Decadal oxygen change in the eastern tropical North Atlantic.
Open accessPublished version of a preprint
Abstract
Abstract. Repeat shipboard and multi-year moored observations obtained in the oxygen minimum zone (OMZ) of the eastern tropical North Atlantic (ETNA) were used to study the decadal change in oxygen for the period 2006–2015. Along 23° W between 6 and 14° N, oxygen decreased with a rate of −5.9 ± 3.5 µmol kg−1 decade−1 within the depth covering the deep oxycline (200–400 m), while below the OMZ core (400–1000 m) oxygen increased by 4.0 ± 1.6 µmol kg−1 decade−1 on average. The inclusion of these decadal oxygen trends in the recently estimated oxygen budget for the ETNA OMZ suggests a weakened ventilation of the upper 400 m, whereas the ventilation strengthened homogeneously below 400 m. The changed ventilation resulted in a shoaling of the ETNA OMZ of −0.03 ± 0.02 kg m−3 decade−1 in density space, which was only partly compensated by a deepening of isopycnal surfaces, thus pointing to a shoaling of the OMZ in depth space as well (−22 ± 17 m decade−1). Based on the improved oxygen budget, possible causes for the changed ventilation are analyzed and discussed. Largely ruling out other ventilation processes, the zonal advective oxygen supply stands out as the most probable budget term responsible for the decadal oxygen changes.
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Oxygen changes in the tropical North Atlantic during the past decade are most likely associated with changes in the eddy-driven zonal current bands at intermediate depths and a shoaling of the wind-driven thermocline circulation, but other processes may contribute.
“Oxygen changes in the tropical North Atlantic during the past decade are most likely associated with changes in the eddy-driven zonal current bands at intermediate depths and a shoaling of the wind-driven thermocline circulation, but other processes, such as variations in the intensity of the mesoscale eddy field, may contribute (Hahn et al., 2017).”
From The tropical atlantic observing system (2019) · cites this paper as Hahn et al., 2017
Based on oxygen observations from repeat ship sections in the OMZ of the eastern tropical North Atlantic for the recent decade (2006-2015), Hahn et al. (2017) suggested the existence of strong oxygen variations over this decade superimposed on the multi-decadal deoxygenation pattern.
“Based on oxygen observations from repeat ship sections in the OMZ of the eastern tropical North Atlantic for the recent decade (2006)(2007)(2008)(2009)(2010)(2011)(2012)(2013)(2014)(2015), Hahn et al. (2017) suggested the existence of strong oxygen variations over this decade that are superimposed on the multi-decadal deoxygenation pattern (Stramma et al., 2009;Brandt et al., 2015;Santos et al., 2”
From The tropical atlantic observing system (2019) · cites this paper as Hahn et al., 2017
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Cites
Decline in global oceanic oxygen content during the past five decades
Schmidtko, S., Stramma, L., & Visbeck, M. (2017) · Nature · doi:10.1038/nature21399 · Cited by 1,398 · see citing works
Self-citationOxygen minimum zones in the eastern tropical Atlantic and Pacific oceans
Karstensen, J., Stramma, L., & Visbeck, M. (2008) · Progress in Oceanography · doi:10.1016/j.pocean.2007.05.009 · Cited by 666 · see citing works
Simple climatic indices for the tropical Atlantic Ocean and some applications
Servain, J. (1991) · Journal of Geophysical Research: Oceans · doi:10.1029/91jc01046 · Cited by 345 · cited 1× · see citing works
“Servain (1991) introduced the AZM as the equatorial sea surface temperature (SST) anomaly and defined the AMM as the anomalous inter-hemispheric SST gradient with negative AMM corresponding to a negative/positive SST anomaly in the Northern/Southern Hemisphere.”
Brandt, P., Bange, H. W., Banyte, D., Dengler, M., Didwischus, S.-H., Fischer, T., Greatbatch, R. J., Hahn, J., Kanzow, T., Karstensen, J., et al. (2015) · Biogeosciences · doi:10.5194/bg-12-489-2015 · Cited by 180 · see citing works
Self-citationOceanic link between abrupt changes in the North Atlantic ocean and the African monsoon.
