There's a catch though: "subaerial" scenarios require feedstock molecules like HCN or CH2O at or close to the surface (at best from the atmosphere) to initiate prebiotic reactions. Unfortunately, these molecules are unstable in the modern, oxidised atmosphere of the Earth. See attached plot from Lichtenberg+ (2022, PPVII), showing the major atmospheric gases released from volcanoes for different interior compositions/chemical oxidation states. The Earth is too far right for stable HCN and CH2O.
This is what motivated the famous Miller-Urey experiment, but Miller-Urey atmospheres actually produce a lot of "goo" that makes the resulting soup unusable and unproductive. Currently suggested alternatives to produce chemically reduced feedstocks like HCN include lightning and meteoritic impact events. The idea for the impacts is that the iron in the impact vaporizes an already present ocean, which makes CH4, which then reacts with UV light to produce HCN. See attached figure from Benner+2020.