The DOI matches its Crossref record; 24 of the 26 references it cites were found in a registry or an index.
Simulated response of the ocean carbon cycle to anthropogenic climate warming
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“Associated with the warming-driven stratification of the ocean is a restriction in nutrient supply and thus biological (export) production [Plattner et al., 2001;Sarmiento et al., 1998], with a peak year $2200 reduction of about 16% (Figure 8b).”
From Regulation of atmospheric CO 2 by deep‐sea sediments in an Earth system model (2007) · cites this paper as Sarmiento et al., 1998
In the citing paper
“Additionally, the upper ocean becomes globally more stratified owing to increases in surface temperature and precipitation [Manabe et al., 1991; Manabe and Stouffer, 1993; Sarmiento et al., 1998].”
From Potential impact of climate change on marine export production (2001) · cites this paper as Sarmiento et al., 1998
In the citing paper
“Upper ocean warming could increase water column stratification [37][38][39], potentially counteracting the effects of intensifying upwelling-favorable winds by reducing the efficacy of coastal upwelling to deliver nutrients to the euphotic zone.”
From Anticipated Effects of Climate Change on Coastal Upwelling Ecosystems (2015) · cites this paper as [37]
In the citing paper
“As a result of enhanced stratification and reduced ventilation, next generation GCMs predict a decline in dissolved oxygen with high certainty [37,52,53]”
From Anticipated Effects of Climate Change on Coastal Upwelling Ecosystems (2015) · cites this paper as [37]
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Nitrogen cycles: Past, present, and future
Galloway, J. N., Dentener, F. J., Capone, D. G., Boyer, E. W., Howarth, R. W., Seitzinger, S. P., Asner, G. P., Cleveland, C. C., Green, P. A., Holland, E. A., et al. (2004) · Biogeochemistry · doi:10.1007/s10533-004-0370-0 · Cited by 5,315
“2000) could lead to both greater upper water column stability through much of the ocean as well as decreased circulation in the deep ocean (Sarmiento et al. 1998; Joos et al. 1999), both with significant implication to the marine N cycle.”
BackgroundAcceleration of global warming due to carbon-cycle feedbacks in a coupled climate model
Cox, P. M., Betts, R., JONES, C. D., Spall, S. A., & Totterdell, I. J. (2000) · Nature · doi:10.1038/35041539 · Cited by 4,169
Climate–Carbon Cycle Feedback Analysis: Results from the C4MIP Model Intercomparison
Friedlingstein, P., Cox, P., Betts, R., Bopp, L., von Bloh, W., Brovkin, V., Cadule, P., Doney, S., Eby, M., Fung, I., et al. (2006) · Journal of Climate · doi:10.1175/jcli3800.1 · Cited by 2,902
“Projected changes in sea surface temperature and oceanic circulation lead to a reduction of carbon uptake (e.g., Sarmiento et al. 1998; Chuck et al. 2005).”
Biogeochemical Controls and Feedbacks on Ocean Primary Production
Falkowski, P. G., Barber, R. T., & Smetacek, V. (1998) · Science · doi:10.1126/science.281.5374.200 · Cited by 2,848
Processes and patterns of oceanic nutrient limitation
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Climate-driven trends in contemporary ocean productivity
Behrenfeld, M. J., O’Malley, R. T., Siegel, D. A., McClain, C. R., Sarmiento, J. L., Feldman, G. C., Milligan, A. J., Falkowski, P. G., Letelier, R. M., & Boss, E. S. (2006) · Nature · doi:10.1038/nature05317 · Cited by 2,485
Self-citationThe Global Carbon Cycle: A Test of Our Knowledge of Earth as a System
Falkowski, P., Scholes, R. J., Boyle, E., Canadell, J., Canfield, D., Elser, J., Gruber, N., Hibbard, K., Högberg, P., Linder, S., et al. (2000) · Science · doi:10.1126/science.290.5490.291 · Cited by 2,177
Ocean Deoxygenation in a Warming World
Keeling, R. F., Körtzinger, A., & Gruber, N. (2010) · Annual Review of Marine Science · doi:10.1146/annurev.marine.010908.163855 · Cited by 1,712
“The realization that future global warming might significantly impact ocean O2 distributions is very recent, dating back only a decade (Sarmiento et al. 1998).”
BackgroundInfluentialMultiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models
Bopp, L., Resplandy, L., Orr, J. C., Doney, S. C., Dunne, J. P. P., Gehlen, M., Halloran, P. R., Heinze, C., Ilyina, T., Séférian, R., et al. (2013) · Biogeosciences · doi:10.5194/bg-10-6225-2013 · Cited by 1,809
“Coupled climate–marine biogeochemical models used over the past 15 yr all project a long-term decrease in the oceanic O 2 inventory in response to anthropogenic global warming (e.g., Sarmiento et al., 1998; Plattner et al., 2001; Bopp et al., 2002).”
