Researchers find massive release of CO2 from Southern Ocean occurred when Antarctic sea ice melted, not due to changes in ocean density. The expansion and retreat of sea ice acted as a 'lid' controlling CO2 exchange between ocean and atmosphere.
Pressure-retarded osmosis (PRO) technology is not feasible due to biofouling, which clogs membrane structures and feed channels. Researchers found that organic matter and bacteria in wastewater streams result in extreme biofouling development.
A computer model predicts changes in tidal water level and salinity in Bangladesh's delta region, affecting farmland and the Sundarbans mangrove forests. The model could inform decisions on irrigation and crop management to mitigate potential flooding and ecosystem damage.
A UK-led study found that seal tags can improve ocean forecasts by providing valuable temperature and salinity recordings in regions rarely sampled. This could lead to better weather predictions and improved marine conditions for industries such as shipping and offshore oil and gas operations.
The ocean microbiome is a vast biological network that regulates global systems, including energy consumption and respiration. Microbes are responsible for virtually all photosynthesis in the ocean and cycle essential nutrients and trace elements.
A study found that coccolithophore abundance has increased by an order of magnitude since the 1960s in the North Atlantic, contrary to predictions. This unexpected finding highlights the complex response of marine ecosystems to climate change.
A new study found a link between abrupt ocean warming at the end of the last ice age and low-oxygen conditions that led to vast marine dead zones. Warming surface temperatures triggered loss of oxygen in the North Pacific, raising concern that similar events will occur again as oceans warm.
A new study finds a link between abrupt ocean warming and low-oxygen conditions that led to vast marine dead zones in the North Pacific. The researchers discovered a clear connection between two prehistoric intervals of abrupt ocean warming that ended the last ice age, resulting in an increase in diatom production and subsequent hypoxia.
Researchers found that dissolved organic carbon is efficiently removed from ocean water when heated to mimic hydrothermal vent conditions. This process converts the organic molecules into carbon dioxide, reducing oceanic carbon storage.
A University of British Columbia study found that major swaths of the ocean must be protected to reach global biodiversity targets. Currently, only 16% of protected areas are designated as 'no-take' zones, which are crucial for conserving marine life.
A new method estimates fish movements using ocean heat content images, revealing detailed movements not apparent with surface temperature data. The analysis shows large migratory fishes have affinities for ocean fronts and eddies, similar to hurricanes.
Despite recent advancements, only 3.5% of the ocean has protection, compared to 15% of terrestrial areas, highlighting a need for accelerated action. Seven key findings from researchers suggest that full protection, networks, and smart planning can enhance biodiversity and economic benefits.
A new study has found that changes in the polar regions can significantly affect the ocean and climate on the opposite side of the world, far quicker than previously thought. The research linked ocean currents to climate conditions during the last ice age, revealing a tight connection between the two.
Ocean acidification is affecting global marine ecosystems, with the Arctic and Antarctic oceans being particularly vulnerable. The study reveals that waters with lower aragonite saturation state are more corrosive to shellfish and coral species.
The Ocean Conservancy's report outlines specific land-based solutions for reducing ocean plastic waste, including a four-point plan to cut leakage by 45% in 10 years. The report estimates a total cost of $5 billion and significant returns to the global economy.
A new study from the University of Exeter solves a long-standing climate science mystery by explaining how changes in ocean circulation affect carbon storage. The researchers found that warmer water upwelling in the Southern Ocean helps store more CO2, contributing to glacial cycles.
Research found that changes in ocean circulation due to Antarctica's temperature had a profound impact on the amount of carbon dioxide absorbed from the atmosphere. When temperatures dropped, nutrient-rich waters rose closer to the Antarctic continent, allowing phytoplankton to thrive and absorb more CO2.
Researchers analyzed deep sea coral samples to reveal that past carbon dioxide spikes occurred alongside high ocean circulation events. The findings suggest that excess carbon in the deep ocean was flushed out, releasing CO2 into the atmosphere.
A new study explores the potential of Pressure Retarded Osmosis technology to extract energy from salinity gradients in Australian waters. The research suggests that brine, rejected during desalination, can be used as a source of osmotic energy, offering a carbon emission-free alternative to fossil fuels.
New studies reveal that the Southern Ocean has increasingly removed more carbon dioxide from the atmosphere since 2002. The research, compiled from millions of ship-based observations, suggests that the Southern Ocean's carbon sink is strengthening, contrary to previous findings.