Chang, P., Zhang, R., Hazeleger, W., Wen, C., Wan, X., Ji, L., Haarsma, R. J., Breugem, W.-P., & Seidel, H. (2008) · Nature Geoscience · doi:10.1038/ngeo218 · Cited by 162 · see citing works
The shallow and deep western boundary circulation of the South Atlantic at 5°-11°S.
Schott, F. A., Dengler, M., Zantopp, R., Stramma, L., Fischer, J., & Brandt, P. (2005) · Journal of Physical Oceanography · doi:10.1175/jpo2813.1 · Cited by 125 · see citing works
Self-citationOpen ocean dead zones in the tropical North Atlantic Ocean.
Karstensen, J., Fiedler, B., Schütte, F., Brandt, P., Körtzinger, A., Fischer, G., Zantopp, R., Hahn, J., Visbeck, M., & Wallace, D. (2015) · Biogeosciences · doi:10.5194/bg-12-2597-2015 · Cited by 105 · see citing works
Self-citationChanges in the ventilation of the oxygen minimum zone of the tropical North Atlantic.
Brandt, P., Hormann, V., Körtzinger, A., Visbeck, M., Krahmann, G., Stramma, L., Lumpkin, R., & Schmid, C. (2010) · Journal of Physical Oceanography · doi:10.1175/2010jpo4301.1 · Cited by 89 · see citing works
Self-citationHahn, J., Brandt, P., Greatbatch, R. J., Krahmann, G., & Körtzinger, A. (2014) · Climate Dynamics · doi:10.1007/s00382-014-2065-0 · Cited by 48 · see citing works
Self-citationZonal structure and seasonal variability of the Atlantic equatorial undercurrent.
Johns, W. E., Brandt, P., Bourlès, B., Tantet, A., Papapostolou, A., & Houk, A. (2014) · Climate Dynamics · doi:10.1007/s00382-014-2136-2 · Cited by 48 · see citing works
Self-citation
Flagged first, then by citations
Research works printed but not linked: 65
- Argo: Argo float data and metadata from Global Data Assembly Centre (Argo GDAC), SEANOE, 2000, available at: http://doi. org/10.17882/42182, last access: March 2016. · DOI
- Ascani, F., Firing, E., Dutrieux, P., McCreary, J. P., and Ishida, A.: Deep Equatorial Ocean Circulation Induced by a Forced- Dissipated Yanai Beam, J. Phys. Oceanogr., 40, 1118-1142, https://doi.org/10.1175/2010jpo4356.1, 2010. · DOI
- Ascani, F., Firing, E., McCreary, J. P., Brandt, P., and Great- batch, R. J.: The Deep Equatorial Ocean Circulation in Wind- Forced Numerical Solutions, J. Phys. Oceanogr., 45, 1709-1734, https://doi.org/10.1175/jpo-d-14-0171.1, 2015. · DOI
- Banyte, D., Tanhua, T., Visbeck, M., Wallace, D. W. R., Karstensen, J., Krahmann, G., Schneider, A., Stramma, L., and Dengler, M.: Diapycnal diffusivity at the upper boundary of the tropical North Atlantic oxygen minimum zone, J. Geophys. Res.-Ocean., 117, C09016, https://doi.org/10.1029/2011jc007762, 2012. · DOI
- Biastoch, A., Böning, C. W., Schwarzkopf, F. U., and Lutje- harms, J. R. E.: Increase in Agulhas leakage due to poleward shift of Southern Hemisphere westerlies, Nature, 462, 495-498, https://doi.org/10.1038/nature08519, 2009. · DOI
- Bopp, L., Le Quéré, C., Heimann, M., Manning, A. C., and Mon- fray, P.: Climate-induced oceanic oxygen fluxes: Implications for the contemporary carbon budget, Global Biogeochem. Cy., 16, 6-1-6-13, https://doi.org/10.1029/2001gb001445, 2002. · DOI
