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. 2023 Sep 4;16(9):768–774. doi: 10.1038/s41561-023-01254-8

Extended Data Table 2.

Cloud occurrence and changes in cloud microphysical and longwave radiative properties attributed to the blowing-snow-produced sea salt aerosols

graphic file with name 41561_2023_1254_Tab2_ESM.jpg

The monthly mean values of cloud occurrence at the MOSAiC location are based on remote sensing measurements. The changes in cloud droplet number concentration (CDNC) and cloud effective radius (re) are based on model simulations. The longwave (LW) downwelling radiation flux at the MOSAiC location and in the Arctic region (north of 80 °N and 60 °N) attributed to the blowing-snow-produced SSA is derived from the changes in re and measured liquid water path (LWP).