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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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Effects of climate variability on the temporal population dynamics of southern fulmars
Jenouvrier, S., Barbraud, C., & Weimerskirch, H. (2003) · Journal of Animal Ecology · doi:10.1046/j.1365-2656.2003.00727.x · Cited by 207
“1997; Chavez et al .”
Kaplan, I., Levin, P., Burden, M., & Fulton, E. (2010) · Canadian Journal of Fisheries and Aquatic Sciences · doi:10.1139/f10-118 · Cited by 101
“In many ways, these problems have been more vexing than the complicated underlying biological processes such as recruitment (i.e., the production of juveniles), dispersal of lar- vae, and annual or decadal shifts in ocean condition (Chavez et al. 1999; Hare and Mantua 2000; Kinlan and Gaines 2003).”
BackgroundMicrobial community structure and variability in the tropical Pacific
Landry, M., & Kirchman, D. (2002) · doi:10.1016/s0967-0645(02)00053-x · Cited by 101
Skill assessment in ocean biological data assimilation
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“There is also evidence of a shift in phytoplankton species resulting from the lower nutrient condition (Chavez et al., 1999).”
BackgroundOlson, R. J., Duffy, L., Kuhnert, P., Galván‐Magaña, F., Bocanegra-Castillo, N., & Alatorre-Ramírez, V. (2013) · Marine Ecology Progress Series · doi:10.3354/meps10609 · Cited by 93
“The El Niño-Southern Oscillation (ENSO) is a wellknown interannual climate perturbation that affects the physics and biology of the ETP (Barber & Chavez 1983, Chavez et al. 1999).”
BackgroundWallace, B. P., Seminoff, J. A., Kilham, S. S., Spotila, J., & Dutton, P. (2006) · doi:10.1007/s00227-006-0247-y · Cited by 99
Co-limitation of diatoms by iron and silicic acid in the equatorial Pacific
Brzezinski, M., Baines, S., Balch, W., Beucher, C., Chai, F., Dugdale, R., Krause, J., Landry, M., Marchi, A., Measures, C., et al. (2011) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/j.dsr2.2010.08.005 · Cited by 98
“…upwelling associated with tropical instability waves (e.g. Strutton et al., 2001) and possibly during longer term perturbations in upwelling intensity associated with the ENSO cycle (Chavez et al., 1999) or other large-scale shifts in vertical nutrient supply within the EEP (Ryan et al., 2002).”
BackgroundSelf-citationZhai, W., Dai, M., Chen, B., Guo, X., Li, Q., Shang, S., Zhang, C., Cai, W., & Wang, D.-X. (2013) · Biogeosciences · doi:10.5194/bg-10-7775-2013 · Cited by 107
TOP-DOWN HERBIVORY AND BOTTOM-UP EL NIÑO EFFECTS ON GALÁPAGOS ROCKY-SHORE COMMUNITIES
Vinueza, L., Branch, G., Branch, M. L., & Bustamante, R. (2006) · Ecological Monographs · doi:10.1890/04-1957 · Cited by 94
“Detailed studies of nutrient concentrations were independently undertaken at the time of our studies (Chavez et al. 1999), so we did not measure nutrients.”
BackgroundInfluentialDo geochemical estimates of sediment focusing pass the sediment test in the equatorial Pacific
Lyle, M., Mitchell, N., Pisias, N., Mix, A., Martínez, J., & Paytan, A. (2005) · doi:10.1029/2004pa001019 · Cited by 94
“Diffuse latitudinal distribution of productivity is also contrary to the latitudinal restriction in upwelled Fe from the Equatorial Undercurrent, a major factor in equatorial Pacific productivity and new production [Coale et al., 1996; Chavez et al., 1999; Le Bouteiller et al., 2003].”
ResultJellyfish swarms, tourists, and the Christ-child
Dawson, M. N., Martin, L. E., & Penland, L. K. (2001) · Hydrobiologia · doi:10.1023/a:1011868925383 · Cited by 68
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“Chavez et al., 1999; Gonza ´lez, Sobarzo, Figueroa, & Nothig, 2000).”