- Brandt, P., Hormann, V., Bourlès, B., Fischer, J., Schott, F. A., Stramma, L., and Dengler, M.: Oxygen tongues and zonal cur- rents in the equatorial Atlantic, J. Geophys. Res.-Ocean., 113, C04012, https://doi.org/10.1029/2007jc004435, 2008. · DOI
- Brandt, P., Greatbatch, R. J., Claus, M., Didwischus, S. H., Hor- mann, V., Funk, A., Hahn, J., Krahmann, G., Fischer, J., and Körtzinger, A.: Ventilation of the equatorial Atlantic by the equatorial deep jets, J. Geophys. Res.-Ocean., 117, C12015, https://doi.org/10.1029/2012jc008118, 2012. · DOI · Paper page
- Bunge, L., Provost, C., Hua, B. L., and Kartavtseff, A.: Variabil- ity at intermediate depths at the equator in the Atlantic ocean in 2000-06: Annual cycle, equatorial deep jets, and intraseasonal meridional velocity fluctuations, J. Phys. Oceanogr., 38, 1794- 1806, https://doi.org/10.1175/2008jpo3781.1, 2008. · DOI
- Cabre, A., Marinov, I., Bernardello, R., and Bianchi, D.: Oxy- gen minimum zones in the tropical Pacific across CMIP5 mod- els: mean state differences and climate change trends, Biogeo- sciences, 12, 5429-5454, https://doi.org/10.5194/bg-12-5429- 2015, 2015. · DOI
- Chang, P., Yamagata, T., Schopf, P., Behera, S. K., Carton, J., Kessler, W. S., Meyers, G., Qu, T., Schott, F., Shetye, S., and Xie, S. P.: Climate fluctuations of tropical coupled sys- tems -The role of ocean dynamics, J. Clim., 19, 5122-5174, https://doi.org/10.1175/jcli3903.1, 2006. · DOI · Paper page
- Czeschel, R., Stramma, L., and Johnson, G. C.: Oxygen decreases and variability in the eastern equatorial Pacific, J. Geophys. Res.- Ocean., 117, C11019, https://doi.org/10.1029/2012jc008043, 2012. · DOI
- Doi, T., Tozuka, T., and Yamagata, T.: The Atlantic Meridional Mode and Its Coupled Variability with the Guinea Dome, J. Clim., 23, 455-475, https://doi.org/10.1175/2009jcli3198.1, 2010. · DOI
- Duteil, O., Böning, C. W., and Oschlies, A.: Variability in subtropical-tropical cells drives oxygen levels in the trop- ical Pacific Ocean, Geophys. Res. Lett., 41, 8926-8934, https://doi.org/10.1002/2014gl061774, 2014a. · DOI
- Duteil, O., Schwarzkopf, F. U., Böning, C. W., and Oschlies, A.: Major role of the equatorial current system in setting oxy- gen levels in the eastern tropical Atlantic Ocean: A high- resolution model study, Geophys. Res. Lett., 41, 2033-2040, https://doi.org/10.1002/2013gl058888, 2014b. · DOI
- Eden, C. and Dengler, M.: Stacked jets in the deep equato- rial Atlantic Ocean, J. Geophys. Res.-Ocean., 113, C04003, https://doi.org/10.1029/2007jc004298, 2008. · DOI
- Fischer, T., Banyte, D., Brandt, P., Dengler, M., Krahmann, G., Tan- hua, T., and Visbeck, M.: Diapycnal oxygen supply to the trop- ical North Atlantic oxygen minimum zone, Biogeosciences, 10, 5079-5093, https://doi.org/10.5194/bg-10-5079-2013, 2013. · DOI · Paper page
- Foltz, G. R., McPhaden, M. J., and Lumpkin, R.: A Strong Atlantic Meridional Mode Event in 2009: The Role of Mixed Layer Dy- namics, J. Clim., 25, 363-380, https://doi.org/10.1175/jcli-d-11- 00150.1, 2012. · DOI · Paper page
