Ocean acidification (OA) has resulted in global-scale changes in ocean chemistry, which
can disturb marine organisms and ecosystems. Despite its extensively populated coastline …

We have estimated global air–sea CO 2 fluxes (fg CO 2) from the open ocean to coastal
seas. Fluxes and associated uncertainty are computed from an ensemble-based …

We present the first global ocean‐biogeochemistry model that uses a telescoping high
resolution for an improved representation of coastal carbon dynamics: ICON‐Coast. Based …

Ocean acidification (OA) progression is affected by multiple factors, such as ocean warming,
biological production, and river runoff. Here we used an ocean‐biogeochemical model to …

Coral reefs are globally in decline and western Atlantic reefs have experienced the greatest
losses in live coral cover of any region. The Flower Garden Banks (FGB) in the Gulf of …

Abstract The South Atlantic Ocean is historically less sampled than the North Atlantic Ocean.
Recent efforts have improved our understanding of the carbonate system variable …

Quantifying air-sea carbon dioxide (CO 2) flux from observations is subject to uncertainties
due to missing data, uneven data distribution, and a relatively short observation period in the …

A four-decade dataset that spans seven estuaries along a latitudinal gradient in the
northwestern Gulf of Mexico and includes measurements of pH and total alkalinity was used …

A three-dimensional (3-D) physical-biogeochemical-carbon cycle coupled model is used to
investigate the interannual variability of the air-sea carbon dioxide (CO2) flux (F CO2) in the …

In the northern Gulf of Mexico shelf, the Mississippi‐Atchafalaya River System (MARS)
impacts the carbonate system by delivering freshwater with a distinct seasonal pattern in …