BackgroundResultInfluentialSeasonal to multiannual marine ecosystem prediction with a global Earth system model
Park, J.-Y., Stock, C., Dunne, J., Yang, X.-S., & Rosati, A. (2019) · Science · doi:10.1126/science.aav6634 · Cited by 91
Radenac, M., Léger, F., Singh, A., & Delcroix, T. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jc007841 · Cited by 94
“…to February months only (not shown) because CP and EP El Niño and La 292 Niña events reach their mature phase in boreal winter for most climate variables [Kao and Yu, 293 2009] and for chlorophyll changes [Chavez et al., 1999; Strutton and Chavez, 2000; Radenac 294 et al., 2001; see also Figure 2].”
BackgroundResultInfluentialThe flip‐side of the North Atlantic Oscillation and modal shifts in slope‐water circulation patterns
Greene, C., & Pershing, A. (2003) · doi:10.4319/lo.2003.48.1.0319 · Cited by 91
“Although overshadowed by the global impacts of the most intense El Nino–Southern Oscillation event on record (Chavez et al. 1999; McPhaden 1999), a large single-year drop in the North Atlantic Oscillation (NAO) index (Hurrell 1995) during 1996 had major regional- and basin-scale impacts for several…”
BackgroundRyan, J., Ueki, I., Chao, Y., Zhang, H., Polito, P., & Chavez, F. (2006) · doi:10.1029/2005jg000084 · Cited by 90
Self-citationUnusual large-scale phytoplankton blooms in the equatorial Pacific
Ryan, J. P., Polito, P. S., Strutton, P. G., & Chávez, F. P. (2002) · Progress In Oceanography · doi:10.1016/s0079-6611(02)00137-4 · Cited by 89
“Physical changes during El Nin ˜ o dramatically reduce euphotic zone nutrient supply and productivity (Fig. 1b) and disrupt food webs across the equatorial and coastal environments of the eastern tropical Pacifi c (Barber & Chavez, 1983, 1986; Fiedler, Philbrick, & Chavez, 1991; Chavez, Strutton, & McPhaden, 1998; Cha…”
BackgroundInfluentialSelf-citationAn introduction to ocean remote sensing
Martin, S. (2004) · doi:10.1017/cbo9781139094368 · Cited by 90
Shi, W., Wang, M., & Jiang, L.-D. (2011) · doi:10.1029/2011jc007234 · Cited by 89
Bricaud, A., Ciotti, Á., & Gentili, B. (2012) · Global Biogeochemical Cycles · doi:10.1029/2010gb003952 · Cited by 88
“The spatial extent of the 1998 bloom was recognized as the largest ever observed for the Equatorial Pacific, with a high abundance of diatoms [Chavez et al., 1999].”
BackgroundPersistent Pelagic Habitats in the Baja California to Bering Sea (B2B) Ecoregion
Etnoyer, P. J., Canny, D., Mate, B. R., & Morgan, L. E. (2004) · Oceanography · doi:10.5670/oceanog.2004.71 · Cited by 86
Biogeography Of Procellariiform Foraging Strategies: Does Ocean Productivity Influence Provisioning?
Baduini, C. L., & Hyrenbach, K. (2003) · Marine Ornithology · doi:10.5038/2074-1235.31.2.570 · Cited by 88
A whirling ecosystem in the equatorial Atlantic
Menkes, C. E., Kennan, S. C., Flament, P., Dandonneau, Y., Masson, S., Biessy, B., Marchal, E., Eldin, G., Grelet, J., Montel, Y., et al. (2002) · Geophysical Research Letters · doi:10.1029/2001gl014576 · Cited by 87
“…distributions of nutrients, CO2, primary productivity, phytoplankton, and zooplankton [Murray et al., 1994; Roman et al., 1995; Foley et al., 1997;Chavez et al., 1999] and, more generally, the equatorial ecosystem just as eddyinduced processes have been invoked to enhance production in other…”
BackgroundBiological response to the 1997–98 and 2009–10 El Niño events in the equatorial Pacific Ocean
Gierach, M., Lee, T., Turk, D., & McPhaden, M. (2012) · doi:10.1029/2012gl051103 · Cited by 86
“Consistent with past studies [Barber and Chavez, 1983; Fiedler et al., 1992; Chavez et al., 1998, 1999; Strutton and Chavez, 2000; Turk et al., 2001, 2011; Radenac et al., 2012], reduced chl-a occurred in the EEP (5 S–5 N, 170 W–90 W) and CEP (5 S–5 N, 160 E–170 W) during the 1997–98 EP-…”
BackgroundResultSelf-citationChanges in water clarity of the Bohai Sea: Observations from MODIS
Shang, S., Lee, Z., Shi, L., Lin, G., Wei, G., & Li, X. (2016) · Remote Sensing of Environment · doi:10.1016/j.rse.2016.08.020 · Cited by 89
“As demonstrated decades ago, repetitive measurements from satellite sensors are the only feasiblemeans to observe and evaluate the temporal variations of geophysical properties of large regions (e.g., Behrenfeld et al., 2001; Chavez et al., 1999; McClain, 2009; Yoder et al., 2002).”