MethodA mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization
Boyd, P. W., Watson, A. J., Law, C. S., Abraham, E. R., Trull, T. W., Murdoch, R. C., Bakker, D. C. E., Bowie, A. R., Buesseler, K. O., Chang, H., et al. (2000) · Nature · doi:10.1038/35037500 · Cited by 1,614
“The Southern Ocean is thought to have a disproportionate influence on the functioning of the global carbon cycle in both the presen”
BackgroundMarine microorganisms and global nutrient cycles
Arrigo, K. R. (2004) · Nature · doi:10.1038/nature04159 · Cited by 1,483
“In addition, if predictions by global climate models (GCMs) are correct and if surface waters in polar regions become more stratifie”
Glacial/interglacial variations in atmospheric carbon dioxide
Sigman, D. M., & Boyle, E. A. (2000) · Nature · doi:10.1038/35038000 · Cited by 1,439
High-latitude controls of thermocline nutrients and low latitude biological productivity
Sarmiento, J. L., Gruber, N., Brzezinski, M. A., & Dunne, J. P. P. (2003) · Nature · doi:10.1038/nature02127 · Cited by 1,402
“The Southern Ocean has long been recognized as playing a central role in the global carbon cycle and biological productivity, and in the response of these to climate chang”
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“Change in ocean circulation, impact on light and nutrient regimes Coupled ocean atmosphere models project there will be changes in ocean circulation and water column stratification (Sarmiento et al., 1998) and therefore light and nutrient regimes over the next decades due to changes in climate.”
BackgroundMcGroddy, M., Daufresne, T., & Hedin, L. O. (2004) · Ecology · doi:10.1890/03-0351 · Cited by 1,122
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Zooplankton fecal pellets, marine snow, phytodetritus and the ocean’s biological pump
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“…pump, particularly in alreadystratified waters of the tropics and subtropics (Behrenfeld et al., 2006; Bopp et al., 2001; Boyce et al., 2010; Doney, 2006; Huisman et al., 2006; Matear and Hirst, 1999; Norris et al., 2013; Sarmiento et al., 1998, 2004; Siegel and Franz, 2010; Yool et al., 2013).”
BackgroundGlobal Climatic Impacts of a Collapse of the Atlantic Thermohaline Circulation
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“The oceanic carbon cycle is sensitive to changes in SST (which affects carbon solubility), to the amount of sea ice cover, and to the amount of vertical mixing and deep water formation that ventilates the deep ocean, (e.g. Sarmiento et al., 1998).”
BackgroundEcosystem dynamics based on plankton functional types for global ocean biogeochemistry models
Quéré, C. L., Harrison, S. P., Prentice, I. C., Buitenhuis, E. T., Aumont, O., Bopp, L., Claustre, H., da Cunha, L. C., Geider, R. J., Giraud, X., et al. (2005) · Global Change Biology · doi:10.1111/j.1365-2486.2005.1004.x · Cited by 894
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“This firstorder response is modified by other processes such as ocean warming and changes in ocean circulation and marine biogeochemistry (Plattner et al., 2001; Sarmiento et al., 1998; Joos et al., 1999).”
Effect of natural iron fertilization on carbon sequestration in the Southern Ocean
Blain, S., Quéguiner, B., Armand, L., Belviso, S., Bombled, B., Bopp, L., Bowie, A., Brunet, C., Brussaard, C., Carlotti, F., et al. (2007) · Nature · doi:10.1038/nature05700 · Cited by 795
Phytoplankton Community Structure and the Drawdown of Nutrients and CO 2 in the Southern Ocean
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Global nitrogen deposition and carbon sinks
Reay, D., Dentener, F. J., Smith, P., Grace, J., & Feely, R. A. (2008) · Nature Geoscience · doi:10.1038/ngeo230 · Cited by 765
Primary production in the Southern Ocean, 1997–2006
Arrigo, K. R., A, G. L. V. D., & Bushinsky, S. M. (2008) · Journal of Geophysical Research Atmospheres · doi:10.1029/2007jc004551 · Cited by 753
“One area of general agreement among models is that stratification of the surface Southern Ocean is likely to increase over the next century in response to changes in atmospheric CO2 and temperature [Sarmiento et al., 1998; Caldeira and Duffy, 2000; Le Quéré et al., 2007].”
BackgroundImpacts of Climate Change on Marine Organisms and Ecosystems
Brierley, A. S., & Kingsford, M. J. (2009) · Current Biology · doi:10.1016/j.cub.2009.05.046 · Cited by 726
“Reduced photosynthetic carbon fixation may reduce CO2[atm] drawdown [106], with further climate consequences.”
