The kinetic coefficient of friction mu(k) was measured for sea ice, stainless steel, and coated steel sliding on a natural sea ice cover. The effects of normal stress (3.10-8.11 kPa), ice columnar grain orientation (vertical and parallel to the sliding direction), sliding velocity (0.02-2.97 m.s(-1)), and contact material were investigated. Air temperature was higher than -5.0 degrees C for the test duration. The results showed a decline of mu(k) with increasing normal stress with mu(k) independent of ice grain orientation. The mu(k) of different materials varied, partly due to distinct surface roughnesses, but all cases showed a similar increasing trend with increasing velocity because of the viscous resistance of melt-water film. The velocity dependence of mu(k) was quantified using the rate- and state-dependent model, and mu(k) was found to increase logarithmically with increasing velocity. In addition, mu(k) obtained at higher air temperatures was greater than at lower temperatures. The stick-slip phenomenon was observed at a relatively high velocity compared with previous studies, which was partly due to the low-stiffness device used in the field. Based on the experimental data, the calculation of physical models can be compared.