Variations in continental water storage lead to loading deformation of the crust with typical peak-to-peak variations at very long baseline interferometry (VLBI) sites of 3–15 mm in the vertical component and 1–2 mm in the horizontal component. The hydrology signal at VLBI sites has annual and semi-annual components and clear interannual variations. We have calculated the hydrology loading series using mass loading distributions derived from the global land data assimilation system (GLDAS) hydrology model and alternatively from a global grid of equal-area gravity recovery and climate experiment (GRACE) mascons.
Eriksson, D., MacMillan, D. Continental hydrology loading observed by VLBI measurements,
Springer Berlin Heidelberg, 2014, с. 675-690.
Eriksson, D., MacMillan, D. .
Continental hydrology loading observed by VLBI measurements.
: Springer Berlin Heidelberg, 2014, с. 675-690.
Eriksson, D., MacMillan, D. (2014)
Continental hydrology loading observed by VLBI measurements,
: Springer Berlin Heidelberg, с. 675-690
Eriksson, D., & MacMillan, D.
(2014).
Continental hydrology loading observed by VLBI measurements. Journal of Geodesy. Springer Berlin Heidelberg 88 (7), с. 675-690.
