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Biological and Chemical Response of the Equatorial Pacific Ocean to the 1997-98 El Niño
Open accessAbstract
During the 1997–98 El Niño, the equatorial Pacific Ocean retained 0.7 × 10 15 grams of carbon that normally would have been lost to the atmosphere as carbon dioxide. The surface ocean became impoverished in plant nutrients, and chlorophyll concentrations were the lowest on record. A dramatic recovery occurred in mid-1998, the system became highly productive, analogous to coastal environments, and carbon dioxide flux out of the ocean was again high. The spatial extent of the phytoplankton bloom that followed recovery from El Niño was the largest ever observed for the equatorial Pacific. These chemical and ecological perturbations were linked to changes in the upwelling of nutrient-enriched waters. The description and explanation of these dynamic changes would not have been possible without an observing system that combines biological, chemical, and physical sensors on moorings with remote sensing of chlorophyll.
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“Sea Surface Temperature (SST), SST anomalies, dissolved oxygen concentration, illumination, wind speed, current movements, depth of mixing layer, upwelling and food availability are major factors which are influencing the growth, and convergence zone”
From El Niño Southern Oscillation (ENSO) impact on tuna fisheries in Indian Ocean (2014) · cites this paper as Chavez et al. 1999
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“Cold equatorial waters, which are nutrient and biologically rich (Chavez et al. 1999) are equatorially upwelled, advected north and downward forming sharp fronts across the frontal boundary.”
BackgroundRadenac, M., Dandonneau, Y., & Blanke, B. (2005) · doi:10.1007/s10236-005-0111-5 · Cited by 11
“In May 1997 and during the depletion period, vertical nitrate supply in the central and eastern equatorial Pacific had greatly decreased (Chavez et al. 1999; Radenac et al. 2001; Christian et al. 2002).”
BackgroundReid, P. C., & Edwards, M. (2001) · doi:10.1006/rwos.2001.0267 · Cited by 11
Ahmed, M. M. M., Else, B., Butterworth, B. J., Capelle, D., Guéguen, C., Miller, L., Meilleur, C., & Papakyriakou, T. (2021) · Elementa: Science of the Anthropocene · doi:10.1525/elementa.2020.00130 · Cited by 10
“For instance, the ocean’s biological pump operates more efficiently in coastal shelves relative to the open ocean as a result of high terrestrial inputs and efficient use of nutrients (Gattuso et al., 1998; Chavez et al., 1999).”
BackgroundMcPhaden, M., Lee, T., Fournier, S., & Balmaseda, M. (2020) · Geophysical Monograph Series · doi:10.1002/9781119548164.ch3 · Cited by 10
Self-citationQuirós‐Collazos, L., Calvo, E., Schouten, S., van der Meer, M. T. J., Rodrigo‐Gámiz, M., Pena, L. D., Cacho, I., & Pelejero, C. (2020) · Paleoceanography and Paleoclimatology · doi:10.1029/2019pa003777 · Cited by 15
“Therefore, changes in biogeochemical properties and different nutrient availability can affect the phytoplankton community composition in this region and, thus, its impact on the carbon cycle (Brzezinski et al., 2011; Chavez, 1999; Gómez et al., 2007; Watkins et al., 1998).”
BackgroundNeeman, N., Spotila, J., & O’connor, M. (2015) · Journal of Theoretical Biology · doi:10.1016/j.jtbi.2015.06.023 · Cited by 10
Martínez-Aguilar, T. I., Giraldo, A., & Rodríguez-Rubio, E. (2010) · doi:10.4067/s0718-560x2010000100014 · Cited by 10
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BackgroundLovelock, C., Clegg, E., Hurrey, L., Udy, J., & Moore, K. M. (2008) · doi:10.1016/j.jembe.2008.06.023 · Cited by 10
Numerical Model Approaches to Address Recent Problems on Pelagic Ecosystems
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“In addition to upwelling due to steady wind stress forcing, equatorial waves such as Kelvin waves and Tropical Instability Waves (TIWs) are attracting attention as mechanisms to supply iron to the surface ocean (Foley et al., 1997; Chavez et al., 1999).”
