Our region is navigating complex decisions on how best to manage nutrients – specifically nitrogen – to maintain healthy habitats. Additional nitrogen from human activities can potentially increase harmful algal blooms, decrease dissolved oxygen, compound ocean acidification, and cause other changes that may harm marine life. New regulation is particularly focused on the impacts that nitrogen from human sources has on low dissolved oxygen in Puget Sound. The nutrient management decisions we make now have the potential to shape the future of wastewater treatment, water quality, and our communities for decades to come.
Looking for a quick policy-focused overview?
Explore key scientific insights and tradeoffs to support strategic nutrient management decisions in our
StoryMap
or
policy briefing sheet
.
For the past several years, the University of Washington Puget Sound Institute has played a central role in advancing the science and modeling that underpin nutrient management decisions in the region, including:
Leading cutting-edge research on species-specific risks that integrates temperature-dependent oxygen supply and demand.
Hosting a series of workshops to build consensus and accelerate scientific progress.
Convening an international Model Evaluation Group and leading ongoing model performance assessments.
Running the Salish Sea Model to test additional nutrient reduction scenarios.
Regulation is particularly focused on the impacts that nitrogen from human sources has on low dissolved oxygen in Puget Sound. A few key scientific insights help ground these management decisions:


Nutrient inputs and primary productivity remain relatively stable

Nutrients feed algal blooms, which support the base of the food web, but can also cause low dissolved oxygen. Interestingly, primary productivity in the Salish Sea has remained stable for several decades. Using nitrogen budgets and sediment isotope analyses, Dr. Sophia Johannesen (Fisheries and Oceans Canada) found that total productivity has changed little since the 1970s. However, the composition of phytoplankton appears to be shifting—from diatoms to dinoflagellates—in some basins.6
As Professor Tim Essington explains, warmer water holds less oxygen while also increasing how much oxygen marine species need to thrive.
University of Washington researchers analyzed more than 12,000 shipboard measurements and identified five sites with sufficient data to track century-scale trends. Over the past century, warming caused most of the 0.3–0.9 mg/L decline in fall, bottom-water oxygen at several long-term monitoring sites in Puget Sound – near Seattle, Point Jefferson, and Carr Inlet.4
At our 2022 workshop, Martha Sutula shared how the Southern California Coastal Water Research Project is jointly modeling temperature and oxygen to understand risk and inform management actions in California. University of Washington scientists are similarly studying temperature and oxygen to identify when and where species in Puget Sound are most vulnerable. Early results show:5
If warming trends continue, climate change could also erode gains from reducing nitrogen inputs to the Sound. For example, in the Chesapeake, temperature increases are expected to offset 6-34% of improvements from the last 40 years.6
Washington State uses both Salish Sea Model outputs and measured data to determine 303(d) listings of impaired water bodies. Under the presumptive water quality standards, a specific location in Puget Sound is considered non-compliant on a given day if:

Most of Puget Sound falls below the numeric criteria even without human impacts, so it is important to consider natural conditions. How we draw the line matters—particularly since most noncompliant areas barely exceed the standard.8
Model results released in June 2025 underpin the Draft Puget Sound Nutrient Reduction Plan, Washington’s advanced restoration strategy for meeting marine dissolved oxygen standards. The State ran several scenarios to explore the potential impact of reducing nutrients from marine point sources and watersheds. The final nitrogen loading targets were ultimately derived from the Opt2_8 modeling scenario in Figueroa-Kaminsky et al. (2025) and would reduce anthropogenic:
In 2023-2024, Puget Sound Institute convened global experts to advise on how to improve the application of the Salish Sea Model to inform recovery goals and nutrient management decisions in Puget Sound. More recently, Puget Sound Institute reviewed Figueroa-Kaminsky et al. (2025) to evaluate how the model updates and analyses influence the proposed nutrient targets. Our analysis reinforced that:
Credibly implementing Washington state’s standard may require model skill beyond what any model can likely ever achieve. 9
Complex environmental challenges benefit from insights and ongoing advice from scientists in other regions like the Chesapeake Bay and the Baltic, where models have been used to manage nutrients for decades. The University of Washington Puget Sound Institute convened global experts to advise on how to improve the application of the Salish Sea Model to inform recovery goals and nutrient management decisions in Puget Sound. We were lucky to benefit from the expertise of Bill Dennison, Jacob Carstensen, Jeremy Testa, Kevin Farley, and Peter Vanrolleghem.
The following technical memorandum reviews the information provided in Figueroa-Kaminsky et al. (2025) to evaluate how presented model updates and analyses influence the proposed nutrient targets.
Puget Sound Institute has complemented the State’s modeling to run additional scenarios to assess the magnitude of change in dissolved oxygen concentrations from changing specific wastewater treatment plant and river loads, including:
By sharing our model analysis and postprocessing scripts, we hope to spark robust scientific discussion and co-development. Other models like LiveOcean and SalishSeaCast also help deepen our scientific understanding to inform management actions.
Our scientific workshops build on regional discussions like Ecology’s Nutrient Forum and the Marine Water Quality Implementation Strategy to dig deeper into uncertainties like the “memory” from sediment oxygen demand and different species’ vulnerability to dissolved oxygen. We appreciate everyone’s generosity with their time and the valuable insights shared by numerous monitoring experts, modelers, managers, and researchers.
2025 workshops
2022 workshops
Have a question or interested in collaborating?
Email Stefano Mazzilli (mazzilli@uw.edu) and Marielle Kanojia (marlars@uw.edu).