Ocean acidity is rising due to increasing carbon dioxide levels, posing a threat to marine life such as corals and shellfish. The study suggests that future changes in ocean acidification are largely independent of climate change.
A feedback mechanism between North Atlantic and tropical hydrology of Central America amplifies the effects of climate change on oceanic circulation. This mechanism, highlighted by scientists at CEREGE1, shows that changes in oceanic circulation influence global water cycle patterns and climatic equator shifts.
A delayed arrival of cold, nutrient-rich water due to altered ocean currents led to reduced barnacle and mussel larvae settlement on rocky shores. The change resulted in lower phytoplankton abundance and a recovery of mussel recruitment when stronger nutrient-rich currents arrived later.
New satellite data show that ocean warming is reducing phytoplankton growth, imperiling ocean fisheries and marine life. Phytoplankton are responsible for about the same amount of photosynthesis as all plants on land combined, making their decline a significant threat to the food chain.
A new climate model predicts that the Southern Ocean's absorption of heat and carbon dioxide will slow the rate of global warming. The ocean's ability to sequester heat and carbon dioxide could lead to sea level rise, but also change the chemistry of the water, making it less habitable for some marine organisms.
Scientists reconstructed a 45,000- to 60,000-year-old record of ocean temperature and salinity using chemical traces in fossil shells. They found the Atlantic got saltier during cold periods and fresher during warm intervals.
Research finds rapid changes in North Atlantic Ocean salinity linked to sudden shifts in Greenland temperatures and tropical rainfall patterns during the last ice age. This provides evidence that climate change can have a direct and rapid impact on ocean circulation and chemistry.
Scientists have documented unprecedented warmth in the Arctic Ocean, with recent surges of warm water from the North Atlantic Ocean continuing to pulse into the region. This increase in warm water could lead to a warmer state in the Arctic Ocean, affecting global climate patterns.
Researchers analyzed temperature and salinity data from sensors along the Southern California coast to detect changes in water quality. They found that fluctuations in sensor data correlate with changes in water quality, allowing for near real-time detection methods.
Scientists determined that nitrogen is the primary element missing for algae growth in the northern tropical Pacific, while iron was lacking everywhere else. The 'iron-effect' decreases carbon ocean plant photosynthesis estimates by two billion tons, allowing for more accurate carbon movement modeling and resource management.
A new study found that large segments of the Pacific Ocean lack sufficient iron to trigger healthy phytoplankton growth, leading to overestimated ocean productivity. The researchers estimate a 2-4% reduction in global ocean carbon uptake due to this oversight.
A sensor package is installed on Cape Cod ferry Katama to measure water temperature, salinity, oxygen levels, and take images of plankton. The project aims to build a detailed portrait of changing water conditions in Nantucket Sound over long time scales.
A new analysis of 50 years of changes in freshwater inputs to the Arctic Ocean and North Atlantic reveals that freshwater increases from Arctic Ocean sources are highly linked to a fresher North Atlantic. The study, published in Science, suggests that changes in climate and atmospheric dynamics may be driving this trend.
Scientists found that massive erosion of the Alps was triggered by a sudden drop in Mediterranean Sea levels and prolonged warmer climate. The event, known as the Messinian salinity crisis, carved deep valleys and left behind lakes, reducing the mountain range's size over millions of years.
Researchers studied ancient Arctic water cycles during a period of rapid, extreme global warming 55 million years ago. The study found that increased precipitation led to lower ocean salinity and drastically lower oxygen levels in the Arctic Ocean, similar to predicted effects of greenhouse gases.
The Ocean Tracking Network, a global collaboration of scientists and experts, aims to track the movements of important species using electronic tags. The network will use an extensive international array of acoustic receivers on the ocean floor to collect data on water temperatures, salinity, and light conditions encountered by animals.
Climate scientist Michael Schlesinger warns of catastrophic consequences of inaction on global warming, citing the shutdown of Atlantic thermohaline circulation. The professor's book emphasizes human-induced climate change and its devastating impact on sea levels and coastal cities.
A team of scientists has successfully drilled into a fossil magma chamber beneath the Pacific Ocean's crust, providing valuable insights into how new ocean crust is formed. The discovery confirms theories about the relationship between seismic velocity and crustal rock composition.
Researchers have developed a method to detect super-salty, submerged eddies called Meddies using sensor data from U.S. and European satellites. These warm, deep-water whirlpools play a significant role in carrying salty water from the Mediterranean Sea into the Atlantic, affecting global ocean circulation and climate change.
The HYbrid Coordinate Ocean Model (HYCOM) provides long-range weather prediction, enhances ocean current understanding, and supports real-time maritime operations. This innovative tool enables accurate forecasts and tracking of pollution, algal blooms, and oil spills.
