Alkalinity, the excess of proton acceptors over donors, plays a major role in ocean chemistry,
in buffering and in calcium carbonate precipitation and dissolution. Understanding alkalinity …

Wetlands cover a small portion of the world, but have disproportionate influence on global
carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes …

The Arctic Ocean has experienced rapid warming and sea ice loss in recent decades,
becoming the first open-ocean basin to experience widespread aragonite undersaturation …

The ocean's chemistry is changing due to the uptake of anthropogenic carbon dioxide
(CO2). This phenomenon, commonly referred to as “Ocean Acidification”, is endangering …

Compound MHW-OAX events, during which marine heatwaves (MHWs) co-occur with ocean
acidity extreme (OAX) events, can have larger impacts on marine ecosystems than the …

According to modelling studies, ocean alkalinity enhancement (OAE) is one of the proposed
carbon dioxide removal (CDR) approaches with large potential, and the beneficial side …

Ocean acidification has altered the ocean's carbonate chemistry profoundly since
preindustrial times, with potentially serious consequences for marine life. Yet, no long-term …

Oceanic dissolved inorganic carbon (TC) is the largest pool of carbon that substantially
interacts with the atmosphere on human timescales. Oceanic TC is increasing through …

A major surface circulation feature of the Arctic Ocean is the Transpolar Drift (TPD), a current
that transports river‐influenced shelf water from the Laptev and East Siberian Seas toward …

Accurately predicting future ocean acidification (OA) conditions is crucial for advancing OA
research at regional and global scales, and guiding society's mitigation and adaptation …