The porosity of a sea ice pressure ridge keel is an important but poorly known variable relevant for determining the mass budget and evolution of the Arctic sea ice cover. Determination of keel porosity from drillholes is time-intensive and only yields limited information because of their limited lateral extent. Since the porosity within a keel equals its liquid water content, surface-nuclear magnetic resonance (surface-NMR) methods can be used to estimate porosity within such features. Surface-NMR tomography measurements were made in April 2011 using seven surface coil positions across a first-year pressure ridge on landfast sea ice near Barrow, Alaska. The inversion results indicate water contents of 30 ± 7 % and 40 ± 10 % in the ridge's shallow and deep parts, respectively. These values are much higher than those obtained from drillholes, which are ~10 % and ~27 %, respectively. In contrast to drilling, surface-NMR tomography yields average porosity values for the entire subsurface volume. However, the inversion process is sensitive to the electrical conductivity distribution; uncertain conductivity estimates limit the reliability of the inverted water contents. Nevertheless, the results suggest that ridge porosities obtained from invasive measurements such as drilling may lead to substantially overestimated sea ice volume.