Quantifying the time lag between organic matter production and export in the surface ocean: Implications for estimates of export efficiency
The ocean's potential to export carbon to depth partly depends on the fraction of primary production (PP) sinking out of the euphotic zone (i.e., the e‐ratio). Measurements of PP and export flux are often performed simultaneously in the field, although there is a temporal delay between those pa...
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Veröffentlicht in: | Geophysical research letters 2017-01, Vol.44 (1), p.268-276 |
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