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Revived oceanic CO2 uptake

The Southern Ocean's carbon sink has revived after 'saturating' since 2005 due to changes in weather patterns. The reinvigoration is attributed to variations in wind and temperature, enabling the ocean to absorb more CO2 from the atmosphere.

SourceETH Zurich·JournalScience·DateSep 10, 2015

A snapshot of Americans' knowledge about science

A recent study by the Pew Research Center reveals significant differences in Americans' understanding of various science topics, with educational level being a major factor. Adults with higher education tend to perform better on science-related questions, while gender also plays a role, with men generally outperforming women.

UEA research shows revived oceanic CO2 uptake

Research from the University of East Anglia reveals that the Southern Ocean's carbon sink has reinvigorated after a decade of stagnant absorption. The team attributes this change to shifts in wind patterns and temperature, which have led to increased upwelling of deep waters containing higher concentrations of dissolved CO2.

SourceUniversity of East Anglia·JournalScience·DateSep 10, 2015

Where does water go when it doesn't flow?

A new study by University of Utah researchers shows that two-thirds of the remaining water after rainfall is released by plants, while more than a quarter lands on leaves and evaporates. The study also found that only 38% of water entering groundwater interacts with soil before reaching streams and groundwater.

SourceUniversity of Utah·JournalScience·DateJul 9, 2015

Where iron and water mix

A new study reveals that chemical-laden plumes from hydrothermal vents can be traced across the Pacific for over 4,000 kilometers and impact global ocean chemistry. The iron transported by these plumes has the potential to serve as a key life-sustaining micro-nutrient in the surface oceans of Antarctica.

Making organic molecules in hydrothermal vents in the absence of life

Researchers at Woods Hole Oceanographic Institution discovered that methane formation occurs independently of venting process and is produced on geological time scales deep beneath seafloor. Abiotic compound formate is formed during vent circulation process, providing evidence for purely chemical processes in origin of life.

SourceWoods Hole Oceanographic Institution·JournalProceedings of the National Academy of Sciences·DateJun 8, 2015

Solving corrosive ocean mystery reveals future climate

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.

SourcePenn State·JournalNature Geoscience·DateMay 11, 2015

Ocean fronts improve climate and fishery production, study finds

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.

SourceUniversity of Georgia·JournalProceedings of the National Academy of Sciences·DateMay 1, 2015

Antibiotic resistance risk for coastal water users

A study published this week found that over 6.3 million people may be exposed to antibiotic-resistant bacteria while engaging in water sports, with surfers and swimmers at highest risk. The research highlights the importance of maintaining good water quality standards to minimize exposure to these harmful microbes.

SourceMicrobiology Society·JournalEnvironment International·DateMar 29, 2015