Ecosystem Targets and Supporting Indicators
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We use several water temperature datasets, located throughout the Sound, to improve our understanding of decadal and long-term changes in water temperature – Niantic Bay by Millstone Environmental Lab, Milford by NOAA Milford Lab, and Woods Hole by Woods Hole Oceanographic Institute, and an average of 17 stations collected throughout the Sound by CT DEEP (i.e., herein referred to as Soundwide). It is important to track water temperature as changes can significantly impact biological, chemical, and physical components in Long Island Sound. For example, increases in surface water temperatures have been linked to observed changes in the fish community – as cold-adapted fish (e.g., alewife, Atlantic cod, and winter flounder) have been observed less frequently in recent years, while warm-adapted fish (e.g., striped bass, black sea bass, and summer flounder) have been observed more frequently. Furthermore, increases in bottom water temperature also have an affect on the benthic community. For example, American lobsters cannot maintain their metabolisms in waters above 20°C for long periods of time and therefore have declined significantly in recent years. Additionally, these changes in fish community can have cascading effects up the food web, where the prey of these species are changing in assemblages, as well. Seasonal increases in water temperature can also impact different life stages of fish, shellfish, crustaceans, and zooplankton, and therefore may hinder their success in growth.
Here we report on both long-term annual and winter water temperatures to show us relative temperature change at several stations throughout the region over time. It helps us see the decade scale-up and downswings in the regional data, as well as the overall year to year variability. We also included winter temperatures because it is less impacted by daily weather patterns and station locations, and therefore stays pretty uniform temperature throughout the Sound. The other dataset shows Soundwide seasonal bottom averages. This dataset is much shorter, but higher resolution. By clicking the individual seasons on or off in the legend, you can more clearly see the patterns within each season.
The long-term annual and winter graphs show several longer datasets from throughout the region. In most cases, these measurements are taken at least weekly from near-surface inshore waters in the vicinity of various laboratory facilities. The seasonal bottom water temperature dataset is collected by CT DEEP from 17 stations located throughout the Sound through the Long Island Sound Water Quality and Hypoxia Monitoring Program.
When all stations are averaged, from 1991-2025, the Soundwide’s annual surface water temperatures has increased by 1.1, with a difference of 0.65°F;  whereas when all embayments are averaged, from 1960-2025, the annual surface water temperatures has increased by 8.6, with a difference of 4.4°F. Using the winter surface water temperature can be a stronger indicator as it removes fluctuations caused by storm disturbances – the Soundwide’s winter surface water temperatures have increased by 4.6 percent, whereas the embayment’s winter surface water temperatures have increased by 19 percent. Moreover, the rate of increase for the winter surface water temperatures in the Sound is approximately 1°F/decade, which is currently above the global average of 0.36°F/decade (NOAA 2025). Seasonal bottom water temperatures have been slowly but steadily increasing throughout the Sound. Because 2025 was a colder year compared to others, from 1991-2025, each season experienced a percent decrease – winter by 4 percent, spring by 0.5 percent, and summer by 0.7 percent (note: data for fall is not available). The overall mean from 1991-2025 is 37.03°F for winter, 49.09°F for spring, and 67.46°F for summer.
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