- Frölicher, T. L., Joos, F., Plattner, G. K., Steinacher, M., and Doney, S. C.: Natural variability and anthropogenic trends in oceanic oxygen in a coupled carbon cycle-climate model ensemble, Global Biogeochem. Cy., 23, 15, GB1003, https://doi.org/10.1029/2008gb003316, 2009. · DOI
- Garzoli, S. L. and Katz, E. J.: The Forced Annual Re- versal of the Atlantic North Equatorial Countercurrent, J. Phys. Oceanogr., 13, 2082-2090, https://doi.org/10.1175/1520- 0485(1983)013<2082:tfarot>2.0.co;2, 1983. · DOI
- Garzoli, S. L. and Richardson, P. L.: Low-frequency meandering of the Atlantic North Equatorial Coun- tercurrent, J. Geophys. Res.-Ocean., 94, 2079-2090, https://doi.org/10.1029/JC094iC02p02079, 1989. · DOI
- Helly, J. J. and Levin, L. A.: Global distribution of naturally occur- ring marine hypoxia on continental margins, Deep-Sea Res. Pt. I, 51, 1159-1168, https://doi.org/10.1016/j.dsr.2004.03.009, 2004. · DOI · Paper page
- Helm, K. P., Bindoff, N. L., and Church, J. A.: Observed decreases in oxygen content of the global ocean, Geophys. Res. Lett., 38, L23602, https://doi.org/10.1029/2011gl049513, 2011. · DOI · Paper page
- Hormann, V., Lumpkin, R., and Foltz, G. R.: Interannual North Equatorial Countercurrent variability and its relation to tropical Atlantic climate modes, J. Geophys. Res.-Ocean., 117, C04035, https://doi.org/10.1029/2011jc007697, 2012. · DOI
- Hummels, R., Brandt, P., Dengler, M., Fischer, J., Araujo, M., Veleda, D., and Durgadoo, J. V.: Interannual to decadal changes in the western boundary circulation in the At- lantic at 11 • S, Geophys. Res. Lett., 42, 7615-7622, https://doi.org/10.1002/2015gl065254, 2015. · DOI · Paper page
- Joyce, T. M., Frankignoul, C., Yang, J. Y., and Phillips, H. E.: Ocean response and feedback to the SST dipole in the tropical Atlantic, J. Phys. Oceanogr., 34, 2525-2540, https://doi.org/10.1175/jpo2640.1, 2004. · DOI
- Kamenkovich, I., Berloff, P., and Pedlosky, J.: Anisotropic Mate- rial Transport by Eddies and Eddy-Driven Currents in a Model of the North Atlantic, J. Phys. Oceanogr., 39, 3162-3175, https://doi.org/10.1175/2009jpo4239.1, 2009. · DOI
- Keeling, R. F. and Garcia, H. E.: The change in oceanic O 2 inven- tory associated with recent global warming, P. Natl. Acad. Sci. USA, 99, 7848-7853, https://doi.org/10.1073/pnas.122154899, 2002. · DOI · Paper page
- Kirchner, K., Rhein, M., Hüttl-Kabus, S., and Böning, C. W.: On the spreading of South Atlantic Water into the North- ern Hemisphere, J. Geophys. Res.-Ocean., 114, C05019, https://doi.org/10.1029/2008jc005165, 2009. · DOI
- Köllner, M., Visbeck, M., Tanhua, T., and Fischer, T.: Diapyc- nal diffusivity in the core and oxycline of the tropical North Atlantic oxygen minimum zone, J. Mar. Syst., 160, 54-63, https://doi.org/10.1016/j.jmarsys.2016.03.012, 2016. · DOI
- Kolodziejczyk, N., Reverdin, G., Gaillard, F., and Lazar, A.: Low- frequency thermohaline variability in the Subtropical South At- lantic pycnocline during 2002-2013, Geophys. Res. Lett., 41, 6468-6475, https://doi.org/10.1002/2014gl061160, 2014. · DOI