BackgroundInterannual variability of the upper ocean carbon cycle at station ALOHA near Hawaii
Brix, H., Gruber, N., & Keeling, C. D. (2004) · Global Biogeochemical Cycles · doi:10.1029/2004gb002245 · Cited by 84
Enhanced chlorophyll associated with tropical instability waves in the equatorial Pacific
Strutton, P. G., Ryan, J. P., & Chavez, F. P. (2001) · Geophysical Research Letters · doi:10.1029/2000gl012166 · Cited by 83
Self-citationLecher, A., Mackey, K., Kudela, R., Ryan, J., Fisher, A., Murray, J., & Paytan, A. (2015) · Environmental Science and Technology · doi:10.1021/acs.est.5b00909 · Cited by 83
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“The most pronounced SST variability within the wavelet power spectrum is observed during the strongest El Niño phenomena encompassed within this time series, namely the 1982–1983 and 1997–1998 events—the latter of which is the strongest El Niño recorded in the 20th century (Chavez et al., 1999).”
BackgroundThe potential impacts of global climate change on marine protected areas
Soto, C. G. (2004) · Reviews in Fish Biology and Fisheries · doi:10.1023/a:1020364409616 · Cited by 83
“In recent years, studies have examined inter-annual and inter-decadal climate variability and elaborated the complex connections between ocean, atmosphere, climate, and effects on productivity of marine systems (Graham, 1994; Francis et al., 1998; Sugimoto and Tadokoro, 1998; Chavez et al., 1999).”
BackgroundAir–sea carbon dioxide fluxes in the coastal southeastern tropical Pacific
Friederich, G. E., Ledesma, J., Ulloa, O., & Chávez, F. P. (2008) · Progress In Oceanography · doi:10.1016/j.pocean.2008.10.001 · Cited by 95
Self-citationMultiyear predictability of tropical marine productivity
Séférian, R., Bopp, L., Gehlen, M., Swingedouw, D., Mignot, J., Guilyardi, E., & Servonnat, J. (2014) · Proceedings of the National Academy of Sciences of the United States of America · doi:10.1073/pnas.1315855111 · Cited by 81
“These natural fluctuations impact marine ecosystems across large oceanic regions (2).”
BackgroundDetection of imperfect population synchrony in an uncertain world
Cazelles, B., & Stone, L. (2003) · Journal of Animal Ecology · doi:10.1046/j.1365-2656.2003.00763.x · Cited by 81
“Putative effects of El Nino on ecosystems and populations have been extensively studied (see recent reviews, Chavez et al . 1999; Holmgren et al . 2001; Jaksic 2001).”
BackgroundMenge, B. A., Gouhier, T. C., Freidenburg, T. L., & Lubchenco, J. (2011) · Journal of Experimental Marine Biology and Ecology · doi:10.1016/j.jembe.2011.02.003 · Cited by 79
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Natural variability and anthropogenic change in equatorial Pacific surface ocean pCO2 and pH
Sutton, A. J., Feely, R. A., Sabine, C. L., McPhaden, M. J., Takahashi, T., Chávez, F. P., Friederich, G. E., & Mathis, J. T. (2014) · Global Biogeochemical Cycles · doi:10.1002/2013gb004679 · Cited by 93
“During the strong El Niño events of 1982–1983 and 1997–1998, upwelling ceased at the equator along with CO2 outgassing as the partial pressure of CO2 (pCO2) in surface waters reduced to equilibriumwith the atmosphere [Feely et al., 1987; Chavez et al., 1999].”
