Absolute and Relative gravity Measurements in Qaqortoq (Greenland) in August 2007

To obtain the gravity value, a linear equation representing the equation of motion is fit to the raw data including the gravity gradient which has been measured with

The gravity site is located in the building of the Department of Low-Frequency Mechanical Motion Quantities, Gravimetry and Angle Metrology (Figure 3).. Inside the building (Figure

To obtain the gravity value, a linear equation representing the equation of motion is fit to the raw data including the gravity gradient that was measured with a

The vertical gravity gradient was measured with the relative spring gravimeter Scintrex CG5 from the University of Luxembourg at the absolute gravity stations.. This gradient is

The Vertical Gravity Gradient (VGG) is needed to linearize the equation of motion but also to transfer the measured absolute gravity value from the reference height around 1.38 m

Though elastic rheology has limitations, this model- ing offers interesting results on what gravity signal can be expected from the AGTO project (Absolute Gravity in the

Now, we can use the absolute gravity measurement value obtained at the station 00001 in 2013 to deduce the gravity values at the other stations (Table 3).. Gravity values at

From these measured gravity differences and the absolute gravity measurements of the FG5X-216 made at the same epoch, we estimated the gravity values as well as their