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.
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.
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.
Recent studies show that CMIP6 models better simulate the spatial distribution of sea surface salinity and freshwater flux variability associated with ENSO. However, some models still have large uncertainties in simulating interannual variations, requiring further improvement in related physical processes.
Floating microplastics from European rivers are found to accumulate in parts of the Arctic Ocean, Nordic Seas, and Baffin Bay. The study's model predicts that these particles have been circulating throughout the Arctic for at least ten years, highlighting concerns for Arctic ecosystems' health.
A new study by Bigelow Laboratory for Ocean Sciences reveals that microbial life in the ocean is adapting to warmer conditions, maintaining vital processes despite climate change. The research found that carbon export was maintained as phytoplankton populations declined due to other small organisms taking up the slack.
Researchers assess predictive skills of ocean heat content in two state-of-the-art seasonal forecasting systems, finding potential to predict sub-surface warming up to two seasons in advance. This could aid mitigation of extreme events and provide early warnings for industries such as aquaculture and fishing.
A global study reveals that freshwater lake ecosystems are being damaged by salt concentrations below government-protective thresholds. The loss of zooplankton triggers a cascade effect causing an increase in algae, potentially altering nutrient cycling and water quality.
Researchers from Texas A&M University have discovered past methane release in the Southern Ocean during a peak glaciation 23 million years ago. This finding suggests that ancient methane gas hydrates could contribute to ocean acidification and low oxygen levels, similar to recent environmental issues in the Gulf of Mexico.
The probe measures salinity, temperature and pressure, making three measurements per metre before returning to the surface. The successful deployment provides valuable insights into freshwater input to the marine Arctic ecosystems and its effects on global ocean currents.
A study led by Monterey Bay Aquarium reveals more than half of the ocean surface has experienced extreme heat since 2014, posing a threat to marine ecosystems. The research found that these heat extremes increase the risk of collapse for crucial ecosystems like coral reefs and kelp forests.
Researchers measured oxygen transport in deep ocean currents, finding that half of atmospheric oxygen is injected into boundary current over 5 months. The findings have implications for climate models and the impact of Arctic changes on the Labrador Sea's 'breathing' process.
University of Delaware professors Wei-Jun Cai and David Kirchman have been named AAAS Fellows for their important contributions to STEM fields. Cai was recognized for his work on the global carbon cycle and ocean acidification, while Kirchman was honored for his research on marine biosciences and microbial ecology.
Research reveals that intense storms in the Southern Ocean increase ocean mixing, bringing carbon dioxide-rich waters to the surface and driving an outgassing of CO2 into the atmosphere. This process has significant implications for understanding global climate models and predicting future climate change.
Researchers from Uppsala University found that ocean productivity declined rapidly 4.6 million years ago in tropical regions, likely caused by reduced East Asian monsoon intensity and decreased riverine nutrient supply, coinciding with changes in the Earth's orbit.
The upper ocean has reached record-breaking temperatures for the sixth consecutive year, with the latest data showing a significant increase in heat content. This warming trend is primarily driven by human-induced climate change, which affects ocean acidification and marine life.
A new study led by NCAR finds that the Southern Ocean absorbs significantly more carbon than it releases, clarifying its role as a carbon sink. Airborne measurements of carbon dioxide reveal critical patterns in the global carbon cycle, providing insights into climate change projections and emission reduction measures.
Ocean predators survive on small, scattered areas of food rather than average concentrations found in the water. Acoustic tools reveal dynamic layered maps of ocean life by interpreting echoes from sound pulses, providing insights into how animals adapt to find and exploit resources.
Scientists have detected a significant acceleration of the Antarctic Circumpolar Current (ACC), the only ocean current that circumnavigates the planet. The study found that climate change is causing the ACC to speed up, with prevailing westerly winds energizing ocean eddies and facilitating property exchange between ocean basins.
A study reconstructed ocean warming history in the Arctic Ocean, finding it began rapidly warming at the start of the 20th century due to Atlantification from the Atlantic Ocean. This warming has led to sea ice retreat and salinity increases.
A new study suggests that the tectonic opening of Southern Ocean seaways led to a sudden cooling event 34 million years ago, contributing to the formation of Antarctic ice sheets. High-resolution simulations showed that this event caused a dramatic drop in coastal temperatures and initiated the Earth's transition into an Icehouse world.
