Direct ocean carbon capture (DOC) technology uses membrane contactors to remove CO2 from seawater, offering a cost-effective alternative to land-based solutions. The University of Pittsburgh team has developed innovative DOC methods using hollow fiber and encapsulated solvents, demonstrating their potential to significantly lower costs.
Scientists developed a new diagnostic framework to analyze oceanic mesoscale eddy transport in the Southern Ocean. The study introduces a holistic picture of eddy potential vorticity transport dynamics, providing theoretical support for potential parameterization.
A recent study found significant changes in ocean color over the past two decades, affecting 56% of the world's oceans. The shift in color indicates changes in marine ecosystems, with tropical regions becoming greener due to human-induced climate change.
Researchers argue that equitable governance and science are crucial for ocean sustainability, prioritizing tropical voices and expertise. The study proposes four key actions: equity in ocean science and governance, reconnecting people and the ocean, redefining ocean literacy, and decolonizing ocean science.
A new study published in Global Change Biology suggests that large-scale ocean iron fertilization could exacerbate climate change-driven nutrient shortages and productivity losses in the tropics, potentially harming coastal fisheries. The research also showed a five percent decline in fish and marine species biomass in tropical areas d...
A pioneering study using deep-sea corals reveals that ocean currents did not fuel the increase in atmospheric carbon dioxide over the past 11,000 years. The research suggests that biogeochemical cycles redistributing nutrients and carbon in the ocean and on land may have influenced this rise.
The InVADER Mission successfully deployed a high-tech laser laboratory on the ocean floor, marking a paradigm shift in ocean research and exploration. The Laser Divebot collects compositional data without disturbing the environment, removing the need for physical samples.
A review of research on Arctic-subarctic ocean linkages suggests stronger heat convergence and increased freshwater input due to climate change. This can impact marine life and the evolution of the climate, with implications for policy-making and mitigation strategies.
Researchers from FSU analyzed the California Current Ecosystem's carbon sequestration, discovering that sinking particles are the primary process transporting organic carbon to the deep ocean. They also found that ocean currents and zooplankton contribute significantly to this process.
A study found that certain pteropod species in the Southern Ocean are vulnerable to climate change due to varying life cycles. The research suggests that population stability is essential for species survival and that prolonged exposure to unfavorable conditions may jeopardize future populations.
Recent research reveals significant increases in tropical cyclone frequency in the North Atlantic and North Indian Ocean, while decreases are observed in the western Pacific. The study also shows varying trends in intensity across different ocean basins.
New research reveals that atmospheric dust supports 4.5% of global annual carbon export production through phytoplankton growth, with regional variation up to 20-40%. This pathway helps regulate atmospheric carbon dioxide levels and mitigate climate change.
A team of scientists has developed an AI model that can accurately predict ocean wave sizes, reducing the need for expensive and time-consuming numerical methods. The ConvLSTM model outperforms existing methods in terms of accuracy and efficiency, paving the way for real-time ocean forecasting.
A recent study reveals that uneven future warming in the Indian Ocean can cause shifts in monsoon precipitation, with potential impacts on societies and ecosystems. The research identifies key mechanisms driving these changes, including winds and ocean currents.
The High Seas Treaty aims to establish cooperative approaches to improve ocean management, but scientists argue that more research is needed to effectively implement the agreement. The treaty proposes massive marine protected areas covering 30% of the ocean by 2030, which could significantly improve ocean conservation.
An international research team has developed a framework to evaluate government preparedness for ocean acidification, a pressing threat to marine ecosystems. The framework identifies six aspects of effective policy and specific indicators, enabling policymakers to assess their own preparedness and identify areas for improvement.
Researchers examine phytoplankton blooms induced by tropical cyclones to predict climate change impacts. The study found a massive bloom in the wake of Cyclone Oma, which occurred once every 1500 years, and may indicate changes in ocean temperatures.
Researchers found giant underwater waves play a crucial role in ocean's ability to store heat and carbon, challenging current climate models. The study highlights the importance of small-scale turbulence in ocean circulation, which can significantly impact global climate projections.
A new study published in PNAS reveals that the dissolution of bubbles in high-latitude oceans is a dominant pathway for gases like oxygen and nitrogen to enter the deep ocean. This improved understanding can help improve the accuracy of climate models, which are crucial for predicting changes in the ocean's carbon dioxide inventory.
Researchers from Florida State University used high-performance computing to simulate the Earth's early history, finding that an ancient magma ocean solidified in under 2 million years. This discovery helps explain chemical diversity in the lower mantle and layering within the Earth.
