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Influence of mesoscale eddies on the distribution of nitrous oxide in the eastern tropical South Pacific

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Academic year: 2017

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Figure 1. Map of sampling locations in the ETSP. Aviso sea level height anomaly for 21 November 2012 is shown (anticyclonic  ed-dies are depicted in red, and cyclonic in blue)
Figure 2. Hydrographic conditions at the time of sampling in the ETSP (0-600 m depth)
Figure 3. Vertical of distribution of N 2 O and O 2 across the mode water eddies A (a–b) and B (d–e), and the cyclonic eddy C (g–h) during the M90 cruise in November 2012
Figure 5. Vertical distribution of N 2 O and O 2 concentrations (a), as well as gene abundance of amoA (b), nirS (c), and hzo (d) within the centre (solid lines) and outside (dashed lines) of eddy A in  De-cember 2012 (M91 cruise)
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