The Southern hemisphere is characterized by its sparsity of in situ atmospheric observations due to large ocean volumes and consequently limited landmass. Meteo-France maintains and operates meteorological measurement facilities at some of the French Sub Antarctic and Antarctic lands. The Southern Oceans weather forecasts benefits from those in situ facilities in combination with remote satellite data (ERA5 Reanalysis, 2017;Levy & Brown, 1991). This study discusses the measurement of atmospheric pressure perturbations and their variations. Those observations have shown to be valuable for studying both infrasound and gravity waves (Blanc et al., 2018;Hupe, 2019;Marlton et al., 2019). Such observations can be retrieved from microbarometer arrays that are part of the global International Monitoring System (IMS). The IMS is in place to verify the Comprehensive Nuclear-Test-Ban Treaty (CTBT; Marty, 2019), and globally monitors the infrasonic wavefield.Deep oceanic ambient noise is globally the most omnipresent seismic and infrasound source. The sea state describes the energy of the ocean surface and is the driving force for four different seismo-acoustic wave contributions (Figure 1a). (a) Evanescent microbaroms at the ocean-air interface are a direct product of traveling ocean surface waves, unregarded the water depth nor bathymetry, and decays vertically (Hetzer et al., 2010;Waxler & Gilbert, 2006). (b) The primary microseisms are related to a traveling ocean waves as well; however, these are only generated at the seafloor whenever the surface wave is in phase with the ocean bathymetry (Ardhuin et al., 2015). Non-linear interaction of counter traveling ocean surface waves results Abstract A method is introduced to reconstruct microbarom soundscapes in absolute values. The soundscapes are compared to remote infrasound recordings from infrasound array I23FR (Kerguelen Island) and in situ recordings by the INFRA-EAR, a biologger deployed near the Crozet Islands. The reconstruction method accounts for all-acoustic contributions, divided into evanescent microbaroms (detectable directly above the source) and propagating microbaroms (detectable over long ranges). It is computed by integrating acoustic intensities over the ocean surface, convolved with the transfer function quantifying the propagation losses and propagation time. The reconstructed soundscapes are found within 2.7 dB for 85% of the measurements in the microbarom band of 0.1-0.3 Hz. Infrasonic soundscapes are essential for understanding the ambient infrasonic noise field and are a basic need for applications, such as atmospheric remote sensing, natural hazard monitoring, and verification of the Comprehensive Nuclear-Test-Ban Treaty.Plain Language Summary Microbaroms are omnipresent sources of low-frequency, inaudible sound, that is, infrasound. They have a characteristic and continuous signature within the infrasound spectrum and are often classified as ambient noise. The microbarom signals can be divided into a direct signal, only detectable close by the sou...