Southern Ocean Cloud and Aerosol data set: a compilation of measurements from the 2018 Southern Ocean Ross Sea Marine Ecosystems and Environment voyage

• Main Authors: Kremser, Stefanie, Harvey, Mike, Kuma, Peter, Hartery, Sean, Saint-Macary, Alexia, McGregor, John, Schuddeboom, Alex, von Hobe, Marc, Lennartz, Sinikka T., Geddes, Alex, Querel, Richard, McDonald, Adrian, Peltola, Maija, Sellegri, Karine, Silber, Israel, Law, Cliff, Flynn, Connor J., Marriner, Andrew, Hill, Thomas C.J., DeMott, Paul J., Hume, Carson C., Plank, Graeme, Graham, Geoffrey, Parsons, Simon
• Format: Dataset
• Language: English
• Published: 2020
• Subjects: aerosol; clouds; ship-based measurements; in situ measurements; remote sensing measurements; New Zealand; Ross Sea; Southern Ocean; Antarc*; Antarctica
• Online Access: https://zenodo.org/record/4060237; https://doi.org/10.5281/zenodo.4060237

Due to its remote location and extreme weather conditions, atmospheric in situ measurements are rare in the Southern Ocean. As a result, aerosol-cloud interactions in this region are poorly understood and remain a major source of uncertainty in climate models. This, in turn, contributes substantially to persistent biases in climate model simulations, numerical weather prediction models and reanalyses. It has been shown in previous studies that in situ and ground-based remote sensing measurements across the Southern Ocean are critical for complementing satellite data sets due to the importance of boundary layer and low-level cloud processes. These processes are poorly sampled by satellite-based measurements which are typically obscured by near-continuous overlying cloud cover observed in this region. Here we provide a comprehensive set of ship-based aerosol and meteorological observations collected on the TAN1802 voyage of R/V Tangaroa across the Southern Ocean, from Wellington, New Zealand, to the Ross Sea, Antarctica. The voyage was carried out from 8 February to 21 March, 2018. The compiled data set provides here includes measurements from a range of instruments, such as (i) meteorological conditions at the sea surface and profile measurements; (ii) the size and concentration of particles; (iii) trace gases dissolved in the ocean surface such as dimethyl sulfide and carbonyl sulfide; (iv) and remotely sensed observations of low clouds. We encourage the scientific community to use these measurements for further analysis and model evaluation studies, in particular, for studies of Southern Ocean clouds, aerosol and their interaction.