Kelp Forests of Catalina Island: A Coastal Atlas Guide
Catalina Island is southern California's kelp capital — Casino Point, Farnsworth Bank, warm-water giants and a century of marine science under the canopy.
Dr. Mara Ellison ·
A guide to the giant kelp beds of Malibu and Santa Monica Bay — their history, decline, restoration wins and the best ways to see them today.
On a February morning with north wind combing the water flat, you can stand on the bluff above Point Dume and watch something that shouldn't exist beside a city of ten million: a kelp canopy, dark as spilled ink, folding over each swellline as the sets arrive. Dolphins cut through it. A gray whale mother rises inside it. Beneath that floating roof, giant kelp stipes climb twenty metres of green-gold water to one of the busiest coastlines in the world.
Malibu's kelp coast is a good place to learn everything at once — what these forests were, what took them down, and what it actually takes to bring them back.
Historically, giant kelp (Macrocystis pyrifera) formed an almost unbroken band along the Southern California coast from Point Conception to the Mexican border, wrapping around every rocky point and island. The big offshore beds of Point Loma, Catalina and the Santa Barbara Channel survived into the modern era; the inshore, urban beds of Santa Monica Bay — the forest that beaches at Santa Monica, Malibu and the Palos Verdes bluffs once faced — did not fare as well.
The bay's decline was a compounding story. Sewage outfalls through the mid-twentieth century degraded water quality and smothered rocky substrate. Warm-water years, especially the strong El Niño winters of 1957–59 and 1982–84, stripped the canopy, and purple sea urchins — their predators long fished down for the urchin roe industry — scythed through recruits faster than kelp could recover. By the 1990s much of the urban bay floor had become urchin barren: reefs crawling with well-fed but reproductively arrested urchins, and almost no canopy left.
Malibu's own beds, at Point Dume, Leo Carrillo and the rocky pockets around Malibu Point, hung on better. The headlands sit farther from the heaviest urban runoff and benefit from cooler, cleaner swells rounding Point Conception's shadow into the Channel. But even these forests have run thin and thick in cycles — hammered by marine heatwaves in 2014–2016 and again by warm spells since, skinned down to stipes, then regrowing in cool La Niña years.
Two ingredients keep Malibu forest-friendly despite the city at its back: rock and water.
The rock is volcanic and sedimentary bluff material of the Santa Monica Mountains, shearing into the sea at Point Dume, Leo Carrillo and the coves of El Matador. Giant kelp needs hard, stable substrate to anchor its holdfast — and Malibu's reefs deliver it at exactly the 8–30 metre band where Macrocystis does its best work.
The water is the second gift. The California Current brings cold, nutrient-rich water south along the coast, and spring up-winds and upwelling pulses keep nitrate high through the growing season. The canyon of Santa Monica Bay and the deep Pacific beyond act like a reservoir of cool water just offshore; even a bad warm spell rarely warms the bottom offshore enough to cook the adults outright.
The third, more recent ingredient is people. A decades-long urchin-removal and outplanting program on the Palos Verdes side of the bay has transformed hundreds of acres of barren reef back into visible canopy — one of the most-cited urban kelp restoration successes anywhere. Divers have removed millions of purple urchins from barrens, and kelp responded within two to three years. Malibu's points sit inside this arc of recovery; each cool year since has spread canopy a little farther along old forest ground.
The wildlife value of an urban kelp forest is easier to see than to believe: - Sea lions haul on the bait barges off Malibu Pier and porpoise through the canopy on calm mornings.
The forest also acts as a nursery. Juvenile rockfish recruit into the canopy rafts of drift kelp; young lobsters shelter in the root zone. Remove the canopy and you remove an entire class of habitat. This is why the bay's restoration story matters well beyond Malibu — see our wider look at Los Angeles-restoration lessons on the Catalina guide, and at why kelp losses and gains ripple through coastal fisheries in the urchin-barrens explainer.
Summer and early autumn (July–October) are the classic windows. Water temperatures reach the mid-to-high teens Celsius, visibility runs 3–10 metres inshore and better at the Channel-side points, and the forest is at or near its annual peak height. By late summer, longbeach commons dolphins, leopard sharks and schools of Pacific sardine are working the canopy edges.
Winter (November–February) brings big northwest swell and murkier water, but also the clearest air and migrating gray whales threading through the kelp line. Storms can strip canopy; a big January swell can shear weeks of growth off in a night.
Spring (March–May) is reset season: cooler water, new recruits, and garibaldi beginning to nest.
To actually see the forest:
Malibu has all the textbook pressures at once: - Marine heatwaves. The 2014–2016 "Blob" years shaved canopy hard; recent warm seasons have done the same in pulses. Kelp here has no deep-cold refuge the way it does on Point Loma — the whole forest rides within the warmed layer.
Every one of these is a measured pattern, not a forecast. Malibu's bed is, in the language Tidewright's field teams use for their own illustrative monitoring work, a sentinel forest: urban, exposed, and a leading indicator of how the whole Southern California Bight will respond to a warming California Current.
There is still kelp. Giant kelp beds persist along Point Dume, Leo Carrillo and pockets of the Malibu shore, though coverage swings year to year with temperature and storms. In strong La Niña years the canopy can expand dramatically; in heatwave years it contracts sharply.
Yes — on calm days the canopy is visible as dark patches on the surface from bluffs at Point Dume and several overlooks along Pacific Coast Highway. Drift kelp also washes up on local beaches after storms.
Late summer through early autumn (roughly August to October), when water temperatures are highest, days are calmest, and the canopy is tallest. Winter diving can be excellent after long dry stretches, but swell quickly kills visibility.
A compounding of mid-century sewage outfalls, repeated strong El Niño events stripping canopy, urchin grazers unchecked after their predators were fished down, and more recent marine heatwaves. Urban runoff and canyon sediment post-fire add chronic pulses of stress.
Yes. A long-running coalition of divers, agencies and NGOs has removed purple urchins from barrens and outplanted kelp across the broader Santa Monica Bay, with canopy returning over hundreds of acres. The city's kelp story is now a model studied worldwide — and a benchmark for the kind of large-scale restoration Tidewright's work aims to extend.
Catalina Island is southern California's kelp capital — Casino Point, Farnsworth Bank, warm-water giants and a century of marine science under the canopy.
Dr. Mara Ellison ·
Where cold northern and warm southern currents collide, the Channel Islands grow California's grandest kelp forests — protected by national park and marine reserves.
Sofia Andersson ·
The Point Loma kelp forest off San Diego is one of the largest and most-studied giant kelp beds on Earth — a story of pollution, recovery and scientific devotion.
Dr. Mara Ellison ·