BackgroundDominance of the Southern Ocean in Anthropogenic Carbon and Heat Uptake in CMIP5 Models
Frölicher, T. L., Sarmiento, J. L., Paynter, D. J., Dunne, J. P. P., Krasting, J. P., & Winton, M. (2014) · Journal of Climate · doi:10.1175/jcli-d-14-00117.1 · Cited by 682
“…Ocean will also likely experience an increase in stratification and a reduction in vertical mixing that may reduce the upward flux of natural CO 2 and the downward flux of anthropogenic CO 2 (Sarmiento et al. 1998), making it difficult to project the impact of strat-ification on the total CO 2 sink.”
BackgroundResultInfluentialSelf-citationProjected 21st century decrease in marine productivity: a multi-model analysis
Steinacher, M., Joos, F., Frölicher, T. L., Bopp, L., Cadule, P., Cocco, V., Doney, S. C., Gehlen, M., Lindsay, K., Moore, J. K., et al. (2010) · Biogeosciences · doi:10.5194/bg-7-979-2010 · Cited by 675
“Two different regimes for change in PP and EP are identified, that were already discussed previously in the literature (Bopp et al., 2001; Sarmiento et al., 1998).”
BackgroundEffects of global climate change on marine and estuarine fishes and fisheries
Roessig, J. M., Woodley, C. M., Cech, J. J., & Hansen, L. J. (2004) · Reviews in Fish Biology and Fisheries · doi:10.1007/s11160-004-6749-0 · Cited by 657
“Increasing water temperature decreases the solubility of CO2, resulting in the slowed uptake of atmospheric CO2 (Kwon and Schnoor, 1994; Sarmiento et al., 1998; Plattner et al., 2001).”
BackgroundInfluentialEcosystems, their properties, goods and services
Fischlin, A., Midgley, G. F., Turley, C., & Velichko, A. A. (2007) · IRIS · Cited by 623
Warming up, turning sour, losing breath: ocean biogeochemistry under global change
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Oceanic sources, sinks, and transport of atmospheric CO2
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“…and natural CO 2 are expected to change considerably in the future in response to continually rising atmospheric CO 2 and global climate change [ Sarmiento et al. , 1998; Joos et al. , 1999b; Matear and Hirst , 1999; Plattner et al. , 2001; Gruber et al. , 2004; Yoshikawa et al. , 2008].”
BackgroundSelf-citationThe impact of remineralization depth on the air–sea carbon balance
Kwon, E. Y., Primeau, F., & Sarmiento, J. L. (2009) · Nature Geoscience · doi:10.1038/ngeo612 · Cited by 515
“The latter model is more appropriate if new production is limited by external factors such as light or micronutrient input from wind-blown dus”
BackgroundSelf-citationPotential impact of climate change on marine export production
Bopp, L., Monfray, P., Aumont, O., Dufresne, J., Le Treut, H., Madec, G., Terray, L., & Orr, J. C. (2001) · Global Biogeochemical Cycles · doi:10.1029/1999gb001256 · Cited by 514
Lutz, M. J., Caldeira, K., Dunbar, R. B., & Behrenfeld, M. J. (2007) · Journal of Geophysical Research Atmospheres · doi:10.1029/2006jc003706 · Cited by 478
Global Nitrogen Cycle: Critical Enzymes, Organisms, and Processes for Nitrogen Budgets and Dynamics
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Understanding the export of biogenic particles in oceanic waters: Is there consensus?
Boyd, P. W., & Trull, T. W. (2006) · Progress In Oceanography · doi:10.1016/j.pocean.2006.10.007 · Cited by 508
Anticipated Effects of Climate Change on Coastal Upwelling Ecosystems
Bakun, A., Black, B. A., Bograd, S. J., García-Reyes, M., Miller, A. J., Rykaczewski, R. R., & Sydeman, W. J. (2015) · Current Climate Change Reports · doi:10.1007/s40641-015-0008-4 · Cited by 470
“As a result of enhanced stratification and reduced ventilation, next generation GCMs predict a decline in dissolved oxygen with high certainty [37, 52, 53]; large-scale ocean circulation could advect these modified deep waters into EBUS [54].”
BackgroundBiogenic Carbon Cycling in the Upper Ocean: Effects of Microbial Respiration
Rivkin, R. B., & Legendre, L. (2001) · Science · doi:10.1126/science.291.5512.2398 · Cited by 460
Response of diatoms distribution to global warming and potential implications: A global model study
Bopp, L., Aumont, O., Cadule, P., Alvain, S., & Gehlen, M. (2005) · Geophysical Research Letters · doi:10.1029/2005gl023653 · Cited by 455
“biogeochemical parameterizations [Sarmiento et al., 1998; Maier-Reimer et al., 1996;Matear and Hirst, 1999; Plattner et al., 2001; Dufresne et al., 2002] or rudimentary biological (NPZD) models [Cox et al.”
