Researchers studying ocean temperatures in West Antarctica found a complex cycle of warming and cooling that affects ice shelf melting rates. The findings suggest that changes in deep ocean temperatures can lead to significant variations in ice sheet melting, with potential implications for global sea-level rise.
A study suggests that increased Southern Ocean upwelling may be responsible for the Holocene's 20 ppm rise in atmospheric carbon dioxide, which stabilized the climate and facilitated human civilization. This process weakened the biological pump, allowing more carbon dioxide to leak into the atmosphere.
Researchers analyzed ocean sediments to understand Atlantic Ocean circulation changes, finding two episodes of ice melting linked to slow-downs in ocean circulation. The findings have implications for future long-term changes in Earth systems with global climate change.
A new study of lake sediments reveals that increased westerly winds are likely to reduce the Southern Ocean's ability to absorb carbon dioxide from the atmosphere. This could accelerate climate change as the Southern Ocean currently absorbs over 40% of human-produced carbon dioxide.
A new study by Florida State University researchers has found that tiny phaeodarian organisms in the ocean's twilight zone are consuming up to 20% of sinking, carbon-rich particles before they reach the deep ocean. This discovery suggests a significant impact on Earth's carbon cycle and challenges current climate dynamics.
De Gruyter integrates Code Ocean's computational reproducibility platform across its journals, enabling authors to share working code and readers to reproduce results. This partnership advances transparency and decision-making in academia and industries.
Researchers reexamined ocean circulations and river carbon transport, finding the Southern Ocean is a smaller carbon sink than thought. Land in the northern hemisphere absorbs less carbon, but rivers send it to the ocean with increased strength, challenging current estimates.
Researchers at the University of East Anglia used satellite-tagged seals to collect data on water temperature and salinity in West Antarctica. The study found that warm, salty deep water is more common during winter months, suggesting increased ice sheet melting.
Researchers at RIKEN have discovered a hormone-like peptide in plants that increases their resistance to excessive salt. The peptide, AT13, enhances salinity stress tolerance and can be applied as a natural supplement for crops growing in high-salt conditions.
Researchers found that the Baltic Sea is experiencing extreme changes, such as warming and oxygen-free zones, which can be used to predict future global ocean changes. The region's unique characteristics make it an ideal model for studying coastal ocean management and sustainable development.
Researchers at HKU and Chinese Research Academy of Environmental Sciences have developed a novel scientific method to derive water quality criteria (WQC) of metals for protecting different marine ecosystems. The new approach considers variable temperature and salinity regimes, improving protection for tropical marine organisms.
A team of researchers discovered that deep ocean aquifers can break down more refractory carbon than previously thought. Microbes in the aquifer consume carbon, changing the composition of the surrounding seawater. This finding has the potential to reshape our understanding of carbon cycling in the deep ocean.
Researchers found a direct link between ocean warming and trends in continental humidity and temperature. Analysis of data from 1979-2016 revealed land temperatures increasing faster than ocean temperatures, but specific humidity over oceans increased faster than over land.
A study by the Cary Institute of Ecosystem Studies found that distance to roads and amount of nearby pavement significantly influence well water salinity. Hotspots with high salinization were identified, particularly near sharp turns, steep grades, and narrow streets.
Researchers studying the Black Sea's oxygen-deprived waters found that chemical and biological processes similar to those in the deep ocean occur. This provides new insights into the ocean's role as a storage reservoir for carbon, helping to dampen the effects of human-driven climate change.
Researchers at Bigelow Laboratory for Ocean Sciences have developed a statistical method to quantify important ocean measurements from satellite data. This breakthrough enables scientists to calculate concentrations of key particles in the water column, providing insights into ocean dynamics and biogeochemistry.
A study found that 90% of coastal freshwater turtle species will be affected by sea level rise by 2100, with some species losing up to 30% of their range. Researchers warn that turtles may not be able to adapt quickly enough to changing environments, threatening their survival.
A recent study at Lake Abert found that low water levels and high salinity affect the availability of brine shrimp, a key food source for waterbirds. The lake's surface area has decreased by nearly 200 football fields since 1986, resulting in a 82% decline in bird sightings during periods of low water and high salinity.
A new study published in Nature Ecology and Evolution suggests that herring larvae may survive better in a future acidified ocean due to an altered food supply. This unexpected result could have implications for the long-term survival of fish populations.
Scientists found a correlation between sea surface temperatures in the Irminger Sea, surface freshwater, and atmospheric conditions in the Labrador Sea. The study suggests that freshwater can weaken deep convection, leading to delayed onset of winter convection and potentially weakening ocean circulation.