BackgroundBetancur, M. J., & Martínez, I. (2016) · doi:10.25268/bimc.invemar.2003.32.0.262 · Cited by 10
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Controls on new production: the role of iron and physical processes
Aufdenkampe, A., & Murray, J. (2002) · doi:10.1016/s0967-0645(02)00052-8 · Cited by 10
“…paradigm of relative biological stability is giving way to the understanding that a number of physical processes can drive substantial variability in chlorophyll, primary, new and export production (e.g. Barber et al., 1996; Chavez et al., 1999; Dunne et al., 2000; Friedrichs and Hofmann, 2001).”
BackgroundMonitoring the Amazon River plume from satellite observations
Shi, W., & Wang, M. (2024) · GIScience & Remote Sensing · doi:10.1080/15481603.2024.2416725 · Cited by 9
“The processes in river estuary involve many atmospheric, ocean, and river processes, e.g., the wind, ocean current, river discharges, and even global atmosphere-ocean events such as El Niño Southern Oscillation (ENSO).”
Zhang, R.-H., Tian, F., Shi, Q.-D., Wang, X.-J., & Wu, T.-W. (2023) · Science China. Earth Sciences · doi:10.1007/s11430-023-1217-8 · Cited by 9
“Satellite data indicate that TIWs are accompanied with large perturbations not only in physical fields, but also in ocean biogeochemistry (Chavez et al., 1999; Strutton et al., 2001; Legeckis et al., 2004; Gorgues et al., 2005).”
Pacific Equatorial Undercurrent: Mean state, sources, and future changes across models
Stellema, A., Gupta, A. S., Taschetto, A., & Feng, M. (2022) · Frontiers in Climate · doi:10.3389/fclim.2022.933091 · Cited by 9
Huang, C., Liu, Y., Luo, Y., Wang, Y., Liu, X., Zhang, Y., Zhuang, Y., & Tian, Y. (2022) · Remote Sensing · doi:10.3390/rs14153610 · Cited by 6
Maillard, L., Boucharel, J., & Renault, L. (2022) · Journal of Physical Oceanography · doi:10.1175/jpo-d-21-0300.1 · Cited by 21
“…Chelton et al. 2001, Hashizume et al. 2001), subsurface temperature (McPhaden 1996, Flament et al. 1996, Kennan and Flament 2000), and ocean color and related biogeochemical properties as well (Yoder et al. 1994, Chavez et al. 1999, Strutton et al. 2001, Legeckis et al. 2004, Evans et al. 2009).”
BackgroundAsymmetric Response of the Biological Carbon Pump to the ENSO in the South China Sea
Li, H.-L., Zhang, J.-J., Xuan, J.-L., Wu, Z., Ran, L., Wiesner, M., & Chen, J.-F. (2022) · Geophysical Research Letters · doi:10.1029/2021gl095254 · Cited by 9
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“During La Niña these conditions reverse, inducing colder SSTs, enhanced near-surface nutrient supply and a subsequent response of marine life [7-11].”
BackgroundImplementing ecosystem considerations in forage fisheries: San Francisco Bay herring case study
Thayer, J. A., Hazen, E. L., García‐Reyes, M., Szoboszlai, A. I., & Sydeman, W. J. (2020) · Marine Policy · doi:10.1016/j.marpol.2020.103884 · Cited by 12
Marine Dinoflagellate Assemblage in the Galápagos Marine Reserve
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Min, W.-G., Kim, D., Rho, H., Chi, S., & Son, S. (2018) · Ocean Science Journal · doi:10.1007/s12601-018-0027-x · Cited by 9
“A dramatic recovery occurred in mid-1998, the system became highly productive, analogous to coastal environments, and carbon dioxide flux out of the ocean was again high (Chavez et al. 1999).”
BackgroundInfluentialOut-of-band effects of satellite ocean color sensors.
