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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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. |
doi_str_mv | 10.1007/s12237-024-01390-3 |
format | Article |
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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.</description><identifier>ISSN: 1559-2723</identifier><identifier>EISSN: 1559-2731</identifier><identifier>DOI: 10.1007/s12237-024-01390-3</identifier><language>eng</language><publisher>New York: Springer US</publisher><subject>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</subject><ispartof>Estuaries and coasts, 2024-12, Vol.47 (8), p.2306-2323</ispartof><rights>The Author(s) 2024</rights><rights>The Author(s) 2024. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c244t-7c61d1936563307c6e1a0b42073d12f74be8334a220cf350fc51cb97d9e1a9713</cites><orcidid>0009-0007-5461-6862</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12237-024-01390-3$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12237-024-01390-3$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>315,781,785,27929,27930,41493,42562,51324</link.rule.ids></links><search><creatorcontrib>Dreiss, Allison</creatorcontrib><creatorcontrib>Azarnivand, Amir Reza</creatorcontrib><creatorcontrib>Hildebrand, Anna</creatorcontrib><creatorcontrib>Pourreza Ahmadi, Seyedeh Fardis</creatorcontrib><creatorcontrib>Ali, Syeda Sadia</creatorcontrib><creatorcontrib>Lucchese, Veronica Malabanan</creatorcontrib><creatorcontrib>Zhang, Qian</creatorcontrib><creatorcontrib>Lapham, Laura L.</creatorcontrib><creatorcontrib>Woodland, Ryan J.</creatorcontrib><creatorcontrib>Harris, Lora</creatorcontrib><creatorcontrib>Testa, Jeremy M.</creatorcontrib><title>Controls on Oxygen Variability and Depletion in the Patuxent River Estuary</title><title>Estuaries and coasts</title><addtitle>Estuaries and Coasts</addtitle><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.</description><subject>Annual variations</subject><subject>Benthic fauna</subject><subject>Benthos</subject><subject>Brackishwater environment</subject><subject>Climate change</subject><subject>Climate variability</subject><subject>Coastal Sciences</subject><subject>Coastal waters</subject><subject>Depletion</subject><subject>Dissolved oxygen</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Estuaries</subject><subject>Estuarine dynamics</subject><subject>Estuarine environments</subject><subject>Eutrophic environments</subject><subject>Eutrophic rivers</subject><subject>Eutrophication</subject><subject>Freshwater & Marine Ecology</subject><subject>Hypoxia</subject><subject>Nutrient loading</subject><subject>Oxygen</subject><subject>Oxygen depletion</subject><subject>Phosphorus</subject><subject>River flow</subject><subject>Rivers</subject><subject>Spatial analysis</subject><subject>Stratification</subject><subject>Stream flow</subject><subject>Summer</subject><subject>Trends</subject><subject>Trophic levels</subject><subject>Variability</subject><subject>Water and Health</subject><subject>Water stratification</subject><subject>Water temperature</subject><subject>Zoobenthos</subject><issn>1559-2723</issn><issn>1559-2731</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp9kE1LxDAQhoMouK7-AU8Bz9VJJmnsUdb1iwVF1GtI23TtUtM1SWX33xut6M3TzMDzzgwPIccMThmAOguMc1QZcJEBwwIy3CETJmWRcYVs97fnuE8OQlgBCClBTMjdrHfR912gvaP3m-3SOvpifGvKtmvjlhpX00u77mxsE9A6Gl8tfTBx2FgX6WP7YT2dhzgYvz0ke43pgj36qVPyfDV_mt1ki_vr29nFIqu4EDFTVc5qVmAuc0RIk2UGSsFBYc14o0RpzxGF4RyqBiU0lWRVWai6SGChGE7Jybh37fv3wYaoV_3gXTqpkbFcSCEhTxQfqcr3IXjb6LVv39KbmoH-cqZHZzo509_ONKYQjqGQYLe0_m_1P6lPF59tnw</recordid><startdate>20241201</startdate><enddate>20241201</enddate><creator>Dreiss, Allison</creator><creator>Azarnivand, Amir Reza</creator><creator>Hildebrand, Anna</creator><creator>Pourreza Ahmadi, Seyedeh Fardis</creator><creator>Ali, Syeda Sadia</creator><creator>Lucchese, Veronica Malabanan</creator><creator>Zhang, Qian</creator><creator>Lapham, Laura L.