Central Puget Lowland

A single American Golden-Plover (*Pluvialis dominica*) has been on the tideflats at Tulalip Bay, on the Tulalip Reservation north of Everett, since September 13. The species passes through Washington in small numbers every fall, mostly along the outer coast at places like Grays Harbor. Around Puget Sound it turns up a bird or two at a time, and a single one on a bay like this is the usual showing. It is a slim, mid-sized plover, bigger than a Killdeer and a little smaller and lighter-built than the Black-bellied Plovers that spend the winter on these same flats. The bill is short and fine. Most of the golden-plovers moving through in September are birds hatched this summer, and a juvenile is neatly spangled above, each back feather fresh and edged in gold and buff so the whole upper side looks scaled. A dark cap sits over a broad pale eyebrow. The throat is white, the breast gray-brown and streaked, the belly white. The Black-bellied Plover is the bird it will most often stand beside here, and the flight view settles it. Black-bellied shows a black patch in the wingpit and a white rump and tail. The golden-plover's underwing is plain gray, and its rump and tail are dark, the same tone as the back. On a standing bird, the golden-plover's wingtips reach well past the tail and the whole bird reads longer and leaner. The harder separation is from Pacific Golden-Plover, which also reaches this coast in fall. Underwing color is no help; both are gray there. The test is the folded wing. On an American, four or five wingtip feathers show beyond the longest tertials at rest and the wingtips extend half an inch or more past the tail. On a Pacific, only two or three show and the wingtips barely clear the tail. American is also a shade duller on the face and neck, and its call is a plaintive two-note "chew-ee" with the stress on the first syllable. The way it feeds shows what kind of bird it is. Golden-plovers hunt by eye, not by touch. The bird runs a few steps, stops, scans the mud, and picks. Dunlin and godwits on the same flat work by feel, probing below the surface with their bills. The plover needs open ground where it can see its prey, and on a tideflat that means small crustaceans and mollusks sitting on top of the mud rather than buried in it. Its presence here in September follows from the shape of its year. American Golden-Plovers nest on low Arctic tundra from Baffin Island west to the Bering Strait. The adults leave in early summer, before their young can fly. Most of them cross to the Atlantic seaboard and launch straight out over the ocean toward northern South America, a nonstop flight that tagged birds have covered in a single 3,100-mile push. The juveniles follow weeks later, on their own, with no adult to lead them. They scatter more widely, and some work down the Pacific coast, which is how one ends up on a Snohomish County mudflat in mid-September. From here the destination is the grasslands of Argentina and Uruguay. In spring the whole population comes north by a different road, up through the Great Plains and the Mississippi Valley, and the species is rarely seen on this coast at all. Fall is the season to look.

Chinook salmon are back in the lower Sammamish River. Over the past four weeks they have been seen along the slow, dredged reach that runs from Kenmore through Bothell toward Woodinville, with a scattering of other sightings toward Edmonds and across the Sound on the Kitsap side. These are adults on the last leg of a trip that began in the North Pacific and passed through the Ballard Locks sometime this summer. The Chinook (Oncorhynchus tshawytscha) is the largest of the Pacific salmon and the easiest to name with the fish in hand: black gums along the lower jaw where a coho's are white, and small dark spots across both lobes of the tail rather than just the upper one. In salt water they are silver with a blue-green back. By the time they reach a river like this one they are darkening to bronze and olive, the males growing the hooked snout and heavy teeth they will use to fight for position on the gravel. Lake Washington fish typically run ten to twenty-five pounds, three to five years old. What they are doing right now is mostly waiting. Adults enter Lake Washington through the locks from June into September and hold in the lake's cooler depths, then push up the Sammamish toward Bear Creek, Cottage Lake Creek and Issaquah Creek to spawn from mid-September into November. The Sammamish is the bottleneck. It was straightened and dredged in the 1960s, runs shallow and slow through open valley floor, and is one of the warmest salmon rivers in the region in late summer. Fish moving through it in August and early September are traveling in water that regularly sits near the twenty-degree mark where migrating salmon start to burn energy they cannot spare. Cooler nights and the first fall rains are what open the door upstream. Snohomish County's dry spell, described here two weeks ago, has not let up; a little over half the county has sat in moderate drought since the third week of August, and the past month at Paine Field ran about 2.7 degrees above normal for daily highs. Those numbers describe the air and the land, not the river, and no current gauge reading on the Sammamish was available to say how the water itself is running. The fish are in it regardless. Once they spawn, Chinook do the thing no other family of fish does at this scale: they die on the gravel and stay. A single carcass feeds bears, otters, eagles, gulls, dippers and the insects the next generation of fry will eat; the nitrogen from an ocean life ends up in streamside alders and cedars. The eggs overwinter in the gravel, the fry emerge in late winter, and most of this run's young will spend only a few months in fresh water before dropping down through the lake and out the locks, small enough to fit in a palm. Puget Sound Chinook have been listed as threatened under the Endangered Species Act since 1999, and the Lake Washington run is among the more heavily worked-on in the region. Adopt A Stream Foundation does its stream restoration from North Creek in Everett, a tributary that meets the Sammamish at Bothell, right in the stretch where these fish were seen. Anyone who wants to watch the run can do it without waders. The fish ladder windows at the Ballard Locks show Chinook passing into the lake through September, and by early October they will be on the gravel in Bear Creek and Issaquah Creek, where a footbridge is all the equipment needed.

