From: Hydrology signal from GRACE gravity data in the Nelson River basin, Canada: a comparison of two approaches
\(\sigma _{\frac{{\mathrm {d}}g _{\mathrm{grace}}}{{\mathrm {d}} t}}\)
F
\(\sigma _{F}\)
\(v^{2}\)
\(\sigma _{v}\)
\(\sigma _{\frac{{\mathrm {d}} g}{{\mathrm {d}} t}}\)
Lambert et al. (2013a, b)
0.073
0.1436
0.012
23.16
0.1
0.094
Wang et al. (2013)
0.100
0.1586
0
0.101