Integral transformations of gravitational gradients onto a Gravity Recovery And Climate Experiment (GRACE) type of observable are derived in this article. The gravitational gradients represent components of the gravitational tensor in the local north-oriented frame. The GRACE type of observable corresponds to a difference between two gravitational vectors as projected onto the line of sight between the two GRACE satellites. In total, three integral transformations relating vertical–vertical, vertical–horizontal and horizontal–horizontal gravitational gradients with the GRACE type of observable are provided.
Sprlak, M., Novak, P. Integral transformations of gradiometric data onto a GRACE type of observable,
Springer Berlin Heidelberg, 2014, с. 377-390.
Sprlak, M., Novak, P. .
Integral transformations of gradiometric data onto a GRACE type of observable.
: Springer Berlin Heidelberg, 2014, с. 377-390.
Sprlak, M., Novak, P. (2014)
Integral transformations of gradiometric data onto a GRACE type of observable,
: Springer Berlin Heidelberg, с. 377-390
Sprlak, M., & Novak, P.
(2014).
Integral transformations of gradiometric data onto a GRACE type of observable. Journal of Geodesy. Springer Berlin Heidelberg 88 (4), с. 377-390.