Wang, M., Naik, P., & Son, S. (2016) · Applied Optics · doi:10.1364/ao.55.002312 · Cited by 9
Li, Y.-C., & Xu, Y.-F. (2013) · Acta Oceanologica Sinica · doi:10.1007/s13131-013-0291-7 · Cited by 9
Prey Abundance And Population Dynamics Of South American Fur Seals (Arctocephalus Australis) In Peru
Cárdenas-Alayza, S. (2012) · doi:10.14288/1.0072800 · Cited by 9
“El Niño events are widely recognized to reduce the abundance and availability of prey and cause the starvation of South American fur seals (Apaza et al. 1998, Barber & Chavez 1983, Chavez et al. 1999, Majluf 1991a, Glynn 1988).”
BackgroundInfluentialSeasonal productivity of the equatorial Atlantic shaped by distinct wind-driven processes
Brandt, P. N., Körner, M., Moum, J. N., Roch, M., Subramaniam, A., Czeschel, R., Krahmann, G., Dengler, M., & Kiko, R. (2025) · Nature Geoscience · doi:10.1038/s41561-024-01609-9 · Cited by 15
Wilson, K. M., McCool, W. C., & Coltrain, J. B. (2023) · Quaternary International · doi:10.1016/j.quaint.2023.07.002 · Cited by 8
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“For example, events such as the 1997–1998 and 2015–2016 El Niño drove a strong chl decrease in the central and eastern Pacific and positive trends in the western Pacific (Chavez et al., 1999; Mélin et al., 2017).”
BackgroundSelf-citationKrasnopolsky, V., Nadiga, S., Mehra, A., & Bayler, E. (2018) · Applied Computational Intelligence and Soft Computing · doi:10.1155/2018/7057363 · Cited by 8
The Las Salinas palaeo-lagoon in the Sechura Desert (Peru): Evolution during the last two millennia
Christol, A., Wuscher, P., Goepfert, N., Mogollón, V., Béarez, P., Gutiérrez, B., & Carré, M. (2017) · doi:10.1177/0959683616646182 · Cited by 8
“The largest El Niño–related anomalies of sea surface temperature and rainfall were observed in this area (Caviedez, 1984; Chavez et al., 1999).”
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“The sea surface temperature (SST), Chl-a, NPP, and fishery yields are strongly influenced by interannual events, such as those caused by the El Nin ˜o-Southern Oscillation (ENSO) in the Pacific Ocean, because this phenomenon causes a multitude of changes in oceanic and atmospheric conditions and consequently causes st…”
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Salihoğlu, B., & Hofmann, E. (2007) · doi:10.1357/no_doi · Cited by 8
“It is the largest region of oceanic upwelling and the high carbon content of upwelled waters makes this region the largest natural source of CO 2 to the atmosphere (Takahashi et al. , 1997; Chavez et al. , 1999).”
InfluentialPhysical control on the seasonal cycle of surface pCO2 in the equatorial Pacific
Jiang, M., & Chai, F. (2006) · doi:10.1029/2006gl027195 · Cited by 8
Introduction to special section on North Pacific Carbon Cycle Variability and Climate Change
Sabine, C., & Gruber, N. (2006) · doi:10.1029/2006jc003532 · Cited by 8
“The tropical Pacific outgassing is well known to respond very sensitively to climatic fluctuations, particularly the El Nin˜o–Southern Oscillation (ENSO) [ Chavez et al., 1999; Feely et al., 1994, 1995, 1997, 1999, 2002, 2004], with the outgassing nearly vanishing during a fully developed El Nin˜o.”
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Mogollón, R. (2020) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2019.103240 · Cited by 8
Ocean’s largest chlorophyll-rich tongue is extending westward (2002–2022)
Peng, S., Yu, X.-L., Lee, Z.-P., Lin, H., Liu, X., Dai, M.-H., & Shang, S. (2025) · Nature Communications · doi:10.1038/s41467-024-55650-8 · Cited by 7
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“…for the study area, BoB and high concentrations of chlorophyll are mostly associated with cool waters (low SST) of ocean, mainly induced from upwelling (Abbott & Zion, 1985; Chavez et al., 1999), and they are the indicators of the fish populations (Carpenter et al., 1985; Sissenwine, 1984).”