The Southern Ocean's carbon sink has renewed its strength, absorbing more atmospheric carbon dioxide over the past decade. This improvement is attributed to changes in sea surface temperature and dissolved inorganic carbon levels.
A new MIT study finds that large seasonal changes in desert dust can dramatically affect surface phytoplankton, which rely on iron as a main nutrient for growth. The team determined that iron has a very short residence time in ocean waters, lasting only six months before sinking into the deep ocean.
Researchers found that sediment-entombed marine archaea's growth varies based on changes in ocean oxygen levels, affecting the accuracy of past ocean temperatures. This discovery highlights the need to consider oxygen levels when interpreting the TEX-86 index, a popular method for measuring ancient ocean temperatures.
Research finds that a conch population outbreak and high water salinity are causing a sharp decrease in oyster populations on Florida reefs. The study suggests that restoring the habitat may fail if an area contains or is likely to develop an outbreak of conchs like the one in Matanzas.
A study by University College London found that warm, stagnant water from the deep Arctic Ocean and Nordic Seas contributed to the end of the last Ice Age. The researchers used proxy data to reconstruct past ocean circulation changes, which showed a warmer deep Arctic Mediterranean during glacial times.
The Ocean Health Initiative aims to protect and restore coastal and marine habitats, supporting the conservation of threatened marine and coastal species. The program, funded by a $1.5 million pledge from SeaWorld Entertainment, will focus on key estuaries along the Eastern Atlantic and Gulf of Mexico.
A study found that simulated seawater flooding significantly reduced growth of sensitive vegetable seedlings. Salt-tolerant varieties like spinach, eggplant, and tomato showed less damage, with some experiencing a 43-67% reduction in photosynthetic rate after two weeks.
The University of Montana's Sunburst Sensors won a $1.5 million XPRIZE for developing an affordable and accurate pH sensor to measure ocean chemistry, recognizing efforts to combat ocean acidification. The company, founded by UM professor Mike DeGrandpre, employed 9 people at the time of the win.
Phytoplankton, the base of marine food chains, may experience significant changes due to ocean acidification, with some species dying out while others thrive. The study found that increased acidity could lead to altered competition among species, affecting entire ecosystems and potentially impacting predators like polar bears.
Ocean organisms produce aerosols that nearly double cloud droplet numbers in summer, boosting sunlight reflection. The study estimates the equivalent solar energy impact over the whole Southern Ocean.
A new study suggests that retreating sea ice in the Iceland and Greenland Seas may be changing the Atlantic Ocean's circulation patterns. This shift could lead to a cooling of western Europe as the Gulf Stream weakens, resulting from reduced oceanic convection.
Scientists developed a computer model that studies ocean mixing in vast eddies, clarifying the complex processes driving ocean storms. The model enables researchers to study heat and carbon fluxes into the deep ocean, increasing global climate simulation accuracy.
The Mid-Atlantic Ocean Data Portal has launched new features to expand pathways for participation and collaboration. The platform now includes Ocean Stories, Map Groups, and enhanced organization tools, empowering stakeholders to share their perspectives and work together on ocean planning challenges.
The Aquarius instrument successfully completed its primary three-year mission in November 2014, achieving its science objectives and providing valuable data on ocean dynamics and climate models. The loss of onboard power regulation and spacecraft attitude stabilization led to the end of operations.
A new study has found that coral reefs in Palau are showing few of the predicted responses to low pH caused by ocean acidification. Instead, these reefs exhibit increased bio-erosion, but also host more species and have greater coral cover than in other naturally low pH reef systems.
A new study found that coral reefs in Palau's naturally acidic waters are thriving, despite the expected negative impacts of ocean acidification. However, increased bioerosion was observed, threatening the long-term survival of these ecosystems. The research team hopes to better understand how corals adapt to low pH conditions.
A NASA spacecraft will use radar equipment developed in Antarctica to scan Europa for potential water plumes and habitable conditions, driven by evidence of an ocean beneath the thick ice cover.
Researchers have found a novel way to 'read the Earth's LIPS', revealing a previously missed connection between Large Igneous Provinces and mid-ocean ridges. This discovery changes our understanding of massive volcanism in ocean basins, suggesting that undersea eruptions are less catastrophic than thought.
Research shows that estuaries offer a parasite-free zone for Dungeness crabs, allowing them to rid themselves of deadly nemertean worms. The crabs thrive in lower-salinity environments, making estuaries an essential habitat for their survival.
Researchers found that coral adaptation to high salinity levels in the southern Persian/Arabian Gulf may prevent them from escaping their fate through global warming. Corals lose their exceptional heat stress tolerance when adapting to normal salinity levels.