BackgroundMethodSterman, J. D., & Sweeney, L. B. (2007) · Climatic Change · doi:10.1007/s10584-006-9107-5 · Cited by 456
Boyd, P. W., Rynearson, T. A., Armstrong, E. A., Fu, F., Hayashi, K., Hu, Z., Hutchins, D. A., Kudela, R. M., Litchman, E., Mulholland, M. R., et al. (2013) · PLoS ONE · doi:10.1371/journal.pone.0063091 · Cited by 429
“Both global modelling experiments [10] and timeseries data [11] reveal that the upper ocean is already warming in many regions (excluding upwelling regions, [12] and is highly likely to continue warming as a result of a changing climate.”
BackgroundOxygen declines and the shoaling of the hypoxic boundary in the California Current
Bograd, S. J., Castro, C. G., Di Lorenzo, E., Palacios, D. M., Bailey, H., Gilly, W., & Chavez, F. P. (2008) · Geophysical Research Letters · doi:10.1029/2008gl034185 · Cited by 420
“with most of this reduction attributed to enhanced nearsurface stratification [Sarmiento et al., 1998; Keeling and Garcia, 2002].”
BackgroundMethodInfluentialOcean primary production and climate: Global decadal changes
Gregg, W. W., Conkright, M. E., Ginoux, P. A., O’Reilly, J. E., & Casey, N. W. (2003) · Geophysical Research Letters · doi:10.1029/2003gl016889 · Cited by 410
“Warmer ocean temperatures increase stratification of the surface mixed layer, which inhibits the entrainment of nutrients from below to support ocean primary production [Sarmiento et al., 1998].”
BackgroundInfluentialMarine viruses and global climate change
Danovaro, R., Corinaldesi, C., Dell’Anno, A., Fuhrman, J. A., Middelburg, J. J., Noble, R. T., & Suttle, C. A. (2010) · FEMS Microbiology Reviews · doi:10.1111/j.1574-6976.2010.00258.x · Cited by 428
Global warming-enhanced stratification and mass mortality events in the Mediterranean
Coma, R., Ribes, M., Serrano, E., Jiménez, E., Salat, J., & Pascual, J. (2009) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0805801106 · Cited by 422
“Stratification of the water column is a key control of marine productivity (32) that affects the flux of carbon and temperature of the coupled ocean–atmosphere system (33, 34), a main determinant of global climate (35).”
BackgroundOcean circulation in a warming climate
Toggweiler, J. R., & Russell, J. L. (2008) · Nature · doi:10.1038/nature06590 · Cited by 398
“According to these models, polar freshening should have already led to some weakening of the overturning and more stratification of the polar oceans in both hemisphere”
Schmittner, A., Oschlies, A., Matthews, H. D., & Galbraith, E. D. (2008) · Global Biogeochemical Cycles · doi:10.1029/2007gb002953 · Cited by 427
“This is also true for estimates of future climate–carbon cycle feedbacks [Maier-Reimer et al., 1996; Sarmiento et al., 1998; Matear and Hirst, 1999; Cox et al., 2000; Joos et al., 2001; Dufresne et al., 2002; Friedlingstein et al., 2003; Jones et al., 2003; Zeng et al., 2004; Govindasamy et al.,…”
BackgroundReduced mixing generates oscillations and chaos in the oceanic deep chlorophyll maximum
Huisman, J., Thi, N. N. P., Karl, D. M., & Sommeijer, B. P. (2006) · Nature · doi:10.1038/nature04245 · Cited by 393
How positive is the feedback between climate change and the carbon cycle?
Friedlingstein, P., Dufresne, J., Cox, P. M., & Rayner, P. J. (2003) · Tellus B · doi:10.1034/j.1600-0889.2003.01461.x · Cited by 391
Science Plan and Implementation Strategy
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Geider, R. J., DeLucia, E. H., Falkowski, P. G., Finzi, A. C., Grime, J. P., Grace, J., Kana, T. M., LaRoche, J., Long, S. P., Osborne, B. A., et al. (2001) · Global Change Biology · doi:10.1046/j.1365-2486.2001.00448.x · Cited by 379
“Sarmiento et al. (1998) suggest that changes in the biology of the pump may be the most critical component of the oceanic responses to future changes in climate and CO2.”
BackgroundJONES, C. D., Arora, V. K., Friedlingstein, P., Bopp, L., Brovkin, V. A., Dunne, J. P. P., Graven, H., Hoffman, F. M., Ilyina, T., John, J. G., et al. (2016) · Geoscientific model development · doi:10.5194/gmd-9-2853-2016 · Cited by 397
“The processes behind the former (carbonate chemistry and solubility) were reasonably well understood (Bacastow, 1993), but the latter was much more uncertain being sensitive to the underlying ocean model circulation (Maier-Reimer et al., 1996; Sarmiento et al., 1998; Joos et al., 1999).”
