Abstract
Abstract
We present the construction of a two-state model of the atomic gravimeter and the associated Kalman recursion to estimate gravity acceleration from an atomic gravimeter. It is found that the Kalman estimator greatly improves the estimation precision in the short term by removing the white phase noise. The residual noise of the estimates follows
for more than
and highlights a precision of
at the measuring time of a single sample, even with no seismometer correction.
Funder
Scientific Research Project of the Educational Department of Liaoning Province
National Natural Science Foundation of China
Subject
General Physics and Astronomy