Water quality

Puget Sound is unique in the lower 48 Unites States because of its fjord-like physiography, inland extent, wide range of depths, and urbanized watersheds and shorelines. Limited exchange of seawater between sub-basins within Puget Sound can result in long residence times, potentially increasing the susceptibility of biota to contamination introduced through human activities. The varied habitats within Puget Sound support multiple life history stages of many species, potentially exposing sensitive life stages to contamination. There are multiple water quality concerns in Puget Sound:

  • Levels of toxic contaminants in biota that live or feed in Puget Sound.
  • The eutrophication of marine waters, producing hypoxic and anoxic regions.
  • Wastewater contamination, principally from combined sewer overflows or septic systems
  • Harmful algal blooms, which introduce toxins that enter the food web
  • Acidification of marine waters, and the adverse ecological effects that result.

Degradation of water quality in Puget Sound occurs through three primary mechanisms. The first is through the introduction of toxic contaminants, primarily comprising manufactured synthetic chemicals, but also including compounds that occur naturally that are concentrated in the local environment to toxic levels via human activities. The second is through human-caused changes in naturally occurring chemicals, compounds, or physical parameters (e.g., temperature, turbidity, nutrients, pH). The third is through introduction of new diseases or pathogens, or through other activities that cause an unnatural increase in disease organisms.

Sources:

Puget Sound Science Review

 

Overview

A 2023 report from the Puget Sound Ecosystem Monitoring Program presents an overview of selected recent monitoring and research activities focused on toxic contaminants in the Salish Sea. 

Cover of 2022 Salish Sea toxics monitoring synthesis: A selection of research

Related Articles

Air temperatures have been slightly warmer and river flows are higher. Blooms are present only in Whidbey Basin and isolated bays. The water column otherwise is relatively clear. Sediment rich water is entering from the Stillaguamish River. Debris lines were visible in Hood Canal and North Sound. Multiple reported oil sheens seen in Lake Washington Ship Canal. Generally, the year 2014 started colder and saltier throughout Puget Sound. Oxygen is lower in Whidbey Basin, Central and South Sound, but higher in Hood Canal. Upwelling favorable conditions stimulate a spring phytoplankton bloom off the Washington coast.

Thousands of different compounds are produced and used as part of our daily lives.  Examples include pharmaceuticals (NSAIDs, birth control pills, etc), personal care products (sun screen agents, scents, preservatives, etc), food additives (artificial sweeteners) and compounds used in industrial and commercial applications (flame retardants, antibiotics, etc).  Advances in analytical methods have allowed the detection of many of these compounds in the environment.

A 2014 paper in the journal PloS One analyzes a large carbonate chemistry data set from Puget Sound as a basis for identifying control conditions in ocean acidification experiments for the region.

Harbor porpoise (Phocoena phocoena) are one of the most frequently sighted cetaceans in the Salish Sea. Anecdotal information, possibly supported with stranding encounter rate data, suggests that harbor porpoise may have increased in Puget Sound, or have shifted their distribution back to Puget Sound relative to earlier decades.

Harbor porpoises were once common in Puget Sound, but had all but disappeared from local waters by the 1970s. Regular and numerous anecdotal sightings in recent years show that populations of these cetaceans are now increasing and may be approaching their former status. The attached document from NOAA Fisheries describes harbor porpoise numbers and their geographic range in Puget Sound as of 2011. 

HARBOR PORPOISE (Phocoena phocoena vomerina): Washington Inland Waters Stock (NOAA Fisheries 2011)

River flows are above normal and air temperatures are increasing slowly. The spring phytoplankton bloom is slow to develop with visible blooms limited to smaller bays such as Sequim and Bellingham Bays. Noctiluca observed in East Sound on Orcas Island, coinciding with high numbers of jellyfish. Debris lines are mostly confined to Hood Canal. Pockets of colder water observed in Central Sound and Hood Canal, likely from the colder, saltier conditions that developed during the winter in the northern regions. Oxygen is variable yet close to expected ranges. Sizable oil sheens were sighted in Gig Harbor and Carr Inlet.