Controls on Oxygen Variability and Depletion in the Patuxent River Estuary

Oxygen depletion in coastal waters is increasing globally due primarily to eutrophication and warming. Hypoxia responses to nutrient loading and climate change have been extensively studied in large systems like the Chesapeake Bay and the Baltic Sea, while fewer studies have investigated smaller, sh...

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Veröffentlicht in:Estuaries and coasts 2024-12, Vol.47 (8), p.2306-2323
Hauptverfasser: Dreiss, Allison, Azarnivand, Amir Reza, Hildebrand, Anna, Pourreza Ahmadi, Seyedeh Fardis, Ali, Syeda Sadia, Lucchese, Veronica Malabanan, Zhang, Qian, Lapham, Laura L., Woodland, Ryan J., Harris, Lora, Testa, Jeremy M.
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container_end_page 2323
container_issue 8
container_start_page 2306
container_title Estuaries and coasts
container_volume 47
creator Dreiss, Allison
Azarnivand, Amir Reza
Hildebrand, Anna
Pourreza Ahmadi, Seyedeh Fardis
Ali, Syeda Sadia
Lucchese, Veronica Malabanan
Zhang, Qian
Lapham, Laura L.
Woodland, Ryan J.
Harris, Lora
Testa, Jeremy M.
description Oxygen depletion in coastal waters is increasing globally due primarily to eutrophication and warming. Hypoxia responses to nutrient loading and climate change have been extensively studied in large systems like the Chesapeake Bay and the Baltic Sea, while fewer studies have investigated smaller, shallower hypoxic zones. Thus, an improved understanding of the interactions of eutrophication and warming on hypoxia expansion (or reduction) in the wide variety of different estuarine environments is needed. We examined interannual controls on oxygen depletion in the Patuxent River estuary, a eutrophic sub-estuary of Chesapeake Bay where seasonal hypoxia develops annually. We conducted a spatial and temporal analysis of dissolved oxygen (DO) trends, timing, and several metrics of depletion over a long-term record (1985–2021). We found an internally generated hypoxic zone that initiates in the middle estuary, spreading upstream and downstream as the summer progresses, and that hypoxic volume days (HVD) have been increasing (0.11 per year, p  = 0.03) over the record despite reduced watershed nitrogen loads and stable phosphorus loads. River flow and temperature have been increasing and are major drivers of increased HVD, with river flow explaining 40% of the interannual variation in HVD (temperature has increased 0.03 and 0.06 °C per year in summer and fall, respectively). Apparent oxygen utilization (AOU) is increasing in bottom waters in the fall, consistent with increasing trends of both water temperature and stratification strength. HVD was negatively related ( r 2  = 0.34, slope = −0.59*HVD) to the biomass of benthic invertebrates in the middle region of the estuary, suggesting that benthic forage for higher trophic levels will be limited by sustained hypoxia. These results indicate that current and future climate variability plays an important role in regulating oxygen depletion in the Patuxent River estuary, which reinforces the need to factor climate change into strategies for the restoration and management of estuaries.
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subjects Annual variations
Benthic fauna
Benthos
Brackishwater environment
Climate change
Climate variability
Coastal Sciences
Coastal waters
Depletion
Dissolved oxygen
Earth and Environmental Science
Ecology
Environment
Environmental Management
Estuaries
Estuarine dynamics
Estuarine environments
Eutrophic environments
Eutrophic rivers
Eutrophication
Freshwater & Marine Ecology
Hypoxia
Nutrient loading
Oxygen
Oxygen depletion
Phosphorus
River flow
Rivers
Spatial analysis
Stratification
Stream flow
Summer
Trends
Trophic levels
Variability
Water and Health
Water stratification
Water temperature
Zoobenthos
title Controls on Oxygen Variability and Depletion in the Patuxent River Estuary
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