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When can ocean acidification impacts be detected from decadal alkalinity measurements? ArchiMer
Carter, B. R.; Frolicher, T. L.; Dunne, J. P.; Rodgers, K. B.; Slater, R. D.; Sarmiento, J. L..
We use a large initial condition suite of simulations (30 runs) with an Earth system model to assess the detectability of biogeochemical impacts of ocean acidification (OA) on the marine alkalinity distribution from decadally repeated hydrographic measurements such as those produced by the Global Ship-Based Hydrographic Investigations Program (GO-SHIP). Detection of these impacts is complicated by alkalinity changes from variability and long-term trends in freshwater and organic matter cycling and ocean circulation. In our ensemble simulation, variability in freshwater cycling generates large changes in alkalinity that obscure the changes of interest and prevent the attribution of observed alkalinity redistribution to OA. These complications from...
Tipo: Text Palavras-chave: Alkalinity; Ocean acidification; Trend detection; Repeat hydrography; Carbon cycle; Carbonate system.
Ano: 2016 URL: https://archimer.ifremer.fr/doc/00383/49419/49860.pdf
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Quantification of ocean heat uptake from changes in atmospheric O-2 and CO2 composition ArchiMer
Resplandy, L.; Keeling, R. F.; Eddebbar, Y.; Brooks, M.; Wang, R.; Bopp, L.; Long, Mc; Dunne, J. P.; Koeve, W.; Oschlies, A..
The ocean is the main source of thermal inertia in the climate system. Ocean heat uptake during recent decades has been quantified using ocean temperature measurements. However, these estimates all use the same imperfect ocean dataset and share additional uncertainty due to sparse coverage, especially before 2007. Here, we provide an independent estimate by using measurements of atmospheric oxygen (O-2) and carbon dioxide (CO2) - levels of which increase as the ocean warms and releases gases - as a whole ocean thermometer. We show that the ocean gained 1.29 +/- 0.79 x 10(22) Joules of heat per year between 1991 and 2016, equivalent to a planetary energy imbalance of 0.80 +/- 0.49W watts per square metre of Earth's surface. We also find that the...
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Ano: 2019 URL: https://archimer.ifremer.fr/doc/00676/78794/81050.pdf
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Air-sea CO2 flux in the Pacific Ocean for the period 1990-2009 ArchiMer
Ishii, M.; Feely, R. A.; Rodgers, K. B.; Park, G. -h.; Wanninkhof, R.; Sasano, D.; Sugimoto, H.; Cosca, C. E.; Nakaoka, S.; Telszewski, M.; Nojiri, Y.; Fletcher, S. E. Mikaloff; Niwa, Y.; Patra, P. K.; Valsala, V.; Nakano, H.; Lima, I.; Doney, S. C.; Buitenhuis, E. T.; Aumont, Olivier; Dunne, J. P.; Lenton, A.; Takahashi, T..
Air-sea CO2 fluxes over the Pacific Ocean are known to be characterized by coherent large-scale structures that reflect not only ocean subduction and upwelling patterns, but also the combined effects of wind-driven gas exchange and biology. On the largest scales, a large net CO2 influx into the extratropics is associated with a robust seasonal cycle, and a large net CO2 efflux from the tropics is associated with substantial interannual variability. In this work, we have synthesized estimates of the net air-sea CO2 flux from a variety of products, drawing upon a variety of approaches in three sub-basins of the Pacific Ocean, i. e., the North Pacific extratropics (18-66 degrees N), the tropical Pacific (18 degrees S-18 degrees N), and the South Pacific...
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Ano: 2014 URL: http://archimer.ifremer.fr/doc/00192/30320/28789.pdf
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