Ocean acidification could lead to extinction of many marine species due to increased acidity and dissolution of calcium carbonate shells. The last time oceans endured such a drastic change in chemistry was 65 million years ago, at the same time dinosaurs went extinct.
Researchers are using electronic tags on marine animals to collect data on oceanographic conditions, such as water temperature and salinity. This data is being used to improve ocean circulation models and gain insights into the lives of California sea lions and other apex predators.
A study by Michael Schlesinger predicts a high likelihood of thermohaline circulation collapse due to global warming. The shutdown would have devastating effects on the climate, including warmer temperatures in the southern hemisphere and colder temperatures in the northern hemisphere.
Researchers sequenced goby DNA to find evidence of invasion; genetic analysis suggests Atlantic gobies invaded during warm period 150,000 years ago. Warmer climate may lead to further expansion of marine species beyond cold water barriers.
Researchers found that Agulhas eddies, which transport seawater from the Indian Ocean to the South Atlantic Ocean, are large warm rings of water with a diameter of about 300 kilometres. These eddies import considerable quantities of heat into the Atlantic Ocean, contributing to climate change and global warming.
The Gaza Strip faces a severe contaminated water crisis, with the only source being unsuitable for drinking due to high levels of salinity and pollution. A proposed management plan aims to provide a win-win situation but requires cooperation between Israel and Palestine.
Researchers at the University of Illinois found that climate change affects the oceans' ability to store carbon dioxide. The best location for injecting CO2 into the deep ocean changes with climate change, with the Atlantic Ocean proving more effective than other locations.
Long-term data shows that road salt is accumulating in ground water and aquifers, causing year-round increases in freshwater salinity. This has detrimental effects on aquatic ecosystems, even in rural areas with low road density.
Historical records show salinity concentrations increasing in groundwater and aquifers due to urbanization and deicer use. High chloride levels can induce mortality in aquatic animals and alter plant composition.
A computerized water monitoring system is deployed on the historic schooner The Pioneer, measuring water temperature, salinity, and dissolved oxygen in New York Harbor. Students can access data from home to learn about forecasting and environmental monitoring.
Researchers discovered a stable state in the ocean-atmosphere system that is dramatically different from today's, contradicting previous studies. This finding suggests the Earth's system functioned differently in the past, and highlights the need for improved climate models to reproduce various climate states.
Researchers estimate that excess fresh water entered the North Atlantic Ocean, causing salinity changes and potentially slowing the ocean conveyor. The study suggests that a freshening threshold could be reached in a century, affecting heat transport and climate.
Carlos Manuel Rodriguez was awarded the first-ever Global Ocean Conservation Award for his groundbreaking work in advancing global marine conservation, fisheries reform, and ocean science. He is recognized for his leadership in securing a U.N. moratorium on high seas bottom trawling and promoting sustainable fishing practices.
A new study links drought in southern Africa to the warming of the Indian Ocean, contradicting earlier research that connected it to the Sahelian region. The analysis suggests a late 20th-century cooling of the North Atlantic Ocean was key to Sahelian drought, with recent warming leading to increased rainfall in the area.
Researchers monitoring two PennDOT-installed data loggers measure high salt levels in runoff wetland, reaching half the salinity of seawater. The effects on species and soil quality are still unknown but may include decreased midge populations and increased algae growth.
Researchers from WHOI studied salt fingers in the tropical Atlantic, injecting a tracer into the ocean and measuring its spread nine months later. The results showed enhanced mixing of salt and heat, with salt fingers playing a crucial role in shaping the ocean's temperature and salinity structure.
Researchers have drilled a historic hole in the Atlantic Ocean floor, collecting over 3,000 feet of core samples that will be analyzed for years to come. The discovery could provide new insights into how the ocean crust was formed and has evolved over time, challenging previous understanding of the Earth's interior.
A study by Oregon State University suggests that ocean currents could disrupt the marine food chain, leading to a decline in phytoplankton productivity. The Atlantic Conveyer current, which warms Europe, is a critical component of this process, and its disruption could have far-reaching consequences for global food security.
A research team has confirmed that ocean circulation in the southern hemisphere adapts to sudden changes in the north, enabling more accurate forecasts of ocean reactions to climate change. The study reveals a mechanism linking the two hemispheres, with waters in the southern hemisphere playing an active role in sudden climate changes.
Phytoplankton amounts have increased globally by over 4% along coastal regions, while declines were observed in mid-ocean gyres. This shift may indicate changes in the biology of oceans, particularly in coast regions, and has implications for ocean ecosystems and climate change.