Snohomish County has gone from essentially drought-free to fully dry in a single summer. As of late April, no part of the county registered even the lowest tier of the U.S. Drought Monitor's dryness scale. By the first two weeks of August, that lowest category, Abnormally Dry, covered the entire county wall to wall. A smaller slice, about 2.6 percent of the county's land area, tells a sharper story. That pocket first crossed into Moderate Drought in mid-July and has now held at or above that threshold for a full month straight, without tipping further into Severe Drought. This is a sustained trend tracked week over week on a consistent measure, not a one-off reading, which makes the month-long persistence more meaningful than the raw percentage suggests. The dryness lines up with what's been showing up on the ground all season in the Central Puget Lowland: vine maples were already coloring by mid-July, bunchberry fruited three weeks ahead of schedule, and goldenrod bloomed a full six weeks early. None of these phenology shifts can be attributed to drought specifically without more direct evidence, but a hot, moisture-starved summer is exactly the kind of stress that pushes plants toward early senescence and fruiting. No direct streamflow readings were available this cycle to confirm how the drought is affecting local waterways, but sustained dryness like this is worth watching for its potential effects on salmon habitat, the kind of condition Adopt A Stream Foundation tracks in local streams through the season. Separately, this cycle's regulatory water quality checks on discharge permits in the county, including the Everett Ship Repair facility's permit, haven't flagged any new impairments. The drought, not a discharge event, is the story to watch here this summer.

Copper discharge from the Puget Sound Naval Shipyard in Bremerton has now exceeded its Clean Water Act permit limit for two consecutive quarters, and the trajectory is the notable part: 24% over limit in the quarter ending December 2025, then 101% over limit the following quarter, a roughly fourfold jump in a single reporting period. The outfall empties into Sinclair Inlet, a working embayment that drains directly into central Puget Sound. Copper is a slow, subtle poison rather than an acute one, which is exactly why it deserves attention at these levels. Research on juvenile coho and Chinook Salmon has shown that dissolved copper impairs their sense of smell at concentrations well below what would otherwise be considered dangerous. Salmon depend on olfaction to detect predators and to navigate home to spawn; a fish doesn't need to be poisoned outright to have its odds quietly worsened. That relationship between smell and survival is precisely why copper limits are set where they are, and it's why blowing past one by double is a materially different problem than nudging over it. The pattern isn't confined to one outfall. King County's West Point Treatment Plant, near Discovery Park on the same stretch of Puget Sound, logged a strikingly similar arc over the identical two quarters, exceeding its zinc limit by 95% and then 128%. Two of the largest permitted dischargers into central Puget Sound worsening on different metals over the same span is a signal worth taking seriously in its own right, even before any water-quality sampling confirms measurable effects on fish moving through these waters.

