“…Since the basic components of microscopic and macroscopic oil‐sediment residues are the same (oil and sediment), it is reasonable to expect that the variables that affect the formation of microscopic aggregates would also affect macroscopic agglomerate formation, albeit not necessarily to the same extent. For example, there have been several studies on how mixing energy affects the rate and degree of OPA formation (Ma et al, ; Payne et al, ; Sun et al, , ); however, beyond the conceptual idea that breaking waves facilitate SOA and SOM formation, there is no consensus in the macroscopic community about how more turbulent nearshore environments might affect macroscopic agglomerate formation. Similarly, several studies have been carried out to understand how the likelihood of OPA formation differs for different types of oils (Gustitus et al, ; Guyomarch et al, ; Kepkay et al, ; Khelifa et al, ; Omotoso et al, ; Sørensen et al, ; Stoffyn‐Egli & Lee, ); however, the macroscopic community has not carried out any such controlled studies, although it could be assumed that oil qualities such as density, polarity, and viscosity would have a significant impact on macroscopic agglomerate formation.…”