Ocean microbes produce at least fifty percent of the oxygen in our atmosphere while removing large amounts of carbon dioxide. The new LRAUVs can transit for over 600 miles and use their own 'eyes and ears' to detect important oceanographic events like phytoplankton blooms.
Researchers at KAUST found that high salinity can protect corals from heat stress by increasing the levels of antioxidant floridoside. This compound helps regulate osmotic pressure and prevent severe bleaching in coral model organism Aiptasia.
Brown University researchers discovered that mesoscale eddies in the global ocean tend to merge into larger ones, unlike smaller eddies which break up into smaller scales. This finding could help develop coarser-grained ocean simulations that better capture ocean dynamics.
A recent study by Syracuse University researchers examines the impact of de-icing salts on the Tioughnioga River watershed. The team found that surface-water chloride concentrations are expected to decrease in 20-30 years due to changes in climate and snowfall patterns.
Roots face challenges in saline soils, but plant cells can sense damage and respond with strength-enhancing chemicals to prevent explosion.
Research by University of Delaware oceanographer Wei-Jun Cai and colleagues reveals that coastal water is taking up a larger portion of atmospheric carbon dioxide. The study's findings, published in Nature Communications, may have important implications for understanding the global carbon budget and predicting greenhouse gas emissions.
A study published in Nature Communications finds a correlation between Atlantic Ocean surface currents and rainfall patterns in the Western Hemisphere, both in the past and present. The research suggests that changes in ocean currents can influence global climate and may have far-reaching impacts on future climate change.
According to an updated analysis from the Institute of Atmospheric Physics/Chinese Academy of Sciences, 2017 was the warmest year on record for the global ocean. The oceans accumulated 1.51 × 10^22 J of heat, surpassing the previous second-warmest year of 2015.
Researchers found that ancient methane from ocean sediments is being released into the ocean, but only a small amount survives to be emitted to the atmosphere. The study suggests that catastrophic emission of methane from degrading hydrates may not be an inherent outcome of climate change.
A new international study found that plankton's body size and ocean currents are crucial in determining their dispersal in the ocean. The larger the plankton, the smaller the connection between distant communities. Climate change is rapidly warming marine waters, making it essential to understand how this affects biological communities.
A new study finds that 37% of US drainage areas experienced significant increases in salinity and alkalization, with consequences for pipe stability and drinking water quality. Strategies like pre-wetting salt and monitoring aging pipes are recommended to mitigate effects on public health.
The ocean is losing its breath, with low-oxygen sites increasing fourfold in the open ocean and tenfold in coastal waters since 1950. Climate change and nutrient pollution are driving this decline, which can stunt growth, hinder reproduction, and lead to disease or death.
Scientists warn that the world needs to address climate change and nutrient pollution to halt the decline of ocean oxygen. Low oxygen levels can stunt growth, hinder reproduction, and lead to disease or death in animals, while also triggering toxic chemical releases.
Researchers have developed a new method to measure the average temperature of the global ocean using noble gases in the atmosphere. By analyzing air bubbles trapped in ice cores, scientists can calculate the average global ocean temperature with high precision, providing insights into past climate cycles and modern ocean changes.
Ocean researchers discovered 'smoke rings' that can transport small marine life at high speeds across vast distances. These linked eddies are ten times faster than regular ocean currents and were found in the Tasman Sea and South Atlantic.
A new tool advances understanding of ocean chemistry and suggests that microbial metabolisms shape the ocean's balance. The model simulates impact on North Atlantic chemistry and predicts genes and transcription throughout the ocean.
Researchers have discovered that a high concentration of coccolithophores and diatoms thrive in the Great Calcite Belt, driven by nutrient levels, sea surface temperature, and carbon dioxide concentration. The bloom plays a crucial role in global carbon cycle models and highlights the complexity of phytoplankton ecology.
Researchers from Bigelow Laboratory discovered nitrite-oxidizing bacteria to be key players in the global carbon cycle, capturing more than 1.1 gigatons of CO2 annually. These large, relatively rare bacteria outperform archaea in carbon capture, highlighting a significant shift in our understanding of oceanic carbon cycling.
A new instrument called CaPASOS will be used to measure CO2 levels in the air and surface of the ocean in remote regions. This will provide valuable data on carbon dioxide uptake by the ocean and its impact on climate change.
Scientists from Cardiff University analyzed sediment samples from the North Atlantic Ocean, finding changes in ocean circulation that impacted heat transport to Europe. They linked these changes to historical records of colder and warmer climates, shedding light on past climate variations.
