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. 2022 Mar 17;127(6):e2021JD036059. doi: 10.1029/2021JD036059

Figure 4.

Figure 4

The ice‐active site density (n s) for aerosol sampled during the cruise (see Figure 2 for key to colors) compared to n s parameterisations for desert dust (Ullrich et al., 2017), Icelandic dust (Sanchez‐Marroquin et al., 2020) and for aerosol from the North Atlantic (McCluskey, Ovadnevaite, et al., 2018), which is also consistent with values for aerosol over the Southern Ocean (McCluskey, Hill, et al., 2018).