Fig. 8From: Temperature correction and usefulness of ocean bottom pressure data from cabled seafloor observatories around Japan for analyses of tsunamis, ocean tides, and low-frequency geophysical phenomenaTime series of uncorrected KPG2 (black), corrected KPG2 with the zero-lag regression coefficient (green), NMS09 (blue), and KCTD (red), respectively, at a frequency of lower than 0.5 day−1. The KCTD data include a loss interval around a day of 260.Back to article page