Numerical modelling of the shelf break ecosystem: reproducing benthic and pelagic measurements

A coupled pelagic-benthic biogeochemical model, embedded in a turbulence-cl osure formulation is employed for the Goban Spur shelf-break area (northeas t Atlantic). Our main objectives are to examine the impact of in situ atmos pheric conditions on ecosystem dynamics, to reproduce biogeochemical distri butions in the water column and the sediments, and to derive a nitrogen bud get for the area. Given a data set of atmospheric forcing conditions at 3-h intervals, the model successfully explains the time evolution of the tempe rature field. Most biochemical water column properties are reasonably well simulated, both in timing and in magnitude. Some of the short-term variabil ity, apparent in the data, can be reproduced, suggesting that this may resu lt from variability in the in situ atmospheric forcing. In summer, intermit tent mixing events generate increased ammonium and nitrate concentrations i n the upper water column, consistent with observations. These short-term nu trient injections substantially increase euphotic zone production, mainly b y stimulating new production. The model also reproduces a set of benthic nu trient profiles, measured on two occasions, both qualitatively and quantita tively. The results suggest that there is a significant variability in bent hic properties. A tentative nitrogen budget for the Goban Spur shelf break area is proposed . The sediments account for about 7% of organic nitrogen respiration; about 42% occurs in the euphotic zone, and the remaining 50% takes place in the water column below the euphotic zone. About 3% of the annual primary produc tion of organic nitrogen is denitrified in the sediments and is replenished from lateral sources in the model. Nitrification mainly takes place in the water column below the euphotic zone (66%); sedimentary nitrification and ammonium oxidation in the euphotic zone both account for 17%. Over the year , only 55% of euphotic zone nitrogen assimilation is based on the in situ r egenerated inorganic nitrogen, the remainder is mainly supplied by mixing f rom below the euphotic zone, either in the form of nitrate (72%) or ammoniu m (28%). The implications of these nitrogen pathways in the euphotic zone o n the measured f-ratio are discussed. (C) 2001 Elsevier Science Ltd. All ri ghts reserved.