Sampling Gulf Stream plankton, one teaspoon at a time
Three questions with marine research technician Emily Peacock
These seabirds fly toward cyclones, not away from them
New GPS tracking on petrels reveals a surprising survival strategy hidden in the eye of the storm
Reclaiming knowledge from the sea
WHOI’s Jordan Kennedy draws on Indigenous knowledge, engineering, and observation to rethink how we study and restore coastal landscapes
3 questions with a former NASA astronaut
WHOI Corporation Member Sunita Williams discusses space exploration, ocean science, and environmental stewardship
Ships in the Strait of Hormuz are becoming invasive species breeding grounds
Beneath the waterline of every ship stalled in the Persian Gulf, a thriving underwater city takes shape—barnacles, algae, mussels, sea squirts. Some of those hitchhikers could reach coastlines they’d never find on their own.
Is the ocean carbon sink at risk of faltering?
WHOI scientists explain how the ocean mitigates climate change—and could be compromised by it
3 questions with Cam Braun
Marine biologist Camrin Braun explains why the world’s largest fish visit waters off Cape Cod—and what their epic migrations reveal about a changing ocean
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Our Ocean. Our Planet. Our Future.
Is underwater noise from construction affecting the American Lobster?
WHOI’s Sensory Ecology Lab investigates whether an industrialized soundscape impacts the health of a New England icon
Exploring Atlantic seeps
AUV Sentry leads the way in mapping and monitoring methane bubbling from the seafloor
A once-in-a-generation dive into polar history
40 years after helping reveal the Titanic, Alvin returns to the North Atlantic to document two other legendary shipwrecks
A hadal zone mystery solved
An upside-down swimming isopod shows how tightly we are connected to the deep ocean
A mother seal dives
Follow a Weddell seal as her body adapts to foraging in deep, frigid waters
A mummy, a myth, and the Titanic
A 1986 handwritten letter to Bob Ballard revisits one of the Titanic disaster’s strangest myths
Turning motion into power: Wave energy converters for sustainable ocean monitoring
In the rapidly evolving world of ocean technology, wave energy is emerging as a promising…
The world’s most abundant fish once thrived in an extreme climate
Fossilized teeth show bristlemouth fish evolved during one of the ocean’s hottest periods
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How a cargo ship is tracking hidden ocean life in the Atlantic
With funding support from CMA CGM, ocean observations aboard Bermuda Container Line’s M/V Oleander now include a window into microscopic life
Alvin vs. the swordfish
During a 1967 dive off Florida, a startled swordfish rammed the famed submersible Alvin—lodging its sword in the hull and forcing the crew to abort the mission
Inside Room 71: WHOI history in seven artifacts
Some of the technology, art, and gifts that tell the story of the institution’s early days
A scientist’s quest to find Earth’s oldest ice
After recovering ice that dates back 6 million years, Sarah Shackleton hopes to dig deeper into Earth’s history from a remote Antarctic moraine
It’s the most ocean-friendly map ever created. Why haven’t more people seen it?
Discover the Spilhaus Projection, a radical world map that reveals Earth as one connected ocean—and reshapes how we see the planet.
Luxury cruises with a side of climate science
A new partnership gives scientists rare access to remote Antarctic glaciers—and a new way to engage the public
The unseen toll of war on science
As the changing climate accelerates the spread of toxic algal blooms in the Arctic, the Russia–Ukraine war is cutting off critical international collaboration needed to understand and protect vulnerable ecosystems and communities.
The human cost of Brazil’s floods
New research maps social vulnerability after the 2024 deluge
Catching the Rain: Sediment Trap Technology
WHOI Senior Engineer Ken Doherty developed the first sediment trap in the late 1970s for what has come to be known as the WHOI PARFLUX (for “particle flux”) group. Working closely with the scientific community, Doherty has continued to improve sediment traps for two decades, and these WHOI-developed instruments are widely used both nationally and internationally in the particle flux research community.
Replacing the Fleet
When R/V Atlantis arrived in Woods Hole for the first time on a bright, beautiful April 1997 day, it represented not only a welcome addition to the WHOI fleet but also the culmination of a 15-year UNOLS fleet modernization.
