Summary
The delay times reported for 42,717,476 mantle and core phases in the ISC-EHB Bulletins for the years 1964-2018 are averaged into 12,041,671 summary rays. For each summary ray I estimate the standard variance of the mean delay and an upper bound for use in tomographic inversion. The trade-off between model norm and the fit to mantle P wave data shows that the regularized tomographic problem for these data is well posed, with data adequately fit between their error bounds.