ON A METHOD FOR DETERMINING THE PRECISE GRAVIMETER PHASE LAG

X Zhang

Open publisher page 0 citations

Abstract

Since the 1980s, global earth models based on seisndc and free oscillation datahave predict 0°-0.02° phase lag corresponding to about 0- 2 s time lag for tidalwaves at the earth's surface' In principle, phases from earth tide observations couldhelp to verify the global earth models or to constrain the adustment of these modelsif the phases of earth tide observations corrected would be accurate to much betterthan 0'02 ° . For this purpose, it is important to deterndne the phase lag of the pre-cise gravimeter' ACCording to system identification principle, a method fordeterndning the phase lag of the precise gravimeter is given in this paPer' As anexample, the method was used to detendne the phases lag of the ET-2l and it wasshown that the phases lag angle t0 be relative to l5 main tidal waves individually'

About this research paper

What this paper is about

Since the 1980s, global earth models based on seisndc and free oscillation datahave predict 0°-0.02° phase lag corresponding to about 0- 2 s time lag for tidalwaves at the earth's surface' In principle, phases from earth tide observations couldhelp to verify the global earth models or to constrain the adustment of these modelsif the phases of earth tide observations corrected would be accurate to much betterthan 0'02 ° . For this purpose, it is important to deterndne the phase lag of the pre-cise gravimeter' ACCording to system identification principle, a method fordeterndning the phase lag of the precise gravimeter is given in this paPer' As anexample, the method was used to detendne the phases lag of the ET-2l and it wasshown that the phases lag angle t0 be relative to l5 main tidal waves individually'

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Since the 1980s, global earth models based on seisndc and free oscillation datahave predict 0°-0.02° phase lag corresponding to about 0- 2 s time lag for tidalwaves at the earth's surface' In principle, phases from earth tide observations couldhelp to verify the global earth models or to constrain the adustment of these modelsif the phases of earth tide observations corrected would be accurate to much betterthan 0'02 ° . For this purpose, it is important to deterndne the phase lag of the pre-cise gravimeter' ACCording to system identification principle, a method fordeterndning the phase lag of the precise gravimeter is given in this paPer' As anexample, the method was used to detendne the phases lag of the ET-2l and it wasshown that the phases lag angle t0 be relative to l5 main tidal waves individually'

Key concepts: Gravimeter, Lag, Phase lag, Geodesy, Time lag, Phase (matter), Geology, Oscillation (cell signaling)

Related papers

Back to paper searchBrowse research topicsOriginal source
STUDIES ON A METHOD FOR DETERMINING THE PRECISE GRAVIMETER PHASE LAG — Research Paper | ScholarLens