WHOI and Access to the Sea
In the mid-term future, two WHOI ships (Knorr in about 2006 and Oceanus in about 2009) will reach the end of their planned service lives. There is general agreement that WHOI should work to replace them with two vessels.
A Northern Winter
As the 1996-1997 ship schedule began to take shape in 1995, we learned that Voyage 147 would take R/V Knorr into the North Atlantic from October ’96 through March of ’97. The various science missions would require station keeping during CTD casts, deployment of current drifters, and expendable bathythermograph (XBT) launches, as well as weather system analysis designed to put Knorr in the path of the harshest weather conditions possible during the winter season. Long before the cruise, we began to tap all available assets that would help us with this challenge.
Adventure in the Labrador Sea
The sound of the general alarm bell reverberated through the ship. At 2:30 AM, this couldn’t be a drill. Even more puzzling, we were still dockside in Halifax, four hours from our scheduled departure for the Labrador Sea.
“What a Year!”
Four technologies that have been developing separately for some time were brought together this year by WHOI’s Deep Submergence Laboratory (DSL) to serve three very different user communities. With images from the towed vehicle Argo II and the remotely operated vehicle Jason, DSL scientists and engineers created mosaic images of a sunken British cargo ship and 20-meter-tall hydrothermal vent chimneys, both in the Pacific Ocean, and ancient shipwreck sites in the Mediterranean. The three expeditions thus served the marine safety, scientific, and archaeological communities.
Access to the Sea
Oceanographic fieldwork has traditionally meant going to sea on a ship. In recent years, it has expanded to include activities that may require a ship for a short period but then continue independently. Floats that drift with ocean currents, periodically reporting their positions via satellite, for example, are generally launched from ships but do most of their work independently. Long-term seafloor observatories may need ships to set them up and service them occasionally, but, again, they are designed to collect data for long periods without needing a ship. We have come to think of the body of ways oceanographers glean information from the ocean as “access to the sea,” and so that is the topic for this issue of Oceanus.
The Magnetic Thickness of a Recent Submarine Lava Flow
Submarine lava flows and their associated narrow feeder conduits known as dikes constitute the basic building blocks of the upper part of the ocean crust. We are only beginning to understand how lava erupts and forms on the seafloor by flooding topographic lows, flowing through channels or tubes, centralizing into volcanoes, or some combination of all of these.
New Data on Deep Sea Turbulence Shed Light on Vertical Mixing
The global thermohaline circulation is basically a wholesale vertical overturning of the sea, driven by heating and cooling, precipitation and evaporation.
Labrador Sea Water Carries Northern Climate Signal South
Changes in wind strength, humidity, and temperature over the ocean affect rates of evaporation, precipitation, and heat transfer between ocean and air. Long-term atmospheric climate change signals are imprinted onto the sea surface layer, a thin skin atop an enormous reservoirA? and subsequently communicated to the deeper water masses. Labrador Sea Water is a subpolar water mass shaped by air-sea exchanges in the North Atlantic. It is a major contributor to the deep water of the Atlantic, and changes of conditions in its formation area can be read several years later at mid-depths in the subtropics. Mapping these changes through time is helping us to understand the causes of significant warming and cooling patterns we have observed at these depths in the North Atlantic and links the subtropical deep signals back to the subpolar sea surface conditions.
North Atlantic’s Transformation Pipeline Chills and Redistributes Subtropical Water
Warm and salty waters from the upper part of the South Atlantic flow northward across the equator and then progress through the tropical and subtropical North Atlantic to reach high latitudes. Beginning with the intense northward flow of the Gulf Stream off the East Coast of the United States, these waters are exposed to vigorous cooling, liberating considerable oceanic heat to the atmosphere. This is the first stage of “warm water transformation within the North Atlantic, a process that culminates in the high latitude production of cold and fresh waters that return to the South Atlantic in deep reaching currents beneath the warm waters of the subtropics and tropics.
If Rain Falls on the OceanDoes It Make a Sound?
As with similar questions about a tree in the forest or a grain of sand on the beach, it may be hard to imagine that a few inches of rain matters to the deep ocean.