Additional file 2 of Azimuthal differences and changes in strain rate and stress of the Japanese Islands deduced from geophysical data

Additional file 2: Data S2. (e.g., 2005-2011diff.out) The comparative results of the strain rate and stress fields for the periods of 2005–2011 in Phase 1 and 2016–2019 in Phase 3. The first column of data represents the longitude of the grid point, the second does the latitude, the third does the optimized smoothing distance D [km], the fourth does the dilatational strain rate [nstrain/year], the fifth does the maximum shear strain rate [nstrain/year], the sixth does the azimuth of the maximum contraction of strain rate $${\tau }_{\mathrm{Hmax}}$$ τ Hmax [°], the seventh does the azimuth of the maximum compressive stress SHmax [°], the eighth does the number of earthquakes, and the ninth does the absolute difference between the azimuths of $${\tau }_{\mathrm{Hmax}}$$ τ Hmax and SHmax [°].