A new study projects that more than eight million tons of pandemic-associated plastic waste have been generated globally, with over 25,000 tons entering the global ocean. The research highlights the need for improved medical waste management in developing countries and calls for global action to reduce plastic pollution.
Researchers have engineered E. coli to produce high levels of ectoine, a natural stabilizer of proteins and membranes, through metabolic engineering and fed-batch fermentation. This breakthrough increases efficiency and reduces the need for high-salinity culture mediums, paving the way for large-scale industrial production.
Researchers found that most coralline algae are negatively impacted by ocean acidification, with decreases in abundance and calcification rates. However, some species, like those in the family Mesophyllumaceae, appear to be more resilient to ocean acidification.
A study found that climate change will alter functioning of marine microbial communities, with plankton at the poles being particularly badly damaged by rising temperatures. In temperate zones, they'll suffer from reduced nutrient flows, while in the tropics, increased salinity will affect them.
Salt stress alters legume responses to symbiotic rhizobacteria by modulating gene expression. Several genes with well-characterized functions in nodulation are highly induced under salt stress, making the plant hypersensitive to bacterial signals.
A new study published in Nature suggests that rainwater is not the primary deposition vector of oceanic mercury, but rather the ocean itself absorbs mercury through gas exchange. The research also indicates that the ocean receives less atmospheric mercury than previously estimated.
A new study led by the University of Miami Rosenstiel School found that changes in ocean salinity due to a more intensified water cycle lead to reduced surface warming. This phenomenon enhances ocean heat uptake into the deep ocean, moderating the pace of global warming.
The Copernicus Ocean State Report reveals record low Arctic ice levels, with a 90% reduction in average sea ice thickness in the Barents Sea. The report also highlights extreme variability in ocean temperatures and oxygen levels, posing significant challenges for marine ecosystems.
Researchers found daily and seasonal fluctuations in chemical conditions despite long-term ocean acidification trends. Massive cycles occur every five to 10 years, causing extreme events that stress sensitive organisms.
Researchers have constructed new sea surface salinity indexes to identify two types of El Niño events (EP and CP) independently. The indexes are based on different key areas with varying ocean salinity patterns.
Researchers tracked insect evolution with major Pacific Ocean currents, revealing species adapted to different conditions. Genetic analysis of ocean skaters found distinct variations among species, mirroring changes in currents and climate.
A study published in Scientific Reports suggests that between 10.3% and 82% of the global ocean may experience new climates with higher temperatures and lower aragonite saturation by 2100. The disappearance of these climates could force marine species to adapt rapidly or disappear.
The deployment of thousands of autonomous robots called BGC-Argo floats is transforming our understanding of marine primary productivity on a global scale. By measuring oxygen production over time, researchers can estimate net primary productivity and shed light on the ocean's role in storing carbon.
A new study led by Bigelow Laboratory for Ocean Sciences suggests that the balance of chemical elements in plankton is primarily dependent on the ratio of nitrogen and phosphorus supplied from the subsurface ocean. This discovery could improve the accuracy of computer models used to forecast ocean change.
A new review paper assesses heat and freshwater changes in the Indian Ocean, finding some consistent responses to anthropogenic global warming. However, observational records are still too short to distinguish natural variability from man-made changes.
A new model developed by Newcastle University's researchers tracks the vertical movement of algae-covered microplastic particles, identifying processes that underpin their trajectories. The study shows that particle properties and algal population dynamics determine the movement of microplastics below the ocean surface.
A study published in Nature Communications found that nearly all nitrogen that fertilizes life in the open ocean of the Gulf of Mexico originates from coastal waters. This discovery is crucial for understanding the food web and survival of commercially valuable species like Atlantic bluefin tuna.
Researchers developed a method to identify areas with smoother waters as indicative of microplastic presence, leveraging CYGNSS satellite data. This technique demonstrates the potential for tracking ocean microplastics from space.
A new report identifies four major barriers to financing a sustainable ocean economy, including weak enabling environment and insufficient public-private investment. Governments, financial institutions, and other players can make financial gains with sustainable ocean investments.
