“…In addition to latitude and longitude, several bathymetric and oceanographic parameters were used to generate the DSM (Table 1) and were selected on the basis of their potential to influence sperm whale distribution and their availability for the whole survey area. These parameters have been linked to sperm whale distribution in other studies, and included depth (Cañadas et al, 2005;Pirotta et al, 2011;Mannocci et al, 2017b;Pace et al, 2018;Pirotta et al, 2020), slope (Cañadas et al, 2005;Praca and Gannier, 2008;Pirotta et al, 2011;Pirotta et al, 2020), aspect (Pirotta et al, 2011;Pirotta et al, 2020), SST (Cañadas et al, 2005;Praca and Gannier, 2008;Pirotta et al, 2011;Pirotta et al, 2020), chlorophyll (Jaquet et al, 1996;Praca and Gannier, 2008;Mannocci et al, 2017b), distance to isobath (including 0, 200 and 1,000 m; Praca and Gannier, 2008;Pace et al, 2018;Sahri et al, 2020;Avila et al, 2022), distance to bathymetric features (such as canyons, escarpments, ridges, seamounts, shelves, slopes, terraces and troughs; Mannocci et al, 2017b;Sahri et al, 2020;Vachon et al, 2022), mixed layer thickness (Avila et al, 2022) and local currents (Vachon et al, 2022). Dynamic oceanographic parameters, such as SST, chlorophyll, depth of mixed layer and water speed/direction, can vary at timescales from seconds to decades.…”