BackgroundCritical oxygen levels and metabolic suppression in oceanic oxygen minimum zones
Seibel, B. A. (2010) · Journal of Experimental Biology · doi:10.1242/jeb.049171 · Cited by 368
The Variable Southern Ocean Carbon Sink
Gruber, N., Landschützer, P., & Lovenduski, N. S. (2018) · Annual Review of Marine Science · doi:10.1146/annurev-marine-121916-063407 · Cited by 356
“However, they provide a glimpse into the future (Sarmiento et al. 1998, Lovenduski & Ito 2009).”
BackgroundEnhanced upper ocean stratification with climate change in the CMIP3 models
Capotondi, A. M., Alexander, M. A., Bond, N. A., Curchitser, E., & Scott, J. D. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jc007409 · Cited by 352
“[5] Oceanic oxygen observations show concentration declines in many areas of the World Ocean, with the North Pacific and tropical oceans being the best resolved regions due to the availability of long-term moorings and repeated hydrographic sections [Sarmiento et al., 1998].”
BackgroundOceanic sinks for atmospheric CO2
Raven, J. A., & Falkowski, P. G. (1999) · Plant Cell & Environment · doi:10.1046/j.1365-3040.1999.00419.x · Cited by 372
Nonlinearities, Feedbacks and Critical Thresholds within the Earth's Climate System
Rial, J. A., Pielke, R. A., Beniston, M., Claussen, M. A., Canadell, J. G., Cox, P. M., Held, H., de Noblet‐Ducoudré, N., Prinn, R. G., Reynolds, J. F., et al. (2004) · Climatic Change · doi:10.1023/b:clim.0000037493.89489.3f · Cited by 351
Global Warming and Marine Carbon Cycle Feedbacks on Future Atmospheric CO 2
Joos, F., Plattner, G., Stocker, T. F., Marchal, O., & Schmittner, A. (1999) · Science · doi:10.1126/science.284.5413.464 · Cited by 345
Vulnerability to climate change and reasons for concern: a synthesis
Smith, J. B., Schellnhuber, H. J., Mirza, M. M. Q., Fankhauser, S., Leemans, R., Lin, E., Ogallo, L. A., Pittock, B., Richels, R., Rosenzweig, C. E., et al. (2001) · Socio-Environmental Systems Modeling · Cited by 342
Climate‐induced oceanic oxygen fluxes: Implications for the contemporary carbon budget
Bopp, L., Quéré, C. L., Heimann, M., Manning, A. C., & Monfray, P. (2002) · Global Biogeochemical Cycles · doi:10.1029/2001gb001445 · Cited by 339
“However, in addition, this warming is also likely to lead to changes in ocean dynamics (stratification, convective mixing, and deepwater formation) [Manabe and Stouffer, 1993; Sarmiento et al., 1998], which would in turn impact biological activity [Bopp et al., 2001].”
BackgroundResultInfluentialPositive feedback between future climate change and the carbon cycle
Friedlingstein, P., Bopp, L., Ciais, P., Dufresne, J., Fairhead, L., Treut, H. L., Monfray, P., & Orr, J. C. (2001) · Geophysical Research Letters · doi:10.1029/2000gl012015 · Cited by 338
Rapid and early export of Phaeocystis antarctica blooms in the Ross Sea, Antarctica
DiTullio, G. R., Grebmeier, J. M., Arrigo, K. R., Lizotte, M. P., Robinson, D. H., Leventer, A. R., Barry, J., VanWoert, M., & Dunbar, R. B. (2000) · Nature · doi:10.1038/35007061 · Cited by 334
“and is expected to be vulnerable to changes in carbon export forced by anthropogenic climate warmin”
BackgroundDetoxification of sulphidic African shelf waters by blooming chemolithotrophs
Lavik, G., Stührmann, T., Brüchert, V., van der Plas, A. K., Mohrholz, V., Lam, P., Mußmann, M., Fuchs, B. M., Amann, R., Lass, U., et al. (2008) · Nature · doi:10.1038/nature07588 · Cited by 329
Environmental control of open‐ocean phytoplankton groups: Now and in the future
Boyd, P., Strzepek, R., Fu, F.-X., & Hutchins, D. A. (2010) · Limnology and Oceanography · doi:10.4319/lo.2010.55.3.1353 · Cited by 323
“This trend is, however, reversed for CO2, which is projected to increase with climate change toward concentrations that are now more typical of the winter season (Sarmiento et al. 1998).”
BackgroundMethodInfluentialFarrera, I., Harrison, S. P., Prentice, I. C., Ramstein, G., Joel Guiot, B., Bartlein, P. J., Bonnefille, R., Bush, M. B., Crämer, W., von Grafenstein, U., et al. (1999) · Climate Dynamics · doi:10.1007/s003820050317 · Cited by 327
“The need to understand the processes which bring about major state changes in the Earth's climate is made clear by atmosphere-ocean model simulations showing that there are complex transient e!ects in the response of climate to anthropogenic changes in greenhouse gas budgets (Rahmstorf 1994; Stocker and Schmitter 1997…”
BackgroundGruber, N. (2008) · Elsevier eBooks · doi:10.1016/b978-0-12-372522-6.00001-3 · Cited by 362
“For example, nearly all climate projections for the 21st century suggest that oceanic stratification will increase (Sarmiento et al., 1998), primarily as a result of the input of heat into the surface ocean, but in part also by a freshening of the upper ocean.”