Vine maple (Acer circinatum) has begun turning color by mid-July — a shift that typically doesn't occur until September or October when fall rains return and the light angles lower. This is not an isolated quirk. Beaked hazelnut (Corylus cornuta) is coloring, Canada goldenrod (Solidago canadensis) bloomed six weeks ahead of schedule, and bunchberry dogwood (Cornus canadensis) has already completed its fruit cycle by mid-month. These events are moving through the understory in tandem, a pattern of heat stress rather than scattered phenological variation. Vine maple is one of the most structurally important trees in the Pacific Northwest understory, forming the mid-canopy shade that keeps stream banks cool and shelters the shallow pools where juvenile coho and cutthroat spend their first summers. Early senescence now means that canopy shade — already weakened by a warm July — begins to fail months before fall rains arrive to replace it. The consequence reaches deeper than the forest floor: young fish in streams across the region are losing thermal refuge precisely when they need it most.

Canadian bunchberry (Cornus canadensis) has ripened to red fruit in just three weeks — completed July 12 — while kinnikinnick berries are coming in alongside it. The acceleration is matched by Canada goldenrod, which opened July 13, nearly six weeks ahead of its typical late-August bloom. Mid-July here is a narrow fruiting window—thrushes and cedar waxwings have only days to exploit this brief pulse of seed and sugar before the resource passes. Earlier phenology is compressing the timeline for migrants and residents alike, testing whether their movements stay synchronized with the plants they depend on.

Juvenile salmon are moving through Puget Sound this season, their olfactory systems primed to detect the chemical signatures that will guide them home. It is a critical window — and right now, the region's largest sewage treatment plant is sending zinc into that same water at more than one and a quarter times its permitted level, sustained through two consecutive quarters. Zinc at sub-lethal concentrations impairs salmon olfaction directly, dulling the very sensory pathway they depend on to navigate. The West Point facility violations are chronic rather than dramatic — no single catastrophic spill, just sustained exceedance — which means they rarely make headlines. But the harm is no less real. Impaired homing means lost fish, reduced returns, and stress on populations already pressed by dams, temperature, and development. What happens in the outfall reaches far upstream, year after year.

Ochre sea stars (Pisaster ochraceus) are spreading across the low intertidal again this week, from Alki to Port Orchard, their brick-red bodies exposed in numbers on the extreme low tides of late June. For nearly a decade after sea star wasting disease swept through in 2013, they vanished almost entirely from these shores. Seeing them at so many sites now—over two hundred confirmed this past week—is slow recovery made tangible, a return to the ecological baseline that makes the difference between a thriving intertidal and one that has collapsed into monoculture. Their recovery matters because sea stars are keystone predators. Ecologist Robert Paine showed that without them, mussels overwhelm the rock face, crowding out the intricate community of smaller herbivores, filter-feeders, and grazers that once gave intertidal pools their visual and ecological richness. These starfish don't just live here—they architect the entire system. Watching them return is watching an ecosystem remembering how to sustain itself.

