Publications about Chesapeake Bay

IAN is committed to producing practical, user-centered communications that foster a better understanding of science and enable readers to pursue new opportunities in research, education, and environmental problem-solving. Our publications synthesize scientific findings using effective science communication techniques.

2016 Chesapeake Bay Report Card (Page 1)

2016 Chesapeake Bay Report Card

Caroline Donovan, Alexandra Fries, Dylan Taillie, Bill Dennison ·
8 May 2017

This report card provides a transparent, timely, and geographically detailed assessment of Chesapeake Bay. In 2016, the report card includes five water quality indicators and two biotic indicators. In 2016, the overall grade for Chesapeake Bay is a 54%, a C. This means the Bay is in moderate health. Long term trends of each reporting region health and a fisheries index are also presented. For further details, visit the Report Card Website.

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Tidal water quality indicator factsheets (Page 1)

Tidal water quality indicator factsheets

Caroline Donovan, Suzanne Webster, Alexandra Fries ·
18 April 2017

The Chesapeake Monitoring Cooperative (CMC), as part of the Indicator Effectiveness Matrix objective, produced 12 factsheets describing 14 tidal water quality indicators. These indicators are part of the CMC's tidal water quality Quality Assurance Project Plan and Method Manuals. The factsheets are intended for nontraditional and volunteer monitoring groups to include as part of their water quality monitoring programs as education materials for their volunteers.

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Assessing water quality of the Chesapeake Bay by the impact of sea level rise and warming (Page 1)

Assessing water quality of the Chesapeake Bay by the impact of sea level rise and warming

Wang P,Linker L, Wang H, Bhatt G, Yactayo G, K Hinson K and Tian R ·
2017

The influence of sea level rise and warming on circulation and water quality of the Chesapeake Bay under projected climate conditions in 2050 were estimated by computer simulation. Four estuarine circulation scenarios in the estuary were run using the same watershed load in 1991-2000 period. They are, 1) the Base Scenario, which represents the current climate condition, 2) a Sea Level Rise Scenario, 3) a Warming Scenario, and 4) a combined Sea Level Rise and Warming Scenario.

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Multiple stressors threaten the imperiled coastal foundation species eelgrass (Zostera marina) in Chesapeake Bay, USA (Page 1)

Multiple stressors threaten the imperiled coastal foundation species eelgrass (Zostera marina) in Chesapeake Bay, USA

Lefcheck JS, Wilcox DJ, Murphy RR, Marion SR, and Orth RJ ·
2017

Interactions among global change stressors and their effects at large scales are often proposed, but seldom evaluated. This situation is primarily due to lack of comprehensive, sufficiently long-term, and spatially extensive datasets. Seagrasses, which provide nursery habitat, improve water quality, and constitute a globally important carbon sink, are among the most vulnerable habitats on the planet.

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2015 Chesapeake Bay Report Card (Page 1)

2015 Chesapeake Bay Report Card

Caroline Donovan, Alexandra Fries, Bill Dennison ·
17 May 2016

This report card provides a transparent, timely, and geographically detailed assessment of Chesapeake Bay. In 2015, the report card includes five water quality indicators and two biotic indicators. In 2015, the overall grade for Chesapeake Bay is a 53%, a C. This means the Bay is in moderate health. Long term trends of each reporting region health and a fisheries index are also presented. For further details, visit the Report Card website.

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Effects of cross-channel bathymetry and wind direction on destratification and hypoxia reduction in the Chesapeake Bay (Page 1)

Effects of cross-channel bathymetry and wind direction on destratification and hypoxia reduction in the Chesapeake Bay

Wang P, Wang H, Linker L, and Tian R ·
2016

A coupled estuarine hydrodynamic model and water quality model were used to analyze differences in destratification and anoxia/hypoxia reduction by wind directions in the north-south oriented Chesapeake estuary, USA. The predominant cross-channel bathymetry in the Bay's anoxic center is asymmetric with a steeper and narrower shoal on the eastern shore than on the western shore, which modifies wind-induced circulation differently for two opposite wind directions.

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Influence of Reservoir Infill on Coastal Deep Water Hypoxia (Page 1)

Influence of Reservoir Infill on Coastal Deep Water Hypoxia

Linker LC, Batiuk RA, Cerco CF, Shenk GW, Tian R, Wang P, and Yactayo G ·
2016

Ecological restoration of the Chesapeake through the Chesapeake Bay total maximum daily load (TMDL) requires the reduction of nitrogen, phosphorus, and sediment loads in the Chesapeake watershed because of the tidal water quality impairments and damage to living resources they cause. Within the Chesapeake watershed, the Conowingo Reservoir has been filling in with sediment for almost a century and is now in a state of near-full capacity called dynamic equilibrium.

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Long-Term Changes in Sediment and Nutrient Delivery from Conowingo Dam to Chesapeake Bay: Effects of Reservoir Sedimentation (Page 1)

Long-term changes in sediment and nutrient delivery from Conowingo Dam to Chesapeake Bay: Effects of reservoir sedimentation

Zhang Q, Hirsch RM, Ball WP ·
2016

Reduction of suspended sediment (SS), total phosphorus (TP), and total nitrogen is an important focus for Chesapeake Bay watershed management. The Susquehanna River, the bay’s largest tributary, has drawn attention because SS loads from behind Conowingo Dam (near the river’s mouth) have been rising dramatically. To better understand these changes, we evaluated histories of concentration and loading (1986−2013) using data from sites above and below Conowingo Reservoir.

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