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Table 4 Chosen numerical values of the regularization parameters. The values are valid for all the models built in this paper insofar as the regularization terms are applicable to the specific model

From: Co-estimating geomagnetic field and calibration parameters: modeling Earth’s magnetic field with platform magnetometer data

Description of the model parameters

Regularization parameter

Internal field

Time-dependent

\(\lambda _t = {1.0}\,{\left( \frac{\hbox {nT}}{\hbox {yr}^{3}}\right) ^{-2}}\), \(\lambda _{t_\text {s}} = {0.03}\,{\left( \frac{\hbox {nT}}{\hbox{yr}^{2}}\right) ^{-2}}\), \(\lambda _{t_\text {e}} = {0.03}\,{\left( \frac{\hbox {nT}}{\hbox {yr}^{2}}\right) ^{-2}}\),

\(\lambda _{0} = 60\), \(\lambda _{m} = 0.65\)

External field

RC-baseline corrections

\(\lambda _{\text {ext}} = {4 \times 10^5}\,{\left (\frac{\hbox {nT}}{\hbox {yr}}\right )^{-2}}\)

\(\hbox {Calibration}^{1}\)

CryoSat-2 FGM1

\(\lambda _b = {9.1\times 10^2}\,{\left (\frac{\hbox {eu}}{\hbox {yr}}\right )^{-2}}\), \(\lambda _s = {9.1\times 10^{10}}\,{\left (\frac{\hbox {eu}}{\hbox {nTyr}}\right )^{-2}}\), \(\lambda _u = {2.8\times 10^2}\,{\left (\frac{1{}^{\circ }}{\hbox {yr}}\right )^{-2}}\)

CryoSat-2 FGM2

\(\lambda _b = {9.1\times 10^2}\,{\left (\frac{\hbox {eu}}{\hbox {yr}}\right )^{-2}}\), \(\lambda _s = {9.1\times 10^{10}}\,{\left (\frac{\hbox {eu}}{\hbox {nTyr}}\right )^{-2}}\), \(\lambda _u = {2.8\times 10^2}\,{\left (\frac{1{}^{\circ }}{\hbox {yr}}\right )^{-2}}\)

CryoSat-2 FGM3

\(\lambda _b = {9.1\times 10^2}\,{\left (\frac{\hbox {eu}}{\hbox {yr}}\right )^{-2}}\), \(\lambda _s ={9.1\times 10^{10}}\,{\left (\frac{\hbox {eu}}{\hbox {nTyr}}\right )^{-2}}\), \(\lambda _u ={2.8\times 10^2}\,{\left (\frac{1{}^{\circ }}{\hbox {yr}}\right )^{-2}}\)

GRACE-A

\(\lambda _b = {1.2\times 10^3}\,{\left (\frac{\hbox {eu}}{\hbox {yr}}\right )^{-2}}\), \(\lambda _s = {1.2\times 10^{13}}{\left (\frac{\hbox {eu}}{\hbox {nTyr}}\right )^{-2}}\), \(\lambda _u = {3.7\times 10^8}\,{\left (\frac{1{}^{\circ }}{\hbox {yr}}\right )^{-2}}\)

GRACE-B

\(\lambda _b = {1.2\times 10^3}\,{\left (\frac{\hbox {eu}}{\hbox {yr}}\right )^{-2}}\), \(\lambda _s = {1.2\times 10^{13}}\,{\left (\frac{\hbox {eu}}{\hbox {nTyr}}\right )^{-2}}\), \(\lambda _u = {3.6\times 10^8}\,{\left (\frac{1{}^{\circ }}{\hbox {yr}}\right )^{-2}}\)

  1. \(^{1}\) Not applicable to Model-A, which was not derived from platform magnetometer data