A new study finds that coccolithophores, a common group of marine phytoplankton, dominate the production of calcium carbonate in the surface ocean. This process controls atmospheric CO2 levels and is crucial for understanding climate change and ocean acidification.
Research reveals hydrothermal vents as a previously undiscovered source of dissolved black carbon in the oceans, transporting it thousands of kilometers away. This discovery sheds light on the ocean's role as a carbon sink and provides insights into the formation of recalcitrant dissolved organic carbon.
Numerical simulations suggest that Mimas' Herschel impact basin is compatible with a thinning ice shell and geologically young ocean. The results imply that the present-day ocean within Mimas must have been warming and expanding since its formation, potentially making it an emerging ocean world.
Scientists have recorded another year of record-breaking ocean temperatures, indicating a perpetually heating climate. The added heat content has serious consequences, including ocean deoxygenation, altering the exchange of heat, carbon, and oxygen between the ocean and atmosphere.
A new study reveals that changing ocean circulation strengthens precipitation patterns in the Indian Ocean, leading to more intense flood events and droughts. The research suggests a mutual amplification of these effects due to global warming and weakened ocean circulation.
A study by Brown researchers reveals how climate change can impact the Indian Ocean dipole, leading to extreme weather events like megadroughts in East Africa and flooding in Indonesia. The analysis compares long-term climate data with simulations from an advanced climate model.
New study reveals marine algae adapt to nutrient-poor ocean conditions, sustaining productivity even in depleted waters. This 'metabolic hack' could impact global ocean productivity and carbon sequestration.
A study found that ocean warming and acidification decrease the nutritional quality of coccolithophores, a crucial food source for zooplankton species. The study's experiment showed an increase in lipid availability under ocean warming but reduced nutritional content under acidification.
A team of scientists found that the largest open ocean dead zone in the eastern Pacific Ocean emerged eight million years ago due to increasing nutrient content. This natural phenomenon was caused by changes in weathering and erosion on land, leading to a major transition in terrestrial ecosystems.
The Southern Ocean's ecosystem is facing major stressors from climate change, including melting sea ice and ocean acidification. Overfishing of species such as toothfish and krill is predicted to exacerbate environmental impacts on the entire ecosystem.
The Arctic Ocean's pH is decreasing at a rate 3–4 times faster than in other oceans, with acidification impacting marine life. Sea butterflies, a key food source for whales, may face reduced availability due to increased carbon dioxide uptake.
A study published in Nature suggests that ocean heating in the western tropical Pacific will make the East Asian monsoon season wetter. The researchers found a correlation between increases in monsoonal rain in eastern China and the heat content of the Indo-Pacific Warm Pool over the past 360,000 years.
A comprehensive review of ocean warming reveals that global ocean heat content has increased by over 90% since the 1950s. The study predicts that if greenhouse gas emissions are not reduced, ocean warming will continue to accelerate, leading to more intense storms, droughts, and sea-level rise.
FathomNet aggregates images from multiple sources to create a publicly available, expertly curated underwater image training database. The database uses artificial intelligence and machine learning to alleviate the bottleneck for analyzing underwater imagery, accelerating important research around ocean health.
A new study shows that the Galépagos Islands' cool waters are due to a strengthening cold ocean current. The current, which has been getting stronger since the early 1990s, provides a buffer against warming Pacific Ocean waters.
A new study reveals a strong correlation between accelerating Arctic ice melt and ocean acidification, posing a dual threat to climate and marine life. The increased acidity levels in the western Arctic Ocean could lead to devastating consequences for plants, shellfish, coral reefs, and other organisms.
A new study reveals the western Arctic Ocean's ocean acidification is happening at a rate three to four times higher than other oceans due to sea ice loss. The researchers found a correlation between the decrease in sea ice and increased acidification, suggesting this process could intensify over the next few decades.
A new field study reveals a previously unobserved fluid dynamic process that affects the ocean's deep-sea mining operations. Researchers equipped a pre-prototype collector vehicle with instruments to monitor its sediment plume disturbances, finding that the plumes remained relatively low and spread under their own weight.
The Southern Ocean dominates ocean heat uptake due to its unique wind-driven circulation. Rising temperatures could lead to devastating impacts on the food web and ice shelves around Antarctica, with urgent calls for reduced greenhouse gas emissions.
Researchers found that open ocean oxygen-deficient zones shrank during past warm periods due to reduced denitrification rates and changes in tropical Pacific Ocean oxygen content. This suggests a possible link between climate change and ocean oxygen levels.
