- online INP concentrations increased with wind speed
- offline INP concentrations did not
- INP activated fraction, morphology, and composition varied with wind speed
- seawater ice nucleation entities were stable over time; atmospheric INPs were driven by wind speed
- online INP concentrations increased with wind speed
- offline INP concentrations did not
- INP activated fraction, morphology, and composition varied with wind speed
- seawater ice nucleation entities were stable over time; atmospheric INPs were driven by wind speed