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Contrasting Controls of Acidification Metrics Across Environmental Gradients in the North Pacific and the Adjunct Arctic Ocean: Insight From a Transregional Study

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This article is published in Geophysical Research Letters.The article was published on 2021-10-16. It has received 6 citations till now. The article focuses on the topics: Arctic.

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Ocean Biogeochemical Dynamics

TL;DR: Sensitivity of global ocean biogeochemical dynamics to ecosystem structure in a future climate and model methods for Marine Science are described.
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Climate change drives rapid decadal acidification in the Arctic Ocean from 1994 to 2020

TL;DR: In this article , the authors report rapid acidification in the Arctic Ocean, with rates three to four times higher than in other ocean basins, and attribute it to changing sea ice coverage on a decadal time scale.

Accelerated Accumulation of Anthropogenic CO2 Drives Rapid Acidification in the North Pacific Subtropical Mode Water During 1993–2020

TL;DR: In this paper , the authors show that the acidification rate of the North Pacific subtropical mode water (STMW) during 2005-2020 is about two times of that during 1993-2005, which is due to cooling-driven enhanced CANT accumulation in the formation waters in the recent period.
References
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Ocean Acidification: Present Conditions and Future Changes in a High-CO2 World

TL;DR: In this article, the authors published a paper entitled "Oceanography 22 no. 4 (2009): 36-47", which is a summary of the Oceanography 22 No. 4 issue.
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Relationship between wind speed and gas exchange over the ocean revisited

TL;DR: In this paper, the authors provide an update on the frequently used method of Wanninkhof (1992) for estimating bulk fluxes of atmospheric gases across the air-sea interface, using revised global ocean 14C inventories and improved wind speed products.
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Ocean pCO2 calculated from dissolved inorganic carbon, alkalinity, and equations for K1 and K2: validation based on laboratory measurements of CO2 in gas and seawater at equilibrium

TL;DR: In this paper, the first and second dissociation constants of carbonic acid, K 1 and K 2, were reformulated to give equations for pK 1 and p K 2 (p K =−log 10 K ) as a function of seawater temperature and salinity, consistent with the total hydrogen ion concentration scale.
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Ecosystem effects of ocean acidification in times of ocean warming: a physiologist’s view

TL;DR: In this paper, the authors build on the view that development of a cause and effect understanding is required beyond empirical observations, for a more accurate projection of ecosystem effects and for quantitative scenarios, and identify the mechanisms through which temperature and CO2-related ocean physicochemistry affect organism fitness, survival and success.
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Photosynthetic quotients, new production and net community production in the open ocean

TL;DR: Based on balanced chemical equations for the production of proteins, polysaccharides, lipids and nucleic acids from inorganic precursors and reported estimates of the composition of microalgal biomass, the photosynthetic quotients (PQs) for new and recycled production are estimated to be 1.4 ± 0.1, respectively.
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