Accuracy and precision of helicopter electromagnetic (HEM) sounding are the essential parameters for HEM sea-ice thickness profiling. For sea-ice thickness research, the quality of HEM ice thickness estimates must be better than ![]()
ath mml" alt="Formula" src="F127/embed/mml-math-1.gif" /> to detect potential climatologic thickness changes. We introduce and assess a direct, 1D HEM data inversion algorithm for estimating sea-ice thickness. For synthetic quality assessment, an analytically determined HEM sea-ice thickness sensitivity is used to derive precision and accuracy. Precision is related directly to random, instrumental noise, although accuracy is defined by systematic bias arising from the data processing algorithm. For the in-phase component of the HEM response, sensitivity increases with frequency and coil spacing, but decreases with flying height. For small-scale HEM instruments used in sea-ice thickness surveys, instrumental noise must not exceed ![]()
ath mml" alt="Formula" src="F127/embed/mml-math-2.gif" /> to reach ice thickness precision of ![]()
ath mml" alt="Formula" src="F127/embed/mml-math-3.gif" /> at 15-m nominal flying height. Comparable precision is yielded at 30-m height for conventional exploration HEM systems with bigger coil spacings. Accuracy losses caused by approximations made for the direct inversion are negligible for brackish water and remain better than ![]()
ath mml" alt="Formula" src="F127/embed/mml-math-4.gif" /> for saline water. Synthetic precision and accuracy estimates are verified with drill-hole validated field data from East Antarctica, where HEM-derived level-ice thickness agrees with drilling results to within 4%, or ![]()
ath mml" alt="Formula" src="F127/embed/mml-math-5.gif" />.