A 55-million-year-old global warming event triggered a highly corrosive deep-water current in the North Atlantic Ocean. Researchers recreated the ocean basins and land masses of that time using a global climate model to understand how this event occurred.
Researchers discovered that a 55 million-year-old ocean current, formed by the North Atlantic's shape and changes in ocean currents, caused more severe acidification than other oceans during the Paleocene Eocene Thermal Maximum. This event may have implications for today's climate sensitivity to increasing carbon dioxide.
A new study led by University of Southampton researchers suggests that ocean acidification may not have caused the mass extinction of ammonites and other planktonic calcifiers. The research found that the asteroid impact was the primary cause of the extinctions, but not due to ocean acidification levels being too weak.
A new computer model developed by NOAA and research institutions will help inform scallop management decisions. The integrated assessment model evaluates the impacts of ocean acidification on Atlantic sea scallops, predicting potential declines in harvest levels and landings over the next several decades.
Researchers found that ocean currents strongly affect methane-consuming bacterial populations in Arctic cold seeps, controlling their prevalence and methane consumption rates. Fluctuations in these communities were linked to changes in water temperature and salinity.
A recent study published in the Proceedings of the National Academy of Sciences found that ocean fronts increase total ecosystem biomass and fisheries production. By incorporating front dynamics into current climate models, researchers found that these regions can aggregate food and resources, leading to higher productivity in the ocean.
Researchers at Woods Hole Oceanographic Institution discovered that stressed and dying phytoplankton release chemicals that stimulate marine bacteria to quickly convert organic carbon back into CO2. This process reduces the amount of sinking detritus, releasing more CO2 into the shallow ocean and atmosphere.
A study published in Nature Geoscience found that ocean currents can significantly impact the removal of methane from seawater. The researchers discovered that fluctuations in current strength and variability control the prevalence of methanotrophic bacteria, leading to reduced methane consumption.
A study published in Science reveals that swirling ocean currents, known as eddies, play a significant role in delivering carbon from phytoplankton blooms to the deep ocean. The research, led by Melissa Omand, found that these currents transport small, non-sinking phytoplankton cells to depths of up to 1,000 meters.
Researchers found a 24 percent decline in calcium carbonate production in large areas of the Southern Ocean over the past 17 years. This decline is linked to ocean acidification caused by climate change, which reduces calcification rates of coccolithophores.
The study found that the Atlantic Ocean's overturning has been weakening since 1970, mainly caused by freshwater from melting Greenland ice sheets. This could lead to major negative effects on ocean ecosystems, fisheries, and regional sea-level rise.
Researchers from the Malaspina Expedition found that dissolved organic carbon (DOC) in the deep ocean is not degraded by bacteria due to low concentrations of degradable compounds. The study provides new insights into the regulation of the carbon cycle and global climate.
A new study suggests that ocean pipes would increase global warming due to decreased cloud cover and increased sea-ice melting, rather than cooling the Earth as predicted.
Researchers develop 'dynamic ocean management' to integrate real-time data and crowd-sourced reports into ocean industry applications. This approach aims to protect vulnerable ecosystems while promoting sustainable resource use, in line with industries' profitability.
A study by Alfred Wegener Institute finds that ocean acidification negatively impacts diatom growth in the Southern Ocean, particularly under changing light conditions. Diatoms' biomass production could be drastically reduced in future scenarios with more acidic water.
Scientists from GEOMAR Helmholtz Centre for Ocean Research Kiel reconstructed pH values of northern Pacific ocean over past 120 years with monthly resolution. The study found that the pH value has been declining since late 19th century, coinciding with rising carbon dioxide levels in atmosphere.
A $2.5 million NSF grant will support the five-year Agulhas System Climate Array project, which aims to monitor changes in the ocean's circulation due to climate change. The research will focus on the physical characteristics of the Agulhas Current and its role in global climate variability.
New techniques using satellite-mounted cameras and microwave sensors can monitor large areas of the ocean, quickly identifying regions most at risk from increasing acidification. This approach offers remote monitoring and could lead to further development of satellite sensors in the coming years.
A recent study published in Science estimates that between 4.8 and 12.7 million metric tons of plastic enter the ocean every year, mainly from coastal regions. The researchers used a grand model to estimate the amount of plastic waste entering the ocean and found that it is significantly higher than previously estimated.
A study published in Nature shows that a release of carbon dioxide from the deep Southern Ocean helped bring an end to the last Ice Age. The finding provides insight into how oceanic carbon storage affects climate change.