- Liu, L. L. and Huang, R. X.: The Global Subduction/Obduction Rates: Their Interannual and Decadal Variability, J. Clim., 25, 1096-1115, https://doi.org/10.1175/2011jcli4228.1, 2012. · DOI
- Lübbecke, J. F., Durgadoo, J. V., and Biastoch, A.: Contribution of Increased Agulhas Leakage to Tropical Atlantic Warming, J. Clim., 28, 9697-9706, https://doi.org/10.1175/jcli-d-15-0258.1, 2015. · DOI
- Luyten, J. R., Pedlosky, J., and Stommel, H.: The Ventilated Thermocline, J. Phys. Oceanogr., 13, 292-309, https://doi.org/10.1175/1520- 0485(1983)013<0292:tvt>2.0.co;2, 1983. · DOI
- Marshall, J., Kushner, Y., Battisti, D., Chang, P., Czaja, A., Dickson, R., Hurrell, J., McCartney, M., Saravanan, R., and Visbeck, M.: North Atlantic climate variability: Phenomena, impacts and mechanisms, Int. J. Climatol., 21, 1863-1898, https://doi.org/10.1002/joc.693, 2001. · DOI
- Matear, R. J. and Hirst, A. C.: Long-term changes in dis- solved oxygen concentrations in the ocean caused by pro- tracted global warming, Global Biogeochem. Cy., 17, 1125, https://doi.org/10.1029/2002gb001997, 2003. · DOI
- Maximenko, N. A., Bang, B., and Sasaki, H.: Observational evi- dence of alternating zonal jets in the world ocean, Geophys. Res. Lett., 32, L12607, https://doi.org/10.1029/2005gl022728, 2005. · DOI
- Ollitrault, M. and de Verdiere, A. C.: The Ocean General Circu- lation near 1000-m Depth, J. Phys. Oceanogr., 44, 384-409, https://doi.org/10.1175/jpo-d-13-030.1, 2014. · DOI
- Oschlies, A., Schulz, K. G., Riebesell, U., and Schmittner, A.: Simulated 21st century's increase in oceanic suboxia by CO 2 - enhanced biotic carbon export, Global Biogeochem. Cy., 22, GB4008, https://doi.org/10.1029/2007gb003147, 2008. · DOI
- Pena-Izquierdo, J., van Sebille, E., Pelegri, J. L., Sprintall, J., Ma- son, E., Llanillo, P. J., and Machin, F.: Water mass pathways to the North Atlantic oxygen minimum zone, J. Geophys. Res.- Ocean., 120, 3350-3372, https://doi.org/10.1002/2014jc010557, 2015. · DOI
- Perez, R. C., Lumpkin, R., Johns, W. E., Foltz, G. R., and Hormann, V.: Interannual variations of Atlantic tropi- cal instability waves, J. Geophys. Res.-Ocean., 117, C03011, https://doi.org/10.1029/2011jc007584, 2012. · DOI
- Plattner, G. K., Joos, F., and Stocker, T. F.: Revision of the global carbon budget due to changing air-sea oxy- gen fluxes, Global Biogeochem. Cy., 16, 12, 1096, https://doi.org/10.1029/2001gb001746, 2002. · DOI
- Qiu, B., Chen, S. M., and Sasaki, H.: Generation of the North Equatorial Undercurrent Jets by Triad Baroclinic Rossby Wave Interactions, J. Phys. Oceanogr., 43, 2682-2698, https://doi.org/10.1175/jpo-d-13-099.1, 2013. · DOI
- Rabe, B., Schott, F. A., and Kohl, A.: Mean circulation and variability of the tropical Atlantic during 1952-2001 in the GECCO assimilation fields, J. Phys. Oceanogr., 38, 177-192, https://doi.org/10.1175/2007jpo3541.1, 2008. · DOI
- Rhein, M., Kirchner, K., Mertens, C., Steinfeldt, R., Walter, M., and Fleischmann-Wischnath, U.: Transport of South At- lantic water through the passages south of Guadeloupe and across 16 • N, 2000-2004, Deep-Sea Res. Pt. I, 52, 2234-2249, https://doi.org/10.1016/j.dsr.2005.08.003, 2005. · DOI