New research suggests that artificial ocean alkalinization can offset ten years of projected acidification in the Great Barrier Reef. The study used a high-resolution model to simulate the impact of alkalinity injection on the reef's acidity, finding that it could sequester 35,000 tons of carbon per year and alleviate the effects of oc...
Researchers found that global warming is causing changes to the Arabian Sea upwelling, which could impact commercial fishing, regional climate, and socioeconomics. The study used coral fossils to analyze seawater temperature and salinity changes over a 1,000-year period.
Researchers found that adding aluminum to seawater increases net carbon fixation of marine diatoms by 10-30%, improving the ocean's ability to absorb CO2. This process can significantly increase the ocean's carbon sink capacity and sequester carbon for long periods, aiding climate change mitigation.
Researchers at George Mason University are studying the impact of castrating parasites on an estuarine crab host in the Chesapeake Bay. They will investigate how environmental salinity affects parasite survival and metamorphosis.
Researchers at FSU's Center for Ocean-Atmospheric Prediction Studies have developed a new virtual tool to track marine litter in the ocean. The tool provides insights into where mismanaged plastic waste is released and ends up, informing policies and regulations to mitigate its impact.
A new study has reduced the Southern Ocean's CO2 uptake uncertainty by 50% using a novel method that constrains the ocean's carbon sink. The approach links human-made CO2 uptake to surface water salinity, allowing for more accurate projections of future climate change.
The Red Sea is now considered a mature ocean basin, approximately 13 million years old, with features similar to those of the young southern Atlantic Ocean. The study uses gravity and earthquake data to develop a new tectonic model, revealing hidden structures such as rift axes and transform faults.
Researchers at UNH discovered that climate change impacts deep-sea corals and sponges variably, with temperature and dissolved oxygen affecting sponge distribution and coral growth. High-resolution video analysis identified specific environmental ranges influencing species sensitivity.
A new study suggests that microplastic ingestion by zooplankton can significantly affect the marine ecosystem's nutrient cycling and oxygen levels. Even low concentrations of microplastics can lead to a strong impact on ecosystems.
The Ocean and Climate Innovation Accelerator (OCIA) consortium aims to advance knowledge of the ocean's role in combating climate change and develop new solutions. The consortium will focus on advancing the 'networked ocean' concept, placing sensors across oceanic environments to monitor critical metrics.
A new study reveals that ocean oxygen depletion will continue for centuries if all CO2 emissions were stopped immediately, more than quadrupling the current loss. The long-term decrease in oxygen primarily affects deeper layers, leading to major shifts in marine ecosystems and potentially changing habitats.
Researchers have reconstructed ocean temperatures over the past 700,000 years using ice core samples from Antarctica, finding that mean ocean temperatures have fluctuated by up to 3°C between ice ages and warm periods.
A new study examines the feasibility of ocean alkalinization to simultaneously address global warming and ocean acidification. The research reveals that nearly doubling the carbon-dioxide uptake rate of the Mediterranean Sea after 30 years could mitigate climate change and counteract acidification.
Scientists predict ocean currents on Enceladus, driven by salinity variations like those in Earth's Southern Ocean. The research suggests a pole-to-equator circulation influencing heat and nutrient distribution.
New study by Stanford and Carnegie Mellon researchers finds that managing high salinity brines from efficient underground carbon sequestration imposes significant energy and emissions penalties. The approach prioritizes storage in low salinity reservoirs, minimizing extraction ratios and recovery extent to reduce penalties.
Research conducted by CNRS and international collaborators reveals that climate change has made the ocean six times stabler over the past 50 years. This increased stability limits oceanic mixing, making it harder for marine organisms to access light and for the ocean to function as a global thermostat.
Researchers from Bigelow Laboratory discovered that copepods gather around small vortexes in the ocean, affecting the food web. These tiny vortexes have significant implications for understanding copepod behavior and their impact on marine ecosystems.
Iron, a micronutrient crucial for phytoplankton, is being released from deep ocean sediments, providing a new source of nutrition for drifting marine organisms. This finding challenges previous expectations and has significant implications for studying the ocean carbon cycle and managing the marine environment.
An international team of researchers has discovered a new type of basalt beneath the Pacific Ocean, which was formed during large and exceptionally hot volcanic eruptions. The discovery suggests that ocean floor eruptions sourced in the Earth's mantle were even hotter and more voluminous than previously thought.