Anthropogenic nutrient loads and season variability drive high atmospheric N<sub>2</sub>O fluxes in a fragmented mangrove system.

Sci Rep · 2021 · PMC7994627 · PMID 33767286

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may not be significantno p-value reported

As the MCW is a fragmented mangrove, it’s atmospheric contribution of N 2 O calculated using Wanninkhof 15 is quite small (ranging from 1.1 ± 0.2 × 10 6 μmol day −1 during post-monsoon season to 2.4 ± 1.2 × 10 6 μmol day −1 during monsoon season) and on its own may not be significant.

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