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Seasonality and trends in coastal water temperature from NOAA water level monitoring stations along US coasts

Our take

Coastal regions represent complex interfaces vulnerable to localized impacts from climate change and natural hazards. A newly validated dataset of coastal water temperature (WT) from NOAA’s Center for Operational Oceanographic Products and Services (CO-OPS) stations, spanning 1995-2023 and encompassing major US coastal regions, reveals significant seasonality and trends. Analysis of 90 stations indicates consistent seasonal cycles linked to solar heating, with pronounced differences across regions. Notably, 46 stations exhibited statistically significant warming trends, averaging 0.5°C/decade, particularly along the Mid-Atlantic and Southeast coasts.
Seasonality and trends in coastal water temperature from NOAA water level monitoring stations along US coasts

The confluence of oceanic, atmospheric, and terrestrial forces shaping our coastal regions demands increasingly precise and localized data, a need underscored by recent findings and further illuminated by this new dataset from NOAA’s Center for Operational Oceanographic Products and Services (CO-OPS). The introduction of a quality-controlled coastal water temperature dataset, spanning from the mid-1990s to 2023 across 90 stations, represents a significant advancement in our ability to understand and predict coastal dynamics. This development builds upon existing efforts to leverage complex data streams for improved resource management, as explored in A computational intelligence framework for multimodal oceanic data analysis and predictive modeling in sustainable marine resource management. Further context is provided by research focusing on Arctic zooplankton dynamics, highlighting the importance of long-term observational data for understanding ecosystem responses to change, as seen in Production estimates of the dominant copepod Metridia longa from nauplii to adults in the western Arctic Ocean, based on year-round observations at an ice station. The ability to track seasonal cycles, identify extreme quantiles, and assess long-term trends with this level of detail is vital for informed decision-making in vulnerable coastal communities.

The study’s findings reveal a nuanced picture of coastal warming. The observed lag between peak air temperature and peak water temperature, consistently documented across regions, reinforces the thermal inertia of ocean systems. The stark contrast in seasonal cycles and temperature ranges between the East Coast/Great Lakes and the West Coast/Island regions is particularly noteworthy, underscoring the geographic variability of climate impacts. The prevalence of positive warming trends, with statistically significant rates observed at nearly half of the stations, is a cause for continued scrutiny. The pronounced trends along the Mid-Atlantic, Southeast, and Gulf regions, coupled with the comparatively smaller trends in the Northwest, highlight the uneven distribution of warming effects. These regional variations necessitate tailored adaptation strategies and a deeper understanding of the underlying drivers—a challenge that echoes the complexities of legal frameworks surrounding the Arctic blue economy, as discussed in Legal frameworks for the Arctic blue economy: risks and regulatory responses.

The comparison to NOAA’s Optimum Interpolation SST dataset and the case study on marine heatwaves in South Florida effectively demonstrate the value of localized, in situ monitoring. While global datasets provide valuable context, the resolution and accuracy of local measurements are essential for assessing specific vulnerabilities and triggering timely responses. This new dataset provides a robust foundation for continuous environmental monitoring, enabling researchers and policymakers to track changes, validate models, and refine predictive capabilities. The consistent and reliable nature of the data, stemming from CO-OPS’s established infrastructure, significantly enhances its utility for long-term trend analysis and risk assessment. The emphasis on quality control is paramount, ensuring the data’s suitability for supporting critical decision-making processes related to coastal infrastructure, ecosystem management, and public safety.

Ultimately, this work underscores the escalating importance of localized ocean intelligence. The increasing frequency and intensity of coastal hazards, exacerbated by climate change, demand a more granular understanding of ocean conditions. The availability of this comprehensive and validated dataset represents a crucial step toward achieving that understanding. A key question moving forward is how this data, and others like it, can be integrated into predictive models capable of forecasting localized impacts and informing proactive adaptation measures. Will we see a shift towards more adaptive infrastructure planning and ecosystem-based management strategies, driven by the insights gleaned from these increasingly sophisticated ocean monitoring systems?

Coastal regions are complex environments. They lie at the confluence of physical oceanic, atmospheric, and land-based processes, and continue to undergo significant change due to both natural and human-driven factors. Impacts from the natural hazards affecting these regions are highly localized, such as infrastructure damage due to coastal flooding or ecosystem stress due to marine heatwaves. This paper introduces a new quality-controlled dataset of coastal water temperature collected at NOAA Center for Operational Oceanographic Products and Services (CO-OPS) water level monitoring stations. Water temperature (WT) data records were analyzed at 90 stations extending from the mid-1990s to 2023 and representing all major US coastal regions. A series of basic statistical metrics were computed and compared across regions, including daily and monthly WT climatologies, empirical extreme quantiles, and linear trend rates. WT seasonal cycles tracked well with solar heating and peak WTs consistently tracked behind peak air temperature by a few days to a few weeks. US East Coast and Great Lakes regions have much stronger WT seasonal cycles and larger ranges (up to 25°C) than West Coast and Island regions (as low as 3°C). The great majority of stations experienced positive trends over this time period, with statistically significant linear trend rates at 46 of 90 stations, averaging nearly 0.5 °C/decade. Largest trends were found along Mid-Atlantic, Southeast, and Gulf regions while smallest trends found in the Northwest. Lastly, two case studies were examined, a comparison to NOAA's Optimum Interpolation SST global dataset and frequency of marine heatwaves in South Florida, both of which highlight the need for local in situ monitoring. This new WT dataset from CO-OPS provides consistent, reliable data that can support continuous local environmental monitoring and helps inform future planning and decision-making in this dynamic environment.

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