The Salish Sea

Marine ecology of Puget Sound, the straits, and the inland waters
The water in front of Mukilteo is not just "Puget Sound." It is part of the Salish Sea — an interconnected inland sea shared between the United States and Canada, where orcas follow salmon, tides shape shorelines, and stormwater carries the fingerprint of every road and roof in the watershed.
~18,000 km² total area
365m max depth
~73 southern resident orcas
5 salmon species
2009 officially named

1. The Salish Sea

Definition and Geography

The Salish Sea is defined as the interconnected body of water comprising Puget Sound, the Strait of Juan de Fuca, the Strait of Georgia, and the waterways surrounding the San Juan Islands. It was jointly named in 2009 by the U.S. Board on Geographic Names and the Geographical Names Board of Canada, honoring the Salish peoples who have lived along these shores for millennia.

The name does not replace existing names — Puget Sound is still Puget Sound. "Salish Sea" describes the whole system as a single ecological and hydrological unit, which is how the water actually behaves.

Physical Dimensions

Component Area Max Depth Character
Puget Sound 2,632 km² 283 m Deep fjord-like basins, glacially carved
Strait of Georgia 6,900 km² 365 m Broad basin between Vancouver Island and mainland BC
Strait of Juan de Fuca 3,540 km² 250 m Pacific gateway, strong tidal exchange
San Juan / Gulf Islands ~4,900 km² varies Archipelago with complex channels and passes
Total Salish Sea ~18,000 km² 365 m 6,900 sq mi of inland sea

Tidal Exchange with the Pacific

The entire Salish Sea breathes through a single opening: the Strait of Juan de Fuca. Twice daily, billions of gallons of Pacific water enter and leave through this channel, driven by mixed semidiurnal tides. The narrow passes between the San Juan Islands create some of the strongest tidal currents in the world — Deception Pass runs up to 8 knots.

Connection to our data: NOAA tide station 9447659 (Mukilteo) measures these tides in real time. The mixed semidiurnal pattern — two highs and two lows of unequal height each day — is characteristic of the Salish Sea's complex geometry.

2. Southern Resident Orcas (J, K, L Pods)

Population Status

Critically Endangered Year-round Resident (J Pod) Seasonal (K & L Pods)

The Southern Resident Killer Whales are a genetically distinct population of approximately 73 individuals, listed as endangered under both the U.S. Endangered Species Act (2005) and Canada's Species at Risk Act. They are divided into three family groups:

Pod Approx. Size Range Pattern Key Traits
J Pod ~24 Year-round in Puget Sound / Salish Sea Most frequently sighted, tightest family bonds
K Pod ~16 Seasonal; oceanic in winter, inland in summer Often travels with L Pod offshore
L Pod ~33 Most oceanic; returns to inland waters May–October Largest pod, ranges to northern California

Diet: Salmon Specialists

Unlike transient (Bigg's) orcas that hunt marine mammals, Southern Residents are salmon specialists. Chinook salmon make up approximately 80% of their diet during summer months. This extreme dietary specialization is the root of their vulnerability — as Chinook populations decline, the orcas decline with them.

The orcas use echolocation to hunt individual salmon, often at depth. Vessel noise directly competes with their sonar, reducing foraging efficiency by an estimated 25% in heavy traffic.

Threats

Mukilteo connection: Orcas transit Possession Sound following salmon runs heading toward the Snohomish River estuary. J Pod has been documented in the waters directly off Mukilteo, pursuing Chinook salmon moving between the main basin of Puget Sound and the river system we monitor at USGS gauge 12150800.

3. Salmon Runs

Five Species of Pacific Salmon in the Salish Sea

Species Scientific Name Run Timing Significance
Chinook (King) O. tshawytscha Year-round (peak Aug–Oct) Primary orca prey; largest species; ESA threatened
Coho (Silver) O. kisutch Sep–Nov Popular sport fish; vulnerable to 6PPD-quinone
Pink (Humpy) O. gorbuscha Aug–Oct (odd years) Most abundant; strict two-year lifecycle
Chum (Dog) O. keta Oct–Dec Late-season spawner; important marine nutrient transport
Sockeye (Red) O. nerka Jun–Aug Lake-rearing juvenile phase; highly valued commercially

The Snohomish River System

The Snohomish River watershed is one of the most productive salmon systems in Puget Sound. Its two major tributaries — the Skykomish and the Snoqualmie — drain the western Cascades, collecting snowmelt and rain that sustains salmon from egg to ocean and back.

