A set of 11 aerosol turbidity profiles (ATP) and 2 aerosol extinction profiles (AEP) at λ = 0.55 µm, observed with searchlight in New Mexico at 32° N, has been digitized from plots in scientific articles. They cover the period February to June 1963 and September 1965 to May 1975, complementing the already rescued and previously published 105 individual AEP, corresponding to 36 days, between December 1963 and December 1964. Eleven AEP are calculated (AEP<sub>c</sub>) from the ATP, and the corresponding stratospheric aerosol optical depth (sAOD) between 12 and 25 km is also derived. Estimates of the digitization’s errors for the AEP<sub>c</sub> and the sAOD are also calculated using information available in the literature. The combined set of rescued AEP reported here and the earlier rescued set of AEP from searchlight observations, are the only AEP dataset covering the period between the 1963 Mt Agung and the 1974 Fuego eruptions at northern midlatitudes. In this regard two relevant features identified in the AEP and the sAOD are described here. The first, using AEP<sub>c</sub> from March and April 1963 identified what could be the date of arrival of the stratospheric aerosols from the Mt. Agung first eruption on March 17<sup>th</sup> 1963. This fact challenges the accepted criteria that the arrival of the stratospheric aerosols from Mt Agung arrived at the northern hemisphere midlatitudes in the second half of 1963. The second feature evidences two anomalous increases of the sAOD during a period supposed to be the decay of the sAOD from Mt. Agung eruption. They show our limited knowledge and understanding of the 1963 Mt Agung volcanic stratospheric aerosol transport. Finally, we describe evidences found in the literature pointing to the possible existence of the original searchlight raw signals and its processing software. The dataset described in this work is available at: <a href="https://issues.pangaea.de/browse/PDI-43217" target="_blank" rel="noopener">https://issues.pangaea.de/browse/PDI-43217</a>, (Antuña-Marrero et al., 2026).