Reiner Schlitzer, E. (2002) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(02)00004-8 · Cited by 325
“PII: S 0 9 6 7 - 0 6 4 5 ( 0 2 ) 0 0 0 0 4 - 8 results of Sarmiento et al. (1998, 2000), and Caldeira and Duffy (2000) also show high fluxes of anthropogenic carbon dioxide into the Southern Ocean as a result of physical and biological processes.”
BackgroundGlobal Observing Needs in the Deep Ocean
Levin, L. A., Bett, B. J., Gates, A. R., Heimbach, P., Howe, B. M., Janßen, F., McCurdy, A., Ruhl, H. A., Snelgrove, P. V. R., Stocks, K. I., et al. (2019) · Frontiers in Marine Science · doi:10.3389/fmars.2019.00241 · Cited by 342
The Southern Hemisphere Westerlies in a Warming World: Propping Open the Door to the Deep Ocean
Russell, J. L., Dixon, K. W., Gnanadesikan, A., Stouffer, R. J., & Toggweiler, J. R. (2006) · Journal of Climate · doi:10.1175/jcli3984.1 · Cited by 317
“Increasing ocean stratification has been posited to serve as a positive feedback on global warming by reducing the storage of anthropogenic carbon dioxide and heat by the ocean (Sarmiento et al. 1998; Matear and Hirst 1999; Caldeira and Duffy 2000).”
BackgroundSelf-citationModelling regional responses by marine pelagic ecosystems to global climate change
Boyd, P., & Doney, S. (2002) · Geophysical Research Letters · doi:10.1029/2001gl014130 · Cited by 347
“Experiments using COAM’s provide a method for assessing marine biogeochemical responses to and feedbacks on future climate change [Sarmiento et al., 1998; Joos et al., 1999].”
MethodThe seasonal cycle of phytoplankton biomass and primary productivity in the Ross Sea, Antarctica
Smith, W. O. J., Marra, J. F., Hiscock, M. R., & Barber, R. T. (2000) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(00)00061-8 · Cited by 312
Evidence for greater oxygen decline rates in the coastal ocean than in the open ocean
Gilbert, D., Rabalais, N. N., Díaz, R. J., & Zhang, J. (2010) · Biogeosciences · doi:10.5194/bg-7-2283-2010 · Cited by 306
“A number of biogeochemical models embedded within ocean circulation models (Sarmiento et al., 1998; Matear et al., 2000; Bopp et al., 2002) predicted that as a consequence of global warming, oxygen levels in the ocean will decrease at a rate that is typically three to four times faster than one…”
BackgroundSurface-water iron supplies in the Southern Ocean sustained by deep winter mixing
Tagliabue, A., Sallée, J., Bowie, A. R., Lévy, M., Swart, S., & Boyd, P. W. (2014) · Nature Geoscience · doi:10.1038/ngeo2101 · Cited by 306
ENVIRONMENTAL FACTORS CONTROLLING PHYTOPLANKTON PROCESSES IN THE SOUTHERN OCEAN1
Boyd, P. W. (2002) · Journal of Phycology · doi:10.1046/j.1529-8817.2002.t01-1-01203.x · Cited by 305
“…Nelson et al. 2001) and Indian (modeling, Pondaven et al. 2000) sectors by Nelson et al. (2001). climate variability and change At present, global circulation models predict that climate change will have a marked effect on the South- ern Ocean (Sarmiento et al. 1998, Bopp et al. 2001).”
BackgroundEnhanced CO2 outgassing in the Southern Ocean from a positive phase of the Southern Annular Mode
Lovenduski, N. S., Gruber, N., Doney, S. C., & Lima, I. D. (2007) · Global Biogeochemical Cycles · doi:10.1029/2006gb002900 · Cited by 337
“Processes that regulate the exchange of CO2 between the ocean and atmosphere are likely to change in a future characterized by global warming, leading to positive and negative feedbacks in the global climate system [Sarmiento et al., 1998; Joos et al., 1999; Matear and Hirst, 1999; Plattner et al., 2001; Gruber et al.…”
BackgroundMatear, R. J., & Hirst, A. C. (2003) · Global Biogeochemical Cycles · doi:10.1029/2002gb001997 · Cited by 303
“…(Figure 1c), which is responsible for the reduction and/or shoaling of the oceanic overturning circulation and the reduction of oceanic ventilation evident in many coupled climate models under global warming [Bopp et al., 2002; Matear et al., 2000; Plattner et al., 2001; Sarmiento et al., 1998].”