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“Probably as a consequence of the weak El Niño, apart from temperature, most of the other observed water parameters were comparable to CoI, and did not resemble the extremes recorded during strong El Niño or La Niña events (Chavez et al., 1999; Palacios, 2004; Liu et al., 2014).”
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“Consequently, during an El Nino period PP in the tropical Pacific is reduced whereas at a La Nina situation it is enhanced (Behrenfeld et10 al., 2001; Chavez et al., 1999).”
BackgroundOn the Variability of Equatorial Pacific Nitrate and Iron Utilization
Rafter, P. (2024) · Oceanography · doi:10.5670/oceanog.2024.411 · Cited by 7
“The tropical Pacific is an excellent natu-ral laboratory for investigating the temporal variability of nitrate and iron utilization (Chavez et al., 1999; Murray et al., 1994; Strutton et al., 2008, 2011) because of its long history of biogeo-chemical research (e.g., the JGOFS and EB04 cruises;…”
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Toward an integrated pantropical ocean observing system
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“The TEP is recognized as an iron-limited region 13,31,32 , with chlorophyll exhibiting greater sensitivity to iron than nitrate (Extended Data Fig.”
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“…largely differ in genesis and development (Dewitte & Takahashi, 2017; Mogollón, 2019), emphasizing the increasing complexity of El Niño manifestations observed in this productive EBUS (Aguilera et al., 2019; Chavez et al., 1999; Escribano et al., 2004; Silva et al., 2009; Torres et al., 2003).”
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“The prolonged 1998‐2001 LN event had exceptionally strong SST anomalies and was reported as an event that triggered significant phytoplankton blooms along the equatorial Pacific (Chavez et al., 1999; Martin et al., 1994; Messié & Radenac, 2006; Murtugudde et al., 1999; Ryan et al., 2002, 2006).”
BackgroundBallesteros-Prada, A. (2018) · Advances in South American Micropaleontology · doi:10.1007/978-3-030-02119-1_9 · Cited by 6
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Self-citationTHE EFFECTS OF CLIMATE CHANGE ON GLOBAL WILDLIFE AND TERRESTRIAL ECOSYSTEMS
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Progress in multidisciplinary sensing of the 4-dimensional ocean
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“Within the past two decades, optical and chemical systems have been deployed from some of the moorings in this array to significant advantage for atmospheric and oceanographic research and predictions (e.g., Foley et al., 1997; Chavez et al., 1999; Chris Sabine pers. comm.).”
BackgroundMioni, C. E., Pakulski, J., Poorvin, L., Baldwin, A., Twiss, M., Jeffrey, W., & Wilhelm, S. (2007) · Aquatic Microbial Ecology · doi:10.3354/ame046239 · Cited by 6
“…an area of interest because this highly productive region supports one of the world’s largest industrial fisheries (Thorpe et al. 2000) and is periodically affected by the El NiñoSouthern Oscillation (ENSO) event, which causes a breakdown of these fisheries (Lehody et al. 1997, Chavez et al. 1999).”
BackgroundHartshorn, G., & Bynum, N. (1999) · Science · doi:10.1126/science.286.5447.2093 · Cited by 6
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“5 Pg (1015 g) of carbon as C 0 2 to the atmosphere (Chavez et al., 1999).”
BackgroundInfluentialStrengthening of the Equatorial Pacific Upper‐Ocean Circulation Over the Past Three Decades
Tuchen, F. P., Perez, R., Foltz, G., McPhaden, M., & Lumpkin, R. (2024) · Journal of Geophysical Research - Oceans · doi:10.1029/2024jc021343 · Cited by 5
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“A scanty work on chemodiversity and biological potential of T. falconeri has been reported in literature, however, other Tanacetum plants are rich in terpenes mostly as essential oils [7–13], sterols [14–16], phenolic acids and flavonoids [17].”
BackgroundSuetin, V. S., & Korolev, S. (2018) · Physical Oceanography · doi:10.22449/1573-160x-2018-4-330-340 · Cited by 5
The 1997–1998 El Niño event recorded by a stalagmite from central China
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Biogeochemistry: Ocean hotspots of nitrogen loss
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“Our study coincided with a relatively strong El Niño event that began in 1997 and continued through the spring of 1998 (Chavez et al. 1999).”
