Modeling the Links Between Discharge and Nutrients from the Mississippi River Basin to the Gulf of Mexico Hypoxia

EPA researchers have created a state-of-the-art three-dimensional model of the oxygen starved waters in the Gulf of Mexico. Each summer, as the waters warm, nearly 8,000 square miles of water becomes a dead zone killing bottom-dwelling marine life and pushing others further out to sea. This dead zone has been well-documented for years but now EPA researchers have developed a 3-D model to better predict where the dead zone will occur each year and ways to reduce its negative effects. The model was developed in partnership with physical oceanographers at the U.S. Naval Research Laboratory who provided data on the swirling currents where the Mississippi meets the Gulf of Mexico.

Read the Science Matters story, Into the Dead Zone.

Publications 

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1. Carbon dynamics and community production in the Mississippi River plume

Dissolved inorganic carbon (DIC), total alkalinity (TAlk), pH, and dissolved oxygen (DO) were determined in the Mississippi River plume during five cruises conducted in the spring, summer, and fall.

2. Microbial respiration and ecoenzyme activity in sediments from the Gulf of Mexico hypoxic zone

Sediment chemistry, microbial respiration, and ecoenzyme activity were measured in 4 zones of similarity in the northern Gulf of Mexico.

3. Microphytobenthos production potential and contribution to bottom layer oxygen dynamics on the inner Louisiana continental shelf (subscription only)

To investigate the relative importance of microphytobenthos (MPB) oxygen (O2) production on a river-dominated shelf, sediment core incubation measurements of MPB O2 production and sediment O2 consumption were compared to water-column measures of primary production and respiration during one spring and two summer cruises.

4. Nutrient distributions, transports and budgets on the inner margin of a river-dominated continental shelf (subscription only)

Physical and biogeochemical processes determining the distribution, transport, and fate of nutrients delivered by the Mississippi and Atchafalaya river basin to the inner Louisiana continental shelf were examined using a three-dimensional hydrodynamic model and observations of hydrography, nutrients, and organic carbon collected during 12 cruises.

5. Plankton community respiration, net ecosystem metabolism, and oxygen dynamics on the Louisiana continental shelf: implications for hypoxia (subscription only)

A multi-year study was conducted of the Louisiana continental shelf to better understand the linkages between water column metabolism and the formation of hypoxia (dissolved oxygen <2 ml O2 l−1) in the region.

6. Sediment-water fluxes of dissolved inorganic carbon, O2, nutrients, and N2 from the hypoxic region of the Louisiana continental shelf

One of the largest coastal hypoxic regions has been observed during the summer in the bottom-water of the Louisiana continental shelf.  In this study, the sediment-water fluxes of dissolved inorganic carbon, oxygen, nutrients, and denitrification were measured on the Louisiana shelf during six cruises from 2005 to 2007.