BackgroundResultInfluentialKeeling, R. F., Graven, H., Welp, L. R., Resplandy, L., Bi, J., Piper, S. C., Sun, Y., Bollenbacher, A. F., & Meijer, H. A. J. (2017) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1619240114 · Cited by 300
“Allowing for increases in marine pump efficiency with time, as might occur due to warming-induced stratification (22), slightly increases the overprediction error (SI Appendix, Table S2, set 4).”
Ridgwell, A., Hargreaves, J. C., Edwards, N. R., Annan, J. D., Lenton, T. M., Marsh, R., Yool, A., & Watson, A. (2007) · Biogeosciences · doi:10.5194/bg-4-87-2007 · Cited by 295
“For instance, anthropogenically-driven increases in atmospheric CO2 are amplified because CO 2 solubility decreases at higher temperature and as a result of thermally (and/or fresh water) induced changes in ocean stratification and transport (Sarmiento et al., 1998; Plattner et al., 2001).”
VAQUER-SUNYER, R., & DUARTE, C. M. (2011) · Global Change Biology · doi:10.1111/j.1365-2486.2010.02343.x · Cited by 288
“, 2007), acting through a multitude of interacting processes, including the role of ocean warming in increasing stratification and reducing ventilation of marine waters (Sarmiento et al., 1998).”
BackgroundLarge scale importance of sea ice biology in the Southern Ocean
Arrigo, K. R., & Thomas, D. N. (2004) · Antarctic Science · doi:10.1017/s0954102004002263 · Cited by 293
“Finally, increased global temperatures over the next century are expected to increase surface stratification in the Southern Ocean (Sarmiento et al. 1998).”
BackgroundCO 2 sensitivity of Southern Ocean phytoplankton
Tortell, P. D., Payne, C. D., Li, Y., Trimborn, S., Rost, B., Smith, W. O. J., Riesselman, C. R., Dunbar, R. B., Sedwick, P. N., & DiTullio, G. R. (2008) · Geophysical Research Letters · doi:10.1029/2007gl032583 · Cited by 306
GFDL's CM2 Global Coupled Climate Models. Part II: The Baseline Ocean Simulation
Gnanadesikan, A., Dixon, K. W., Griffies, S. M., Balaji, V., Barreiro, M., Beesley, J. A., Cooke, W. F., Delworth, T. L., Gerdes, R., Harrison, M., et al. (2006) · Journal of Climate · doi:10.1175/jcli3630.1 · Cited by 283
“Such differences could have major implications for ocean ecosystems, which are very dependent on the rate of vertical exchange (Gnanadesikan et al. 2002) and for the response of the carbon cycle to climate change (Sarmiento et al. 1998).”
BackgroundSelf-citationManning, A. C., & Keeling, R. F. (2006) · Tellus B · doi:10.1111/j.1600-0889.2006.00175.x · Cited by 274
“, 2000) may induce O2 outgassing due to changes in both the solubility and biological pumps (Sarmiento et al., 1998), offsetting the observed atmospheric O2 decrease.”
BackgroundInfluentialNutrient Cycles and Marine Microbes in a CO2-Enriched Ocean
Hutchins, D. A., Mulholland, M. R., & Fu, F. (2009) · Oceanography · doi:10.5670/oceanog.2009.103 · Cited by 278
“Several investigators have predicted large increases in ocean suboxia as a result of future sea surface warming and intensified stratification (Sarmiento et al., 1998; Matear and Hirst, 2003; Gnanadesikan et al., 2007).”
BackgroundWu, T., Li, W., Ji, J., Xin, X., Li, L., Wang, Z., Zhang, Y., Li, J., Zhang, F., Wei, M., et al. (2013) · Journal of Geophysical Research Atmospheres · doi:10.1002/jgrd.50320 · Cited by 266
Polar ocean stratification in a cold climate
Sigman, D. M., Jaccard, S. L., & Haug, G. H. (2004) · Nature · doi:10.1038/nature02357 · Cited by 263
The change in oceanic O 2 inventory associated with recent global warming
Keeling, R. F., & Garcia, H. E. (2002) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.122154899 · Cited by 292
Palacios, S., & Zimmerman, R. (2007) · Marine Ecology Progress Series · doi:10.3354/meps07084 · Cited by 253
“These temperature changes will affect heat sensitive organisms directly and alter ocean currents (Manabe & Stouffer 1994, Sarmiento et al. 1998).”