BackgroundResultModulation of Equatorial Currents and Tropical Instability Waves During the 2021 Atlantic Niño
Tuchen, F. P., Perez, R. C., Foltz, G. R., Brandt, P. N., Subramaniam, A., Lee, S., Lumpkin, R., & Hummels, R. (2023) · Journal of Geophysical Research Oceans · doi:10.1029/2023jc020431 · Cited by 10
Variability of pCO2 and FCO2 in the Mexican Pacific during 25 years
Aurora, C.-Á. L. D. L., Martin, H., Antonio, D., Reginaldo, D., Leticia, E.-C. T., Orión, N.-L., Ramón, S.-Á., & Cecilia, C.-B. (2022) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2022.103853 · Cited by 4
The Particulate Organic Carbon-to-Nitrogen Ratio Varies With Ocean Currents
Xiao, S.-J., Zhang, L., Teng, Y., Huang, T., & Luo, W. (2021) · Frontiers in Environmental Science · doi:10.3389/fenvs.2021.757471 · Cited by 4
“As for the North Pacific Current, the increased ratio is probably because of the missing water from the Equatorial Countercurrent which leans toward north and is influenced by the El Nino phenomenon (Chavez et al., 1999).”
BackgroundTamayo-Millán, C., Ahumada-Sempoal, M., Cortés-Gómez, A. A., Leroux, I. M. C.-R., Bermúdez-Díaz, D., & Islas-Villanueva, V. (2021) · Ciencias Marinas · doi:10.7773/cm.v47i3.3184 · Cited by 4
“2014), lo cual lleva a una disminución en la productividad primaria y, consecuentemente, en el número de peces (Chavez et al. 1999).”
BackgroundGallego, M. A. A., Carmona, J. C. H., Payán, L. F., & Giraldo, A. (2020) · Revista de Biología Tropical · doi:10.15517/rbt.v68i2.38642 · Cited by 4
Tindle, R., Tindle, L., Vagenas, D., & Harris, M. (2013) · Marine Ornithology · doi:10.5038/2074-1235.41.2.1027 · Cited by 4
Systematic ENSO‐driven nutrient variability recorded by central equatorial Pacific corals
LaVigne, M., Nurhati, I. S., Cobb, K. M., McGregor, H. V., Sinclair, D. J., & Sherrell, R. M. (2013) · Geophysical Research Letters · doi:10.1002/grl.50765 · Cited by 4
Salihoğlu, B. (2009) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2008.12.004 · Cited by 4
“The vertical distribution of the velocity and temperature measurements is sufficient to resolve variations in the upper water column environmental structure caused by highfrequency events, such as Tropical Instability Waves (TIWs) and Internal Gravity Waves (IGWs), and low frequency events such as ENSO.”
BackgroundInfluentialSuryan, R., Saba, V. S., Wallace, B. P., Hatch, S. A., Frederiksen, M., & Wanless, S. (2009) · doi:10.1016/j.pocean.2009.04.012 · Cited by 4
“Within a region, food-web structure can also respond to climate oscillations as demonstrated in the Eastern Pacific during ENSO events and multi-decadal regime shifts ( Chavez et al., 1999, 2003 ).”
BackgroundFlores-Coto, C., Zavala-García, F., Funes-Rodríguez, R., Espinosa-Fuentes, M. D. L. L., & Zavala-Hidalgo, J. (2008) · doi:10.4067/s0718-19572008000100009 · Cited by 4
“This phenomenon is called El Niño (Philander 1990, Chavez et al. 1999, Schwing et al. 2002), and this event together with the Southern Oscillation is called ENSO.”
