Sentence examples for changes in the gravity from inspiring English sources

The same mass redistribution causes temporal changes in the gravity field coefficients with the second degree harmonics related to the rotational deformation and hence to changes in the Earth's inertial tensor.

Fig. 7 Example of monthly changes in the gravity as equivalent water thickness and the earthquake number from April 2002.

The mesospheric residual mean circulation could be intensified by changes in the gravity wave drag, thus causing a negative temperature trend in the summer polar mesosphere.

Furthermore, gobs(t) increases quickly by a few microgals during precipitation events, in line with the soil moisture increase and water height rise (as seen for March 2009, October 2009, March 2010 and July 2010), suggesting that changes in the gravity signal are associated with corresponding changes in the land-water distribution.

They try to explain this discrepancy by the effect of long-term changes in the gravity wave flux in the thermosphere initiated by a shift in climate regime in oceans in 1976/77, which launched a slow Rossby wave across oceans that continues to propagate until present.

Here, in the light of "phase" of the annual gravity change, which may reflect the surface load effect on seismicity, we show monthly changes in the gravity as equivalent water thickness and the earthquake number from April 2002, at a grid of (longitude, latitude) = (275°, 5°) and at an adjacent grid of (longitude, latitude) = (275°, − 5°), in Fig. 7.

Gravity is perceived in the bundle sheath cells, which contain amyloplasts that sediment to the new cell base when a change in the gravity vector occurs.

Note that a positive change in the output voltage corresponds to a negative change in the gravity for the SG.

This implies that the mean-squared horizontal displacements of the sphere are proportional to the apparent change in the gravity acceleration.

The change in the gravity acceleration is given by Delta g = - Delta a_{z} = frac{g}{2}left( {frac{{beta_{text{H}} mg}}{{alpha_{text{H}}^{2} }} - 1} right)varphi^{2} (19).

Experimentally, the change in the gravity output (Delta g) depends quadratically on the tilt angle, and thus, Delta g = cvarphi^{2} (13 where (varphi) is the deviation angle from the optimal orientation and (c) is a constant.