- Richardson, P. L., Arnault, S., Garzoli, S., and Bruce, J. G.: Annual cycle of the Atlantic North Equatorial Countercurrent, Deep- Sea Res. Pt. A, 39, 997-1014, https://doi.org/10.1016/0198- 0149(92)90036-s, 1992. · DOI
- Roemmich, D., Johnson, G. C., Riser, S., Davis, R., Gilson, J., Owens, W. B., Garzoli, S. L., Schmid, C., and Ig- naszewski, M.: The Argo Program Observing the Global Ocean with Profiling Floats, Oceanography, 22, 34-43, https://doi.org/10.5670/oceanog.2009.36, 2009. · DOI
- Rosell-Fieschi, M., Pelegri, J. L., and Gourrion, J.: Zonal jets in the equatorial Atlantic Ocean, Prog. Oceanogr., 130, 1-18, https://doi.org/10.1016/j.pocean.2014.08.008, 2015. · DOI
- Schmidtko, S. and Johnson, G. C.: Multidecadal Warming and Shoaling of Antarctic Intermediate Water, J. Clim., 25, 207-221, https://doi.org/10.1175/jcli-d-11-00021.1, 2012. · DOI
- Schmidtko, S., Johnson, G. C., and Lyman, J. M.: MIMOC: A global monthly isopycnal upper-ocean climatology with mixed layers, J. Geophys. Res.-Ocean., 118, 1658-1672, https://doi.org/10.1002/jgrc.20122, 2013. · DOI
- Schmittner, A., Oschlies, A., Matthews, H. D., and Galbraith, E. D.: Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business-as-usual CO 2 emission scenario until year 4000 AD, Global Biogeochem. Cy., 22, GB1013, https://doi.org/10.1029/2007gb002953, 2008. · DOI
- Schott, F. A., Dengler, M., Brandt, P., Affler, K., Fischer, J., Bourlès, B., Gouriou, Y., Molinari, R. L., and Rhein, M.: The zonal cur- rents and transports at 35 • W in the tropical Atlantic, Geophys. Res. Lett., 30, 1349, https://doi.org/10.1029/2002gl016849, 2003. · DOI
- Schütte, F., Karstensen, J., Krahmann, G., Hauss, H., Fiedler, B., Brandt, P., Visbeck, M., and Körtzinger, A.: Characteriza- tion of dead-zone eddies in the eastern tropical North Atlantic, Biogeosciences, 13, 5865-5881, https://doi.org/10.5194/bg-13- 5865-2016, 2016. · DOI
- Stendardo, I. and Gruber, N.: Oxygen trends over five decades in the North Atlantic, J. Geophys. Res.-Ocean., 117, C11004, https://doi.org/10.1029/2012jc007909, 2012. · DOI
- Stramma, L. and Schott, F.: The mean flow field of the trop- ical Atlantic Ocean, Deep-Sea Res. Pt. II, 46, 279-303, https://doi.org/10.1016/s0967-0645(98)00109-x, 1999. · DOI · Paper page
- Stramma, L., Hüttl, S., and Schafstall, J.: Water masses and currents in the upper tropical northeast Atlantic off northwest Africa, J. Geophys. Res.-Ocean., 110, C12006, https://doi.org/10.1029/2005jc002939, 2005. · DOI · Paper page
- Stramma, L., Johnson, G. C., Sprintall, J., and Mohrholz, V.: Ex- panding oxygen-minimum zones in the tropical oceans, Science, 320, 655-658, https://doi.org/10.1126/science.1153847, 2008. · DOI
- Stramma, L., Visbeck, M., Brandt, P., Tanhua, T., and Wallace, D.: Deoxygenation in the oxygen minimum zone of the east- ern tropical North Atlantic, Geophys. Res. Lett., 36, L20607, https://doi.org/10.1029/2009gl039593, 2009. · DOI · Paper page
