Ecosystem Targets and Supporting Indicators
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Meeting the hypoxia reduction ecosystem target by increasing oxygen concentrations in the bottom waters is ahead of schedule. The target is measured as the five-year rolling average of the bottom water area with < 3 mg/L dissolved oxygen. The five-year rolling average for 2018-2022 was 87 square miles of hypoxia compared to an average of 208 square miles from the 1987-1999 baseline, a 58 percent reduction. Based on the 2015 CCMP, a 28 percent reduction from the baseline (to about 150 square miles) is necessary to achieve a measurable reduction (see data note). While achieving a measurable reduction in hypoxia from 2018-2022 is a major achievement, further reductions in the hypoxic area are needed through 2035 in order to fully attain water quality standards and achieve the ecosystem target goal.
The five-year average hypoxic area increased slightly by four square miles from last year’s five-year average of 83 square miles (for 2017-2021) even though the maximum area of hypoxia decreased – from 142 square miles in 2021 to 87 square miles in 2022. Dry summer conditions during summer 2022 likely reduced nutrient loading to the Sound from the watershed, likely contributing to the observed reduction in hypoxic area. Excess nutrient loading contributes to conditions that result in hypoxic, or oxygen-depleted, waters.
In assessing trends, LISS uses the five-year rolling average, instead of from year to year, because conditions in any given year could be impacted by variable factors, such as extreme changes in heat or precipitation, which average out over time.
The years 1987-1999 are used as a benchmark (or the baseline) because they represent the beginning of Long Island Sound Study’s water quality monitoring program, prior to the Total Maximum Daily Load (TMDL) agreement in 2000 to reduce nitrogen loads into the Sound.
Warming water temperatures will reduce the amount of oxygen that the water can contain, making it more difficult to meet the target long term. In addition to weather variables affecting the area of hypoxia year to year, longer-term climate influences will affect the vulnerability of the Sound to hypoxia. Improvements in monitoring, including increased monitoring in embayments, will better define areas affected by hypoxia, and the factors contributing to it.
Routine monitoring of bottom-water hypoxia is done monthly throughout the year and biweekly in the summer by the Connecticut Department of Energy and Environmental Protection (CT DEEP).
Additional year-round monitoring is conducted by the Interstate Environmental Commission in Western Long Island Sound and the Narrows. The Long Island Sound Integrated Coastal Observing System (LISICOS) also deploys real-time monitoring instruments on buoys across the Sound, including three with bottom water oxygen sensors in the Western Sound. The three monitoring programs help provide a comprehensive long-term data set on both the area and duration of hypoxia, with the monitoring data going back to 1987 (initially conducted by the University of Connecticut from 1987-1990, and beginning with CT DEEP since 1991).
Bottom hypoxia is measured by lowering instruments with multiple sensors (including dissolved oxygen) through the water column from a research vessel or smaller boat.
Hypoxia, a deficiency in the amount of oxygen in the water, can be harmful or lethal to fish, invertebrates, and other animals and therefore decrease or eliminate them from Long Island Sound.
Hypoxia may also limit the growth of animals that are exposed but not killed.
Dr. James Ammerman, Long Island Sound Study [email protected]
CT DEEP (primary data source), also the Interstate Environmental Commission for Western Long Island Sound, and LISICOS.
Here are links to find data on dissolved oxygen levels and the extent of hypoxia in Long Island Sound:
Hypoxia is more frequent in the western Sound.
2019 Long Island Sound CT DEEP and IEC Hypoxia Review Report