BackgroundSensitivity of equatorial Pacific Ocean circulation to solar radiation absorbed by phytoplankton
Ueyoshi, K., Frouin, R., Nakamoto, S., & Subrahmanyam, B. (2005) · SPIE Optics + Photonics · doi:10.1117/12.621424 · Cited by 4
Scales of Biological–Physical Coupling in the Equatorial Pacific
Strutton, P., & Chavez, F. (2003) · doi:10.1201/9780203489550.ch4 · Cited by 4
“This phenomenon has been described for thermocline variability induced by Kelvin waves [Chavez et al., 1998; Dunne et al., 2000], tropical instability waves [Foley et al., 1997; Strutton et al., 2001] and the El Nino / La Nina cycle [Ryan et al., 2002; Chavez et al., 1999; Strutton and Chavez, 2000; Wilson and Adamec,…”
BackgroundInfluentialSelf-citationChu, S. P., & Elliott, S. (2001) · Journal of Atmospheric Chemistry · doi:10.1023/a:1012221731503 · Cited by 4
Emerging Applications of Longstanding Autonomous Ocean Carbon Observations
Sutton, A. J., & Sabine, C. (2023) · Oceanography · doi:10.5670/oceanog.2023.209 · Cited by 4
“Advancements in buoy-based ocean carbon technology were already leveraging the Tropical Atmosphere Ocean (TAO) array by deploying and testing new autonomous CO 2 sensors (Friederich et al., 1995; Chavez et al., 1999).”
BackgroundShih, C.-L., Chen, Y.-H., & Hsu, C.-C. (2014) · Terrestrial Atmospheric and Oceanic Sciences · doi:10.3319/tao.2014.01.27.01(oc · Cited by 6
Hua, Z.-J., Yang, X.-M., Li, M., Feng, S., & Zhu, J.-F. (2025) · Fishes · doi:10.3390/fishes10080417 · Cited by 3
Estimating Primary Production in the California Current System Using Machine Learning Methods
Ye, Z., Jiang, L., Wang, Q., Li, Q., Wang, L., Gao, S., & Jiang, Z. (2025) · Estuarine, Coastal and Shelf Science · doi:10.1016/j.ecss.2025.109243 · Cited by 3
Scale‐Dependent Drivers of Air‐Sea CO2 Flux Variability
Fay, A. R., Carroll, D., McKinley, G., Menemenlis, D., & Zhang, H. (2024) · Geophysical Research Letters · doi:10.1029/2024gl111911 · Cited by 3
“…of CO 2 outgassing (ocean‐ to‐atmosphere) and during El Niño events, less CO 2 is outgassed as equatorial upwelling of carbon‐rich waters and biological uptake is reduced (Chavez et al., 1999; McKinley et al., 2017) — these bio‐physical dynamics are captured by ECCO‐Darwin (Carroll et al., 2022).”
Thayer, J., Burr, Z., Field, J., Carle, R., & Warzybok, P. (2021) · Fisheries Research · doi:10.1016/j.fishres.2020.105801 · Cited by 3
Kim, H.-C., Nadiga, S., Son, S., Mehra, A., Garraffo, Z., Bayler, E., & Behringer, D. (2018) · doi:10.1080/15481603.2017.1417697 · Cited by 3
“There have been scientific efforts to investigate ocean-biology-induced effects on ocean physics (Lewis et al. 1990; Chavez et al. 1998, 1999; Strutton and Chavez 2004; Manizza et al. 2005; Sweeney et al. 2005; Zhang 2015).”
BackgroundPark, H., Moon, B., Wie, J., Kim, K.-Y., Lee, J., & Byun, Y. (2017) · doi:10.5467/jkess.2017.38.7.469 · Cited by 3
“The model reasonably reproduces the observed chlorophyll patterns with low concentrations at subtropical gyres and high concentrations in the tropical oceans, which are related to inactive subtropical vertical mixing and strong equatorial upwelling, respectively (Chavez et al., 1999).”
BackgroundThe distribution of chlorophyll a in the eastern equatorial Pacific Ocean in boreal autumn
Hong, L.-C., Zhou, Y.-D., Zhang, D., Du, M.-M., Wang, Y., & Wang, C. (2014) · doi:10.1016/j.chnaes.2014.03.004 · Cited by 3
Boyd, P. W. (2009) · Geophysical monograph · doi:10.1029/2008gm000775 · Cited by 5
Organismal biology joins climate research: the example of ENSO
Thatje, S. (2008) · Helgoland Marine Research · doi:10.1007/s10152-007-0098-z · Cited by 3
“Some of the best data available on the impact of EN resulted from the EN 1982–83 (Barber and Chavez 1983; Arntz and Fahrbach 1991; Chavez et al. 1999; Tarazona et al. 2001).”