In the shaded understory of Bainbridge Island's second-growth forest, the ground is white right now. Not snow, not frost, but bunchberry dogwood in full bloom, its flowers open across the forest floor in dense, low mats that catch whatever light filters through the vine maple and redosier dogwood overhead. The blooms are small, a cluster of tiny true flowers surrounded by four white bracts that do the visual work of attracting visitors. Individually they are modest. Collectively, spread across meters of damp ground, they are a significant food source at a moment when the forest needs one. Bunchberry dogwood is a ground-level plant, rarely more than twenty centimeters tall, and it spreads by rhizome into loose colonies across moist, shaded forest floor. What it lacks in height it makes up in density. Each cluster of white bracts frames a tight center of small flowers, and those flowers produce nectar and pollen over a bloom period that coincides almost exactly with the longest days of early summer. The timing matters. This is when aquatic insects are emerging from nearby streams and wetlands, when the forest canopy is thick with flying invertebrates, and when every nesting bird on the island is making repeated foraging trips to feed protein to nestlings. The bunchberry adds to that supply. Not dramatically, but consistently, and at the right moment. The flowers attract small bees, flies, beetles, and wasps, including the invasive European paper wasp, which forages widely across the understory this time of year. These visitors collect pollen and nectar, and in doing so transfer pollen between plants. The pollination mechanism in bunchberry is worth knowing: the flowers are spring-loaded. When a visiting insect contacts the stamens, the anthers release pollen explosively, coating the visitor in under half a millisecond. It is one of the fastest movements in the plant world. The insect moves on, dusted with pollen, and the plant's reproduction moves with it. Look closely at the center of an open flower cluster and you may see the spent anthers, already triggered, curled outward. What the insects carry away, the birds collect indirectly. Chestnut-backed chickadees are nesting now, and they forage heavily on the small insects that gather at flowering plants like this one. Spotted towhees work the leaf litter nearby, turning over debris in search of invertebrates. Bewick's wrens move through shrubby tangles at the forest edge, taking flies and small beetles. These birds are not visiting the bunchberry directly; they are harvesting the insects that the flowers have concentrated. The plant functions as a gathering point, and the gathering feeds the next layer up. Later in the season, bunchberry will produce tight clusters of bright red fruit, and those same birds will return for a different reason entirely. Right now, though, it is the flowers doing the work. The forest floor here holds other plants in bloom or coming into bloom. Common snowberry is opening its small pink flowers along the edges of the understory, and ocean spray is building toward its own peak further out in the drier, more open areas. But bunchberry is the one flowering at ground level, in the shade, where the soil stays cool and damp. That niche is specific. The insects that work low and slow through shaded forest find it reliably. If you are standing near a patch right now, crouch down and watch the flower clusters for thirty seconds. The visitors are small and quick, but they are there.

The rocky shore at Winslow lies exposed under the long light of early summer. Water drains from the tide pools in sheets, leaving dark stones slick and glistening. The air carries the salt tang of kelp and the sharp mineral scent of wet granite. If you are walking these shores, notice how the retreating water reveals a landscape that was hidden just hours before. Among the barnacle-crusted rocks, orange and purple forms grip the stone with hundreds of tube feet. These are ochre sea stars, and they are hunting. Each star moves with deliberate slowness, flowing over the uneven surface of the intertidal zone. Their arms probe crevices and gaps where California mussels cluster in dark blue masses. The mussels pull tight against their shells when touched, but the sea stars are patient. They position themselves over a mussel bed and begin to pull. Two arms anchor against the rock while the others wrap around a single mussel, applying steady pressure that can last for hours. The mussel's muscles tire before the sea star's grip weakens. When the shell opens just a crack, the sea star pushes its stomach through its mouth and into the gap, digesting the mussel from the inside. This hunt shapes everything else on these rocks. Without ochre sea stars, mussels would carpet every available surface, crowding out barnacles, anemones, and the small algae that feed dozens of other species. The sea stars create space by removing the most successful competitor, allowing aggregating anemones to spread their tentacle crowns in the cleared patches, and giving small crabs room to scuttle between the remaining mussel clusters. Each hunting sea star maintains a small clearing in what would otherwise become a mussel monoculture. The pattern repeats across every stretch of rocky shore from Alaska to California. Remove the sea stars, and the diversity collapses within months. Their presence keeps the intertidal zone open and complex, a patchwork of different organisms rather than a single dominant species. The relationship extends beyond mussels. Sea stars also hunt barnacles, limpets, and chitons, but mussels remain their preferred prey when available. During these long summer days, with extended low tides exposing the hunting grounds for hours, the sea stars can reach prey that remains submerged during winter's brief low tides. The timing matters. Early summer brings the year's most accessible feeding, when the combination of daylight and tide cycles allows the deepest reaches of the mussel beds to emerge into air. The water returns gradually, first as a thin film spreading between the rocks, then deeper until it covers the hunting grounds again. You can hear it before you see it, a quiet rushing that grows louder as the tide fills the channels between boulders. The sea stars continue their slow work even as the water rises around them, their orange arms still wrapped around blue shells, still applying that patient, inexorable pressure that keeps these shores diverse and open.