The river we track via USGS gauge 12150800 (Snohomish River near Monroe) carries all five salmon species from the mountains to the Sound. Flow conditions directly affect migration success:

Flow Condition Range (cfs) Impact on Salmon
Very Low < 2,000 Thermal stress, low dissolved oxygen, migration barriers at shallow riffles
Low 2,000–5,000 Marginal passage; adults may hold in deep pools
Optimal 5,000–20,000 Good migration conditions; adequate depth and dissolved oxygen
High 20,000–50,000 Strong migration trigger; freshets attract adults from the Sound
Flood > 50,000 Redd scour risk; eggs and juveniles displaced; debris hazard
Why river flow matters: High flow = good migration conditions. Low flow = stress. Our weather data directly predicts flow conditions — heavy rain in the Cascades drives the freshets that trigger salmon runs.

Hatcheries and Restoration

Two major hatchery systems supplement wild salmon runs in the Snohomish watershed:

The tension between hatchery production and wild stock recovery is one of the central debates in Pacific salmon management. Hatchery fish can compete with and dilute the genetic fitness of wild populations, but without supplementation, some runs might disappear entirely.

4. Marine Mammals

Residents and Visitors of Puget Sound

Species Status When Where to Look from Mukilteo
Harbor Seal Resident Year-round Jetty Island haul-outs; marina docks; ferry terminal rocks
Steller Sea Lion Winter Visitor Oct–Apr Occasionally on navigational buoys in Possession Sound
Gray Whale Spring Migration Mar–May Occasionally enters Puget Sound; more common in outer straits
Humpback Whale Recovering Increasing presence More frequent since population recovery; seen in main basin
Harbor Porpoise Resident Year-round Small, shy, low profile; rarely seen but always present

Harbor Seals: The Locals

Harbor seals (Phoca vitulina) are the most common marine mammal in the Salish Sea, with an estimated population of 14,000+ in Washington waters. They haul out on Jetty Island — the sandbar directly across from Mukilteo's waterfront — to rest, thermoregulate, and nurse pups.

Pupping season runs from June through September. During this time, apparently "abandoned" pups on shore are almost always waiting for their mothers to return from foraging. The standard guidance: observe from 100+ feet, never touch.

The Return of Humpbacks

Humpback whales were hunted to near-extinction in the North Pacific. Since the moratorium on commercial whaling (1966 for humpbacks), populations have recovered dramatically. Their increasing presence in the Salish Sea — rare before 2010, now seen regularly — is one of the clearest marine conservation success stories in the region.

However, their return creates new challenges: humpbacks feeding in the same waters as heavy commercial shipping face entanglement and strike risks. The recovery of one species reveals the complexity of managing an ecosystem, not just individual populations.

5. Tidal Ecology

Mixed Semidiurnal Tides

The Salish Sea experiences mixed semidiurnal tides — two high tides and two low tides each day, but with unequal heights. This is exactly what our NOAA station 9447659 measures at Mukilteo. The "mixed" part comes from the declination of the moon: when the moon is north or south of the equator, the two daily highs (and two lows) differ in height.

Typical tidal range at Mukilteo: 2.5–4.0 meters (8–13 feet). Extreme tides during king tides can exceed 4.5 meters.

Intertidal Zones

The intertidal zone — the strip of shore exposed and submerged by tides — is organized into bands defined by how much air exposure each level tolerates:

Zone Exposure Key Species Character
Splash Zone Above highest tide Lichens, periwinkles, limpets Salt spray only; extreme desiccation tolerance
High Intertidal Submerged only at high tide Barnacles, shore crabs, rockweed Hours of air exposure daily
Mid Intertidal Regularly covered and exposed Mussels, anemones, ochre sea stars Highest biodiversity zone
Low Intertidal Exposed only at low tide Sea urchins, bull kelp, eelgrass, nudibranchs Nearly marine; richest habitat

Eelgrass Meadows: The Underwater Nurseries

Eelgrass (Zostera marina) is not a seaweed — it is a true flowering plant that grows underwater, forming dense meadows in shallow, protected waters. These meadows are critical nursery habitat for juvenile salmon, herring, and hundreds of invertebrate species.

