Abstract
Abstract. Oxygen depletion in coastal and estuarine waters has been increasing rapidly around the globe over the past several decades, leading to decline in water quality and ecological health. In this study we apply a numerical model to understand how salt wedge dynamics, changes in river flow and temperature together control oxygen depletion in a micro-tidal riverine estuary, the Yarra River estuary, Australia. Coupled physical–biogeochemical models have been previously applied to study how hydrodynamics impact upon seasonal hypoxia; however, their application to relatively shallow, narrow riverine estuaries with highly transient patterns of river inputs and sporadic periods of oxygen depletion has remained challenging, largely due to difficulty in accurately simulating salt wedge dynamics in morphologically complex areas. In this study we overcome this issue through application of a flexible mesh 3-D hydrodynamic–biogeochemical model in order to predict the extent of salt wedge intrusion and consequent patterns of oxygen depletion. The extent of the salt wedge responded quickly to the sporadic riverine flows, with the strength of stratification and vertical density gradients heavily influenced by morphological features corresponding to shallow points in regions of tight curvature ("horseshoe" bends). The spatiotemporal patterns of stratification led to the emergence of two "hot spots" of anoxia, the first downstream of a shallow region of tight curvature and the second downstream of a sill. Whilst these areas corresponded to regions of intense stratification, it was found that antecedent conditions related to the placement of the salt wedge played a major role in the recovery of anoxic regions following episodic high flow events. Furthermore, whilst a threshold salt wedge intrusion was a requirement for oxygen depletion, analysis of the results allowed us to quantify the effect of temperature in determining the overall severity and extent of hypoxia and anoxia. Climate warming scenarios highlighted that oxygen depletion is likely to be exacerbated through changes in flow regimes and warming temperatures; however, the increasing risk of hypoxia and anoxia can be mitigated through management of minimum flow allocations and targeted reductions in organic matter loading. A simple statistical model (R2 > 0.65) is suggested to relate riverine flow and temperature to the extent of estuary-wide anoxia.
Highlights
Estuaries provide an important role in the filtering and transformation of carbon and nutrients transported from catchments into marine environments
For the Yarra River estuary, our estimate of α = −0.35 is similar to the Tamar Estuary, a shallow, narrow riverine estuary with tight curvature and the Swan River estuary in Western Australia that has similar morphometry and hydrological regime
Whilst we found no clear correlation between the length of saline intrusion and distribution of anoxia and hypoxia, a parabolic relationship was evident between L2 and the maximum extent of oxygen depletion
Summary
Estuaries provide an important role in the filtering and transformation of carbon and nutrients transported from catchments into marine environments. Global trends, including climate change, increased urbanization and agriculture, have led to a decline in estuarine health across the world (Kennish, 2002; Vitousek et al, 1997; D’Avanzo and Kremer, 1994). Of particular concern is widespread depletion of oxygen in the bottom waters of estuaries, affecting benthic and pelagic habitats and leading to a decline in biodiversity (Kemp et al, 2009; Vaquer-Sunyer and Duarte, 2008). Reduced oxygen leads to altered nutrient budgets, including increased sediment nutrient release, often further contributing to eutrophication and deteriorating water quality (Kennish, 2002; Middelburg and Levin, 2009; Webster and Harris, 2004). Bruce et al.: Dissolved oxygen dynamics in a salt wedge estuary
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