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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.
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Aragonite saturation states and pH in western Norwegian fjords:seasonal cycles and controlling factors, 2005–2009

TL;DR: In this paper, the authors use weekly underway data from the Voluntary Observing Ships (VOS) program covering the period 2005-2009 combined with data from research cruises to estimate aragonite saturation state (ΩAr) and pH values in several adjacent western Norwegian fjords, and evaluate how seawater CO2 chemistry drives their variations in response to physical and biological factors.
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Reconciliation of pH25 and pHinsitu acidification rates of the surface oceans: A simple conversion using only in situ temperature

TL;DR: In this article, the difference between calculated pHinsitu and pH25 is a 1 (T − 25°C), where a1 is a nearly constant of − 0.0151 pH unit °C−1.
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