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On direct passive microwave remote sensing of sea spray aerosol production

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Academic year: 2017

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Table 1. Similar to Fig. 8, the table shows sea spray aerosol surface flux dF/d ln(r dry ) as a func- func-tion of dry radius r dry and brightness temperature polarization difference ∆T B
Figure 3. Snapshot of surface winds output from COAMPS on Year Day 118, 20:00 UTC. Two panels represent a wider view of the Northeastern Pacific and a zoomed in view around the FLIP track, shown with the black line.

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