“…Geostationary satellite infrared radiance (GeoIR) observations, for instance, are usually assimilated with horizontal densities of less than one observation per 100 km 2 (ECMWF, 2016a). In contrast, applications of GeoIR in mesoscale DA generally assimilate GeoIR with horizontal densities greater than one observation per 30 km 2 (Chan & Chen, 2021; Chan, Zhang, et al., 2020; F. Zhang et al., 2016; Hartman et al., 2021; Honda, Miyoshi, et al., 2018; Minamide & Zhang, 2018; Okamoto et al., 2019; Otkin & Potthast, 2019; Sawada et al., 2019a, 2019b; Y. Zhang, Stensrud, et al., 2019; Y. Zhang et al., 2018). Creating an accurate tropical MCS analysis data set thus requires addressing these model‐ and observation‐related issues.…”