This manuscript presents a diagnostic study of whether the standard ACT DR6.02 daytime geographic split into Day-Side (DS) and Day-Night (DN) regions yields statistically interchangeable subsets for temperature (TT) power spectra and temperature-only CMB lensing ($\kappa\kappa$) reconstructions. Using PA6 maps at 90/150 GHz and a common pseudo–$C_\ell$ pipeline with four-way temporal jackknives, the authors compute DS and DN TT autospectra, DS$\times$DN TT cross-spectra (as a null test), and temperature-QE $\kappa\kappa$ autospectra and cross-spectra, focusing on 10 multipole bins ($\ell\approx 557$–$3625$) for the main 150 GHz DS/DN comparisons (Secs. 3–4, Appendix A). The headline empirical results are striking: DS TT power is strongly suppressed relative to DN (mean ratio $\sim0.3$) and DS$\times$DN TT cross-power is near-null; for lensing, DS $\kappa\kappa$ is systematically lower than DN (inverse-variance-weighted ratio $\langle R^\kappa\rangle \approx 0.85$) with an extremely large heuristic $\chi^2$ reported under the naive null (Secs. 4.1–4.2, Table 1). Additional checks (AA 90/150 GHz QE coherence, DS/DN vs AA cross-spectra, and a declination-based split on AA maps) suggest that the dramatic DS/DN behavior is not a generic artifact of arbitrary north–south masking (Secs. 4.3–4.5), and a gradient–$\kappa$ diagnostic indicates internally consistent small-scale structure in DS though it is not treated as a cosmological detection (Sec. 4.6). The paper is timely and potentially useful as a quality-control case study for daytime CMB analyses, but its impact and interpretability would be substantially improved by (i) a precise operational definition and quantitative characterization of DS/DN footprints and weights, (ii) a clearer accounting of calibration/beam/transfer-function/noise contributions to the extreme TT ratio, and (iii) more explicit description of what is (and is not) included in the $\kappa\kappa$ bandpowers and their uncertainties (Secs. 2–6).