- Stramma, L., Schmidtko, S., Levin, L. A., and Johnson, G. C.: Ocean oxygen minima expansions and their bi- ological impacts, Deep-Sea Res. Pt. I, 57, 587-595, https://doi.org/10.1016/j.dsr.2010.01.005, 2010. · DOI
- Stramma, L., Oschlies, A., and Schmidtko, S.: Mismatch be- tween observed and modeled trends in dissolved upper-ocean oxygen over the last 50 yr, Biogeosciences, 9, 4045-4057, https://doi.org/10.5194/bg-9-4045-2012, 2012. · DOI
- Thomsen, S., Kanzow, T., Colas, F., Echevin, V., Krahmann, G., and Engel, A.: Do submesoscale frontal processes ventilate the oxygen minimum zone off Peru?, Geophys. Res. Lett., 43, 8133- 8142, https://doi.org/10.1002/2016gl070548, 2016. · DOI
- Wallace, D. W. R. and Bange, H. W.: Introduction to special section: Results of the Meteor 55: Tropical SOLAS expedition, Geophys. Res. Lett., 31, L23S01, https://doi.org/10.1029/2004gl021014, 2004. · DOI
- Wyrtki, K.: The oxygen minima in relation to ocean circula- tion, Deep-Sea Res., 9, 11-23, https://doi.org/10.1016/0011- 7471(62)90243-7, 1962. · DOI
- Zhang, D. X., McPhaden, M. J., and Johns, W. E.: Observational evidence for flow between the subtropical and tropical Atlantic: The Atlantic subtropical cells, J. Phys. Oceanogr., 33, 1783- 1797, https://doi.org/10.1175/2408.1, 2003. · DOI
- Zhu, J. S., Huang, B. H., and Wu, Z. H.: The Role of Ocean Dynamics in the Interaction between the Atlantic Meridional and Equatorial Modes, J. Clim., 25, 3583-3598, https://doi.org/10.1175/jcli-d-11-00364.1, 2012. · DOI
Cited by
Sorted by citations
The tropical atlantic observing system
Foltz, G. R., Brandt, P., Richter, I., Rodríguez-Fonseca, B., Hernandez, F., Dengler, M., Rodrigues, R. R., Schmidt, J. O., Yu, L., Lefevre, N., et al. (2019) · Frontiers in Marine Science · doi:10.3389/fmars.2019.00206 · Cited by 150 · see citing works
Self-citation
- Authors
- Hahn, J., Brandt, P., Schmidtko, S., & Krahmann, G.
- Affiliations
- GEOMAR Helmholtz Centre for Ocean Research Kiel (DE)
- Christian-Albrechts-Universität zu Kiel (DE)
- Corresponding author
- Hahn, Johannes
- Venue
- Ocean Science
- Publisher
- Copernicus GmbH
- Published
- 2017-07-06
- Volume
- 13
- Issue
- 4
- Pages
- 551-576
- ISSN
- 1812-0784 (ISSN-L)
- 1812-0792
- OpenAlex
- W2568513090
- Cited by
- 38
- References
- 10
- Citations by year
- 2026: 2 · 2025: 1 · 2024: 11 · 2023: 2 · 2022: 3 · 2021: 5 · 2020: 2 · 2019: 7 · 2018: 4 · 2017: 1
- FWCI
- 2.55
- Type
- journal article
- Language
- en
- Open access
- gold
- doi.org
- Licence
- Locations
- Ocean science (publishedVersion, cc-by)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
- DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion)
- Funders
- Deutsche Forschungsgemeinschaft
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Biology and Ecology Research
- Keywords
- oxygen minimum zone, eastern tropical North Atlantic, ocean ventilation, oxygen budget, zonal advection, mooring observations
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review