Researchers have discovered a 'shadow zone' around 2km below the sea surface where ancient water has remained isolated for centuries. This region's unique shape and geothermal heat sources trap ocean water, suspended in an area with minimal vertical movement.
The Scripps Institution of Oceanography will develop an advanced ocean and atmosphere simulator to replicate complex ocean conditions and generate gale-force winds in a controlled setting. The simulator will help researchers understand how pollutants and climate change affect marine animals, plants, cloud formation, and the planet.
Researchers have discovered a novel way to detoxify salty wastewater using bacteria that can generate electricity, producing hydrogen gas. The bacteria, found in deep-water brine pools, thrive in extreme conditions and have the potential to convert waste products into valuable chemical products.
A recent expedition to the Flower Garden Banks National Marine Sanctuary revealed a 10% drop in salinity levels due to Hurricane Harvey's floodwater plume. The team hopes to track the plume as it migrates through the Gulf, aiming to understand its impact on the reefs' health.
Researchers suggest open-ocean wind farms can sustain higher electricity generation rates than on-land wind farms due to kinetic energy reservoir access. Annual global energy demand could be met with commercial-scale open-ocean wind turbines spanning approximately 3 million square kilometers.
The Newport Line, a decades-long ocean monitoring program off the Pacific Northwest coast, has been recognized for its significant contributions to marine science. The PICES Ocean Monitoring Service Award acknowledges the program's value in understanding climate patterns, salmon returns, and ocean currents.
Tiny plant cells in coral tissue produce osmolytes to regulate pressure, helping corals survive in salty waters. This finding has important implications for managing coral reefs under climate change.
Scientists developed a method to quantify past oxygen depletion in oceans using thallium isotope composition of ancient seafloor sediments. The analysis suggests up to half of the deep ocean was oxygen-depleted during Oceanic Anoxic Event 2, with modern trends showing similar rates of deoxygenation.
International research team discovers extremely low-oxygen regions in Atlantic Ocean, producing high levels of nitrous oxide. The phenomenon was previously unknown and had escaped research due to the small size and mobility of these eddies.
A study analyzing five years of Ocean Health Index data for 220 countries found that global ocean health has remained stable, but individual countries have seen changes, particularly in the Arctic and sub-Arctic regions. Improvements in fishery management and marine protected areas may have stabilized ocean health scores in other regions.
A new study analyzing multiple ocean datasets reveals that the oceans are robustly warming, regardless of data used. The heat redistribution among global oceans experienced a significant shift over several decades.
A new study links declining steelhead trout populations to poor survival rates of juvenile fish in the ocean. Ocean survival rates have declined by 77% in some areas, contributing to low adult abundance and impacting conservation efforts.
Researchers propose a new theory on how waves mix and stir the ocean, bringing cold water to the surface. The study explains how internal waves direct themselves based on topography, shedding light on climate-dependent ocean circulation patterns.
A new study reveals that multiple ocean surface temperature changes are the primary driver of multi-decadal global warming accelerations and slowdowns. This finding supports a more accurate estimate of future global warming rates to meet the Paris Conference's 1.5°C target.
A healthy ocean can contribute to achieving Sustainable Development Goal 14: Life Below Water, alleviating poverty, providing livelihoods, and improving global health. The report highlights the critical need for ocean sustainability to address climate change, social inequity, and other challenges.
The 2015-2016 El Niño event was characterized by warmer ocean temperatures in the Pacific, with blue regions representing colder and red regions warmer temperatures. The El Niño-inducing westerlies caused eastward currents to occur in pulses.
Marine microorganisms rely on iron to recycle dead matter and release nutrients such as phosphorus. This process is crucial in the tropical North Atlantic, where nitrogen limitation may be replaced by phosphorus limitation, influenced by human activities.
Researchers discover that cultured picocyanobacteria, such as Synechococcus and Prochlorococcus, release fluorescent components that closely match the typical signals found in oceanic environments. This finding sheds light on the origin of colored dissolved organic matter in the deep ocean.
A recent study reveals that cold-water corals can thrive in warmer temperatures, but are harmed by ocean acidification. The research, conducted at GEOMAR Helmholtz Centre for Ocean Research Kiel, found that elevated temperatures can compensate for the negative effects of acidification on coral growth and fitness.
The eastern Arctic Ocean is exhibiting vertical mixing similar to the Atlantic Ocean, leading to record-breaking losses of sea ice in summers. The changes have substantial impacts on the Arctic Ocean system, including enhanced atmosphere-ocean interactions and altered freshwater storage patterns.