Researchers studied heat movement near North Pole and under Arctic sea ice, providing insights into the mechanisms of Arctic sea ice decline. Their findings suggest that strong winds cause mixing of water where ice and ocean meet, leading to enhanced heat transfer and changes in seawater salinity.
Researchers confirm significant increase in freshwater entering the Arctic Ocean via the Bering Strait, leading to a decrease in saltiness and potential impacts on sea ice formation and regional ecosystems. This change could also affect climate-sensitive processes, such as deep water mixing in the North Atlantic.
A new study by researchers at University of California - Riverside found that the position of continents can have a devastating effect on deep ocean creatures. Continental movement can cause a sudden collapse in global water circulation, leading to a stark separation between oxygen levels in the upper and lower depths.
Marine heatwaves and ocean acidity extremes often co-occur in subtropical oceans, exacerbating negative impacts. Climate change projections indicate a strong increase in compound events, posing severe threats to marine ecosystems.
A new study by the University of British Columbia suggests that BC's ocean contributed around $4.9 billion to provincial GDP in 2015, with marine transport sector making the highest contribution. However, this estimate is likely an underestimate due to excluded ecosystem services and cultural value.
A new analysis reveals that marine RNA viruses predominantly infect protist and fungal hosts, including plankton, and sort into four distinct ecological zones. The study found that RNA viruses have a large influence on the ocean ecosystem, affecting processes like photosynthesis and ocean carbon flux.
Climate scientists argue that climate actions need to be established at multiple time scales, with a focus on slow emerging changes such as deep ocean warming and sea-level rise. This requires the development of a system of scientific ocean monitoring with a time-scale in mind, considering risks like abrupt slowdowns of ocean circulation.
Researchers discovered over 1,200 RNA viruses linked to carbon absorption on the ocean floor. The study suggests engineered viruses could be used as 'knobs' to control carbon storage, potentially slowing climate change.
The International Bathymetric Chart of the Southern Ocean v2 provides the most detailed seafloor map of the region, with new data covering twice the area of its predecessor. This chart will help scientists better understand ocean currents and climate change.
Diatoms, responsible for 40% of ocean plant biomass production, are declining due to ocean acidification. This decline can lead to nutrient scarcity in surface waters and disrupt marine food webs. Global simulations predict a loss of up to 27% silica in surface waters by 2200.
A new study identifies food and oxygen supply as crucial environmental factors influencing the vitality of cold-water corals in the North Atlantic Ocean and Mediterranean Sea. The analysis of ancient sediments reveals that changes in food supply, rather than ocean temperature, are likely to determine the future health of these ecosystems.
Researchers at MBARI use eDNA and autonomous underwater robots to survey marine biodiversity, providing clues about changes in sensitive areas and the presence of rare species. The technology enables persistent monitoring of ocean ecosystems, supporting food webs and regulating climate.
New research suggests that 62% of warming in the subtropical North Atlantic is stored in the deep ocean below 700m. The study estimates a further 0.2°C warming in the next 50 years due to climate change.
The world's ocean is losing its year-to-year memory due to global warming, making it harder to predict ocean conditions. This decline in ocean memory will have significant impacts on fisheries management, population estimates, and land-based weather forecasts.
A recent study found that microplastics in the ocean can carry land-based parasites, such as Toxoplasma gondii, Cryptosporidium, and Giardia, which can infect humans and animals. The researchers used laboratory experiments to test whether these pathogens could associate with plastics in seawater.
Research reveals that tropospheric ozone contributes more to the Southern Ocean's warming than previously thought. This finding highlights the importance of reducing air pollution to mitigate ocean heat uptake and climate change.
A Scripps Oceanography-led study predicts that climate change is making surface ocean currents faster and thinner, affecting global nutrient transport and carbon removal. This change can have a ripple effect on the ocean's ability to remove heat from the atmosphere.
Researchers developed global forecasts that can provide up to a year's notice of marine heatwaves, which can dramatically affect ocean ecosystems. The forecasts help fishing fleets, ocean managers, and coastal communities anticipate the effects of marine heatwaves, reducing ecological and economic impacts.
A recent study led by the University of Bonn found no evidence of iron fertilization stimulating algae growth and sequestering CO2 in the Antarctic Ocean during ice ages. Instead, other processes such as sea ice cover and ocean stratification prevented CO2 from escaping into the atmosphere.
Research by University of Washington reveals that ice shards in Southern Ocean clouds increase the amount of sunlight absorbed by the ocean's surface. The study found a significant impact on temperature, with differences of 10 Watts per square meter between models including and excluding ice formation.