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Ice-nucleating particles (INPs) in the troposphere can form ice in clouds via heterogeneous ice nucleation. Yet, atmospheric number concentrations of INPs (N-INP) are not well characterized, and, although there is some understanding of their sources, it is still unclear to what extend different sources contribute or if all sources are known. In this work, we examined properties of INPs at Cabo Verde (a.k.a. Cape Verde) from different environmental compartments: the oceanic sea surface microlayer (SML), underlying water (ULW), cloud water and the atmosphere close to both sea level and cloud level.

Both enrichment and depletion of N-INP in SML compared to ULW were observed. The enrichment factor (EF) varied from roughly 0.4 to 11, and there was no clear trend in EF with ice-nucleation temperature.

N-INP values in PM10 sampled at Cape Verde Atmospheric Observatory (CVAO) at any particular ice-nucleation temperature spanned around 1 order of magnitude below -15 degrees C, and about 2 orders of magnitude at warmer temperatures (> -12 degrees C). Among the 17 PM10 samples at CVAO, three PM10 filters showed elevated N-INP at warm temperatures, e.g., above 0.01 L-1 at -10 degrees C. After heating samples at 95 degrees C for 1 h, the elevated N-INP at the warm temperatures disappeared, indicating that these highly ice active INPs were most likely biological particles.

INP number concentrations in PM1 were generally lower than those in PM10 at CVAO. About 83 +/- 22 %, 67 +/- 18% and 77 +/- 14% (median +/- standard deviation) of INPs had a diameter > 1 mu m at ice-nucleation temperatures of -12, -15 and -18 degrees C, respectively. PM1 at CVAO did not show such elevated N-INP at warm temperatures. Consequently, the difference in N-INP between PM1 and PM10 at CVAO suggests that biological ice-active particles were present in the supermicron size range.

N-INP in PM10 at CVAO was found to be similar to that on Monte Verde (MV, at 744ma.s.l.) during noncloud events. During cloud events, most INPs on MV were activated to cloud droplets. When highly ice active particles were present in PM10 filters at CVAO, they were not observed in PM10 filters on MV but in cloud water samples instead. This is direct evidence that these INPs, which are likely biological, are activated to cloud droplets during cloud events.

For the observed air masses, atmospheric N-INP values in air fit well to the concentrations observed in cloud water. When comparing concentrations of both sea salt and INPs in both seawater and PM10 filters, it can be concluded that sea spray aerosol (SSA) only contributed a minor fraction to the atmospheric N-INP. This latter conclusion still holds when accounting for an enrichment of organic carbon in supermicron particles during sea spray generation as reported in literature.