BackgroundLong-Term Climate Commitments Projected with Climate–Carbon Cycle Models
Plattner, G., Knutti, R., Joos, F., Stocker, T. F., von Bloh, W., Brovkin, V. A., Cameron, D., Driesschaert, E., Dutkiewicz, S., Eby, M., et al. (2008) · Journal of Climate · doi:10.1175/2007jcli1905.1 · Cited by 251
“…in previous studies investigating carbon cycle– climate feedbacks and their effects on atmospheric CO2 or allowable emissions in future scenarios (Sarmiento et al. 1998; Joos et al. 1999; Matear et al. 2000; Joos et al. 2001; Plattner et al. 2001; Friedlingstein et al. 2001; Cox et al. 2000;…”
BackgroundFeng, Y., Hare, C. E., Leblanc, K., Rose, J. M., Zhang, Y., DiTullio, G., Lee, P., Wilhelm, S. W., Rowe, J., Sun, J., et al. (2009) · Marine Ecology Progress Series · doi:10.3354/meps08133 · Cited by 244
“One of the Ecostats was maintained using this system at ambient SST (12°C) and the other was 4°C above ambient temperature, as has been predicted for high latitude ocean regimes by the year 2100 (Sarmiento et al. 1998, 2004).”
MethodToward a mechanistic understanding of the decadal trends in the Southern Ocean carbon sink
Lovenduski, N. S., Gruber, N., & Doney, S. C. (2008) · Global Biogeochemical Cycles · doi:10.1029/2007gb003139 · Cited by 243
“Thus Southern Ocean biology in our model simulation is not compensating to the degree that the climate change simulation of Sarmiento et al. [1998] would have suggested.”
BackgroundThe Role of the Southern Ocean in Uptake and Storage of Anthropogenic Carbon Dioxide
Caldeira, K., & Duffy, P. B. (2000) · Science · doi:10.1126/science.287.5453.620 · Cited by 241
Regulation of atmospheric CO 2 by deep‐sea sediments in an Earth system model
Ridgwell, A., & Hargreaves, J. C. (2007) · Global Biogeochemical Cycles · doi:10.1029/2006gb002764 · Cited by 213
“Associated with the warming-driven stratification of the ocean is a restriction in nutrient supply and thus biological (export) production [Plattner et al., 2001; Sarmiento et al., 1998], with a peak year 2200 reduction of about 16% (Figure 8b).”
BackgroundRegional variability in the vertical flux of particulate organic carbon in the ocean interior
Lutz, M., Dunbar, R., & Caldeira, K. (2002) · Global Biogeochemical Cycles · doi:10.1029/2000gb001383 · Cited by 260
“0886-6236/02/2000GB001383 11 - 1 biological pump in the global carbon cycle and may have a role in determining oceanic sequestration of anthropogenic CO2, especially in the context of changing ocean circulation [Kurz and Maier-Reimer, 1993; Sarmiento et al., 1998; Pahlow and Riebesell, 2000].”
BackgroundBianchi, D., Dunne, J. P. P., Sarmiento, J. L., & Galbraith, E. D. (2012) · Global Biogeochemical Cycles · doi:10.1029/2011gb004209 · Cited by 238
“Our denitrification estimate for the North Atlantic shelf (29 Tg N year!1 for depths shallower than 200 m) is larger than the estimate of 20 Tg N year!1 by Seitzinger and Giblin [1996], derived from the correlation between benthic denitrification and water-sediment oxygen fluxes, but is in line with the model assessme…”
Self-citationKrumins, V., Gehlen, M., Arndt, S., Van Cappellen, P., & Regnier, P. (2013) · Biogeosciences · doi:10.5194/bg-10-371-2013 · Cited by 242
Manifestation, Drivers, and Emergence of Open Ocean Deoxygenation
Levin, L. A. (2018) · Annual Review of Marine Science · doi:10.1146/annurev-marine-121916-063359 · Cited by 283
“Most early climate models projected that future oxygen loss would accompany ocean warming (Sarmiento et al. 1998, Plattner et al. 2001, Bopp et al. 2002).”
Background
Metadata
- Authors
- Sarmiento, J. L., Hughes, T. M. C., Stouffer, R. J., & Manabe, S.
- Affiliations
- Princeton University (US)
- NOAA Geophysical Fluid Dynamics Laboratory (US)
- Corresponding author
- Sarmiento, Jorge L.
- Venue
- Nature
- Published
- 1998-05
- Volume
- 393
- Issue
- 6682
- Pages
- 245-249
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1481779298
- Cited by
- 899
- References
- 26
- Citations by year
- 2026: 10 · 2025: 15 · 2024: 36 · 2023: 22 · 2022: 27 · 2021: 28 · 2020: 26 · 2019: 20 · 2018: 29 · 2017: 36 · 2016: 31 · 2015: 30 · 2014: 31 · 2013: 52 · 2012: 40
- FWCI
- 36.26
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- RePEc: Research Papers in Economics (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Keywords
- ocean carbon cycle, anthropogenic CO2 emissions, ocean carbon sink, Southern Ocean, ocean stratification, surface freshening, ocean circulation, coupled ocean-atmosphere model, climate change, biological carbon pump, carbon flux
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