BackgroundExploration of Biogeochemical Temporal Variability
Dickey, T. (2004) · doi:10.1007/978-1-4020-2087-2_5 · Cited by 3
Climate-driven population size fluctuations of jellyfish (Chrysaora plocamia) off Peru
Quiñones, J., Mianzan, H., Purca, S., Robinson, K., Adams, G., & Acha, E. M. (2015) · Marine Biology · doi:10.1007/s00227-015-2751-4 · Cited by 2
Yang, J., Wen, Y., Chen, P., Zhang, Z.-H., & Pan, D.-L. (2026) · Isprs Journal of Photogrammetry and Remote Sensing · doi:10.1016/j.isprsjprs.2026.01.002 · Cited by 2
Bedolla-Guzmán, Y. R., Masello, J. F., Aguirre‐Muñoz, A., Rojas-Mayoral, E., Olvera-Guerrero, G., Villasante-Barahona, M., & Quillfeldt, P. (2025) · Marine Biology · doi:10.1007/s00227-025-04747-9 · Cited by 1
“…phenomena such as the El Niño Southern Oscillation (ENSO), characterized by warmer ocean temperatures and a deeper thermocline, disrupt normal upwelling patterns, reducing nutrient availability and productivity in the food web (Barber and Chavez 1983 ; Chavez et al. 1999; McPhaden et al. 2020).”
Oliva-Méndez, N. L., Hernández-Ayón, J., Valencia-Gasti, J. A., Durazo, R., Santamaría-del-Ángel, E., Alin, S., & Feely, R. (2025) · Journal of Geophysical Research - Oceans · doi:10.1029/2024jc021653 · Cited by 2
Self-citationChu, W. U., Mazloff, M., Verdy, A., Purkey, S., & Cornuelle, B. (2024) · Limnology and Oceanography: Methods · doi:10.1002/lom3.10641 · Cited by 2
“The tropical Paci fi c Ocean is an especially critical location to constrain carbon dioxide measurements because it is one of the largest sources of regional CO 2 outgassing (Chavez et al. 1999).”
Zhang, T.-J., Xin, J., Song, L.-M., & Yuan, H.-C. (2024) · Fisheries Management and Ecology · doi:10.1111/fme.12711 · Cited by 2
Metadata
- Authors
- Chavez, F. P., Strutton, P. G., Friederich, G. E., Feely, R. A., Feldman, G. C., Foley, D. G., & McPhaden, M. J.
- Affiliations
- Monterey Bay Aquarium Research Institute, 7700 Sandholdt Road, Moss Landing, CA 95039, USA..
- Monterey Bay Aquarium Research Institute (US)
- National Oceanic and Atmospheric Administration (US)
- Goddard Space Flight Center (US)
- NOAA National Marine Fisheries Service (US)
- Venue
- Science
- Published
- 1999-12-10
- Volume
- 286
- Issue
- 5447
- Pages
- 2126-2131
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W1980051345
- Cited by
- 642
- References
- 41
- Citations by year
- 2026: 18 · 2025: 21 · 2024: 15 · 2023: 24 · 2022: 15 · 2021: 13 · 2020: 19 · 2019: 20 · 2018: 21 · 2017: 23 · 2016: 19 · 2015: 15 · 2014: 35 · 2013: 29 · 2012: 25
- FWCI
- 23.27
- Type
- journal article
- Language
- en
- Open access
- green
- figshare.com
- Licence
- cc-by
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- Figshare (submittedVersion, cc-by)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Keywords
- 1997-1998 El Niño, equatorial Pacific, ocean carbon uptake, phytoplankton blooms, chlorophyll content, nutrient depletion, upwelling, ocean productivity, ocean observing systems
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