Sinks for Anthropogenic Carbon

By J. Sarmiento, N. Gruber. 2002

387 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/247ff1517304ab29e4216b9edcf73931ef10b9b8

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Citations in the corpus

Effects of global climate change on marine and estuarine fishes and fisheries (2004, background): “However, since the Industrial Revolution (19th Century), many compounds that naturally existed in small quantities have been mass produced and added to our atmosphere through anthropogenic activities (Sarmiento and Gruber, 2002).”
Animating the Carbon Cycle (2014, background): “*Corresponding author; e-mail: oswald.schmitz@yale.edu and others 1990; Falkowski and others 2000; Sarmiento and Gruber 2002; Houghton 2007).”
The conundrum of marine N2 fixation (2005, background): “Indermuhle, A., Stocker, T. F., Joos, F., Fischer, H., Smith, H. J., Wahlen, M., Deck, B., Mastroianni, D., Tschumi, J., Blunier, T., Meyer, R., and Stauffer, B., 1999, Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome, Antarctica: Nature, v. 398, p. 121–126.”
Feedback for physicists: A tutorial essay on control (2005, background): “There is a tremendous flux of carbon between the atmosphere and various “sinks,” such as the oceans and forests, and the dependence of these fluxes on greenhouse gasses must be evaluated accurately to know the cumulative effect on climate (Sarmiento and Gruber, 2002).”
The microbial aspect of climate change (2016, background): “The upper oceanic layer is the boundary where CO2 and other greenhouse gases have accumulated in course of decades, and the deep ocean is the most formidable carbon storehouse in the world (Gruber et al. 2002; Sarmiento and Gruber 2002).”
Late-summer carbon fluxes from Canadian forests and peatlands along an east-west continental transect (2006, background): “The two primary factors responsible for modifying the terrestrial C cycle are (i) extraction and emission of C from long-term stores of fossil fuels and (ii) changes in land cover and land use (Sarmiento and Gruber 2002).”
Dynamics of Marine Ecosystems: Mann/Dynamics of Marine Ecosystems (2005, background): “Recent data from the major oceans (Sarmiento and Gruber 2002) show that anthropogenic carbon tends to be confined to the upper few hundred meters of the ocean.”
Well Technologies for CO2 Geological Storage: CO2-Resistant Cement (2007, background): “Storing carbon dioxide underground is considered as the most effective way for long-term safe and low cost CO2 sequestration (Sarmiento and Gruber, 2002; Gielen, 2003).”
A Chinese Sky Trust? Distributional Impacts of Carbon charges and Revenue Recycling in China (2007, background): “2 Oceanic sinks and terrestrial sinks each absorb roughly 1900 million mtC/year; but land-use changes (especially deforestation) release roughly 1700 mtC/year; in net terms, oceanic sinks therefore account for close to 90% of annual carbon sequestration (Sarmiento and Gruber 2002).”
Biomineralization and global biogeochemical cycles (2003, background): “1 Sources: Treguer et al. (1995); Berner and Berner (1996); Sarmiento and Gruber (2002) ; Klaas and Archer (2002); Slomp et al. (2003).”