Researchers found that small sections of the ocean floor may be rotating like imperfectly meshing cogs, contradicting previous expectations. The discovery provides new insights into the evolution of complex plate boundaries and has significant implications for our understanding of plate tectonics.
Scientists have created a mathematical model that accurately describes the evolution and movement of tectonic microplates, which are dynamic whirlpools of ocean floor found at mid-ocean ridges. The model uses a wax tank to simulate the ocean floor, replicating patterns seen in the Earth's crust.
A new NASA tool called Giovanni allows high school and college students to access and analyze satellite-derived ocean color data, providing insights into ocean biology. The tool uses chlorophyll patterns to study phytoplankton growth and its connection to El Nino/La Nina events.
A new study suggests that ocean tides contributed to the enigmatic Heinrich events by breaking gigantic icebergs from the ice sheet covering northern Canada. The research used a state-of-the-art computer model to capture ancient tidal variances with high accuracy, revealing that tides were highest in the Labrador Sea during these events.
The international Argo program has reached a milestone with 1,500 ocean-traveling float instruments now operating, providing valuable data on climate and weather phenomena. This coverage represents half of the target 3,000-float array, enabling scientists to monitor the planet's oceans and gain insights into ocean processes.
The CBLAST-Hurricane project is using new ocean probes to collect data on water conditions before, during, and after hurricanes. This information helps scientists develop better models to predict a hurricane's development, which can inform the size of storm surges that pose a threat to ships in port.
The global survey found that about half of anthropogenic CO2 is taken up by the upper 10% of the ocean. Rising CO2 levels may alter marine food webs and diversity, threatening calcifying organisms.
A Cardiff University-led expedition has traveled aboard the RV Marion Dufresene to collect deep ocean sediment cores and reconstruct past climate changes in the North East Atlantic. The project aims to understand the role of ocean circulation in abrupt climate shifts during the last Ice Age, with a focus on the European Margin.
The US Commission on Ocean Policy released a preliminary report outlining bold and broad-reaching recommendations to reform the nation's ocean policy. The report emphasizes ecosystem-based management, strengthening science and education to inform decision-making, and enhancing regional goals and priorities.
Scientists have quantified the transport of carbon from surface waters to the deep ocean in response to iron fertilization. The study found that while iron fertilization can enhance carbon flux and reduce atmospheric carbon dioxide levels, the quantities removed are no greater than natural plankton blooms, making it a limited solution.
A University of California study suggests that melting Greenland ice could lead to a significant drop in North Atlantic Ocean salinity, triggering colder climates in Northern Europe and Eastern Canada. The research found that elevated Caribbean salinity, transported by the Gulf Stream, amplifies heat transport systems.
The US government is expected to issue a draft report with recommendations for ocean policy, addressing issues like resource stewardship and pollution prevention. The commission's report emphasizes the need for ecosystem-based management to sustain long-term exploitation.
National Ocean Commissioners and scientists propose a holistic ecosystem-based approach to manage the oceans, shifting from single-species management to integrated governance. This approach aims to restore ocean health by considering the interconnectedness of species and ecosystems.
Scientists have developed a real-time operational forecast system using satellite data, providing accurate 3D ocean conditions and helping Coast Guard rescuers determine the direction of stranded individuals. The system uses multiple satellite measurements and sensor data to generate forecasts several days ahead.
A study found that three-quarters of biological activity in oceans relies on a single nutrient-rich water circulation pattern in the Southern Hemisphere. This discovery helps settle a longstanding question about ocean fertility and raises questions about potential impact of climate change.
A new study reports significant changes in ocean salinity levels, with tropical waters becoming saltier and polar regions fresher. These shifts suggest an acceleration of the Earth's water cycle, potentially exacerbating global warming and disrupting ocean circulation.
A recent study reports significant changes in ocean salinity levels, with tropical waters becoming saltier and polar regions fresher. These findings suggest an intensifying global water cycle, which could disrupt ocean circulation patterns and exacerbate global warming.
Researchers at Columbia Climate School have discovered that the majority of water in the Indonesian Throughflow flows below 300m below the surface, making it colder and deeper than thought. This finding has significant implications for understanding heat exchange between oceans and the atmosphere.
Phytoplankton's shift to red pigments occurred due to a global ocean oxygen depletion, which paved the way for their evolution. This discovery reveals how the ocean's chemistry has been dominated by red phytoplankton ever since.
Scientists have developed a new adaptation of seismic reflection profiling to create detailed pictures of oceanic features, including eddies and internal waves. This technique has the potential to improve our understanding of ocean mixing and its role in climate modeling.