Eelgrass provides structure (hiding places from predators), food (epiphytic algae on the blades), and oxygen (photosynthesis). It also stabilizes sediment, reducing erosion. The Snohomish River estuary supports some of the most extensive eelgrass beds in Puget Sound.

Why this connects to everything: Juvenile Chinook salmon shelter in eelgrass meadows before heading to open water. Those Chinook grow into the adults that Southern Resident orcas depend on. Eelgrass health is, indirectly, orca health.

Sea Star Wasting Disease

Between 2013 and 2016, a devastating epidemic called Sea Star Wasting Syndrome (SSWS) swept the Pacific coast from Alaska to Baja California. Affected sea stars developed lesions, lost limbs, and disintegrated within days. The ochre sea star (Pisaster ochraceus) — a keystone predator that controls mussel populations — was especially hard hit.

Puget Sound populations were devastated. The cause was identified as a densovirus (Sea Star-associated Densovirus, SSaDV), potentially triggered or amplified by warming water temperatures. Recovery has been slow and uneven. The loss of sea stars allows mussels to dominate, squeezing out other intertidal species — a textbook demonstration of keystone predator effects.

6. Water Quality

The State of Puget Sound

The Puget Sound Partnership, established in 2007, is the state-led effort to recover the health of Puget Sound by 2050. The partnership coordinates across hundreds of agencies, tribes, and organizations to track and address the ecological indicators that define Sound health: orca population, salmon returns, water quality, habitat extent, and human well-being.

The uncomfortable reality: despite decades of effort and billions in investment, most indicators are flat or declining. The Sound is not getting healthier at the pace needed.

Pollution Sources

Source Rank Key Pollutants Pathway
Stormwater Runoff #1 Heavy metals, petroleum, microplastics, 6PPD-quinone Rain washes roads, roofs, parking lots into streams and Sound
Wastewater #2 Nutrients (N, P), pharmaceuticals, microplastics Treatment plant outfalls and combined sewer overflows
Agricultural Runoff #3 Nutrients, pesticides, fecal coliform Field drainage to rivers to Sound (Skagit, Snohomish valleys)
Industrial Legacy #4 PCBs, PAHs, heavy metals Contaminated sediments from historical industrial activity

6PPD-quinone: The Tire Chemical Killing Coho

In 2020, researchers at the University of Washington identified 6PPD-quinone — a chemical produced when the common tire preservative 6PPD reacts with ozone — as the cause of decades of unexplained Coho salmon die-offs in urban streams.

The discovery is remarkable for several reasons:

Connection to our weather data: Rain intensity directly predicts stormwater pollution events. A heavy rainstorm after a dry spell produces the worst first-flush effect — maximum accumulated pollutant load washed into streams. Our precipitation data from the Mukilteo observatory isn't just about weather; it's a proxy for pollution timing.

Shellfish Growing Areas

Water quality in the Salish Sea directly determines whether shellfish can be safely harvested. The Washington State Department of Health classifies shellfish growing areas based on fecal coliform bacteria levels — the standard indicator of human health risk from contaminated water.

When rain events overwhelm stormwater systems or trigger combined sewer overflows, shellfish beds are closed. These closures are the most immediate, visible connection between land use, weather, and marine ecosystem health. Every impervious surface in the watershed — every road, roof, and parking lot — contributes to the runoff that closes the beds.

Why This Matters for Mukilteo Observatory

Every data stream we collect at the Mukilteo Observatory connects to the Salish Sea ecosystem:

Our Data Source Ecological Connection
Tide levels NOAA 9447659 Intertidal habitat exposure; eelgrass light availability
River flow USGS 12150800 Salmon migration conditions; freshwater input to Sound
Precipitation Weather models + KPAE Stormwater pollution timing; 6PPD-quinone flush events
Temperature Weather models + KPAE Marine heat stress; dissolved oxygen levels in rivers
Wind Weather models + KPAE Surface mixing; vessel traffic safety; whale-watch conditions

A microclimate observatory is not just a weather station. It is a lens into the health of the ecosystem where atmosphere, freshwater, and ocean meet. Understanding the Salish Sea gives every data point we collect its ecological context.