Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6383184 | Continental Shelf Research | 2014 | 16 Pages |
Abstract
Analysis of the terms used in the PNP equation indicate that both NO3 drawdown rates (mean=13.25±9.57 mmol mâ2 dâ1, N=156) and NO3 flux into the euphotic layer (mean=1.36±1.79 mmol mâ2 dâ1, N=156) have high temporal and spatial variability. NO3 drawdown rates were higher than NO3 flux into the control volume by approximately an order of magnitude. Sensitivity analyses of the model using two extreme values of Kz, (10â4 and 10â5 m sâ2) that are widely reported in the literature for the WAP region, yielded a PNP range of 97.13 mg C mâ2 dâ1. The latter accounted for approximately 10% of the overall computed PNP. PNP estimates for the coastal sub-region which includes Marguerite Bay agreed well with estimates of nPP from north Marguerite Bay in a recent study which employed different datasets and research approach.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Marco Pedulli, James J. Bisagni, Hugh W. Ducklow, Robert Beardsley, Cynthia Pilskaln,