</creator><creator>Woodland, Ryan J.</creator><creator>Harris, Lora</creator><creator>Testa, Jeremy M.</creator><general>Springer US</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QG</scope><scope>7SN</scope><scope>7TN</scope><scope>7U7</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>M7N</scope><orcidid>https://orcid.org/0009-0007-5461-6862</orcidid></search><sort><creationdate>20241201</creationdate><title>Controls on Oxygen Variability and Depletion in the Patuxent River Estuary</title><author>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.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c244t-7c61d1936563307c6e1a0b42073d12f74be8334a220cf350fc51cb97d9e1a9713</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Annual variations</topic><topic>Benthic fauna</topic><topic>Benthos</topic><topic>Brackishwater environment</topic><topic>Climate change</topic><topic>Climate variability</topic><topic>Coastal Sciences</topic><topic>Coastal waters</topic><topic>Depletion</topic><topic>Dissolved oxygen</topic><topic>Earth and Environmental Science</topic><topic>Ecology</topic><topic>Environment</topic><topic>Environmental Management</topic><topic>Estuaries</topic><topic>Estuarine dynamics</topic><topic>Estuarine environments</topic><topic>Eutrophic environments</topic><topic>Eutrophic rivers</topic><topic>Eutrophication</topic><topic>Freshwater & Marine Ecology</topic><topic>Hypoxia</topic><topic>Nutrient loading</topic><topic>Oxygen</topic><topic>Oxygen depletion</topic><topic>Phosphorus</topic><topic>River flow</topic><topic>Rivers</topic><topic>Spatial analysis</topic><topic>Stratification</topic><topic>Stream flow</topic><topic>Summer</topic><topic>Trends</topic><topic>Trophic levels</topic><topic>Variability</topic><topic>Water and Health</topic><topic>Water stratification</topic><topic>Water temperature</topic><topic>Zoobenthos</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Dreiss, Allison</creatorcontrib><creatorcontrib>Azarnivand, Amir Reza</creatorcontrib><creatorcontrib>Hildebrand, Anna</creatorcontrib><creatorcontrib>Pourreza Ahmadi, Seyedeh Fardis</creatorcontrib><creatorcontrib>Ali, Syeda Sadia</creatorcontrib><creatorcontrib>Lucchese, Veronica Malabanan</creatorcontrib><creatorcontrib>Zhang, Qian</creatorcontrib><creatorcontrib>Lapham, Laura L.</creatorcontrib><creatorcontrib>Woodland, Ryan J.</creatorcontrib><creatorcontrib>Harris, Lora</creatorcontrib><creatorcontrib>Testa, Jeremy M.</creatorcontrib><collection>Springer Nature OA/Free Journals</collection><collection>CrossRef</collection><collection>Animal Behavior Abstracts</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Toxicology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Estuaries and coasts</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Dreiss, Allison</au><au>Azarnivand, Amir Reza</au><au>Hildebrand, Anna</au><au>Pourreza Ahmadi, Seyedeh Fardis</au><au>Ali, Syeda Sadia</au><au>Lucchese, Veronica Malabanan</au><au>Zhang, Qian</au><au>Lapham, Laura L.</au><au>Woodland, Ryan J.</au><au>Harris, Lora</au><au>Testa, Jeremy M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Controls on Oxygen Variability and Depletion in the Patuxent River Estuary</atitle><jtitle>Estuaries and coasts</jtitle><stitle>Estuaries and Coasts</stitle><date>2024-12-01</date><risdate>2024</risdate><volume>47</volume><issue>8</issue><spage>2306</spage><epage>2323</epage><pages>2306-2323</pages><issn>1559-2723</issn><eissn>1559-2731</eissn><abstract>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.</abstract><cop>New York</cop><pub>Springer US</pub><doi>10.1007/s12237-024-01390-3</doi><tpages>18</tpages><orcidid>https://orcid.org/0009-0007-5461-6862</orcidid><oa>free_for_read</oa></addata></record> |
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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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