ArticleGlobal biogeochemical cycles2022
Attribution of Space-Time Variability in Global-Ocean Dissolved Inorganic Carbon.
Article in Global biogeochemical cycles, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
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Who cites it
3 citing papers in PubMed.
- Mechanistic Insights into Mercury Photoreduction: Effects of Dissolved Organic Matter and Inorganic Carbon in Seawater.Environmental science & technology · 2026Article
- Roles of sulfate-reducing bacteria in sustaining the diversity and stability of marine bacterial community.Frontiers in microbiology · 2023Article
- Attribution of Space-Time Variability in Global-Ocean Dissolved Inorganic Carbon.Global biogeochemical cycles · 2022Article
Corrections and comments
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Authors and funding
19 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The inventory and variability of oceanic dissolved inorganic carbon (DIC) is driven by the interplay of physical, chemical, and biological processes. Quantifying the spatiotemporal variability of these drivers is crucial for a mechanistic understanding of the ocean carbon sink and its future trajectory. Here, we use the Estimating the Circulation and Climate of the Ocean-Darwin ocean biogeochemistry state estimate to generate a global-ocean, data-constrained DIC budget and investigate how spatial and seasonal-to-interannual variability in three-dimensional circulation, air-sea CO
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Registered trials
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