BackgroundSelf-citationRemotely Sensed Biological Production in the Equatorial Pacific
Turk, D., McPhaden, M., Busalacchi, A., & Lewis, M. (2001) · Science · doi:10.1126/science.1056449 · Cited by 74
Self-citationTropical Pacific Observing System
Smith, N., Kessler, W., Cravatte, S., Sprintall, J., Wijffels, S., Cronin, M., Sutton, A., Serra, Y., Dewitte, B., Strutton, P., et al. (2019) · Frontiers in Marine Science · doi:10.3389/fmars.2019.00031 · Cited by 73
Self-citationOceanic Habits and Habitats: Dermochelys coriacea
Saba, V. (2013) · doi:10.1201/b13895-8 · Cited by 73
Carbon fluxes in the equatorial Pacific: a synthesis of the JGOFS programme
Borgne, R. L., Feely, R. A., & Mackey, D. (2002) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(02)00043-7 · Cited by 73
“The first occurred during the recovery of the equatorial upwelling after the strong 1997– 1998 El Ni * no when the chlorophyll a at 01, 1401W increased by a factor of 3–4 in July–September 1998 (Murtugudde et al., 1999; McClain et al., 2002) and 10 at 21N, 1101W ( Chavez et al., 1999 ).”
BackgroundMethodInfluentialSelf-citationMustapha, Z. B., Alvain, S., Jamet, C., Loisel, H., & Dessailly, D. (2014) · Remote Sensing of Environment · doi:10.1016/j.rse.2013.08.046 · Cited by 72
Climate forcing of the spring bloom in Chesapeake Bay.
Miller, W., & Harding Jr, L. (2007) · Marine Ecology Progress Series · doi:10.3354/meps331011 · Cited by 70
Resplandy, L., Séférian, R., & Bopp, L. (2014) · Journal of Geophysical Research Oceans · doi:10.1002/2014jc010463 · Cited by 72
“The CESM and GFLD models show a strong link between air-sea fluxes variability and ENSO, in agreement with previous results based on models and observations [Keeling et al., 1989; Feely et al., 1999; Chavez et al., 1999; McKinley et al., 2003; Peylin et al., 2005; Fr€olicher et al., 2013].”
Gregg, W. W. (2001) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(01)00095-9 · Cited by 63
“These results conform to observations by Chavez et al. (1999), who noted that in the tropical Pacific, El Ni *no is dominated by pico and nanoplankton, and the La Ni *na brings about the increased relative abundance of diatoms.”
BackgroundResultQuiñones, J., Carman, V. G., Zeballos, J., Purca, S., & Mianzan, H. (2010) · Hydrobiologia · doi:10.1007/s10750-010-0225-8 · Cited by 69
“This upwelling sustains high biological productivity and supports one of the world’s largest single-species fisheries ( Chavez et al., 1999, 2008; Pennington et al., 2006).”
InfluentialGoñi, M., Aceves, H., Thunell, R., Tappa, E., Black, D., Astor, Y., Varela, R., & Muller-Karger, F. (2003) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/s0967-0637(03)00060-8 · Cited by 68
“The 1997–1998 period coincided with an El Niño event (Chavez et al., 1999) and was characterized by significantly lower winds (Astor et al., 2003).”
MethodDugdale, R., Wischmeyer, A., Wilkerson, F., Barber, R., Chai, F., Jiang, M., & Peng, T.-H. (2002) · doi:10.1016/s0967-0645(02)00046-2 · Cited by 68
Larval dispersal in a changing ocean with an emphasis on upwelling regions
Bashevkin, S. M., Dibble, C. D., Dunn, R. P., Hollarsmith, J. A., Ng, G., Satterthwaite, E. V., & Morgan, S. G. (2020) · Ecosphere · doi:10.1002/ecs2.3015 · Cited by 93
Recycled iron fuels new production in the eastern equatorial Pacific Ocean
Rafter, P., Sigman, D., & Mackey, K. (2017) · Nature Communications · doi:10.1038/s41467-017-01219-7 · Cited by 67
Reum, J. C. P., Alin, S. R., Harvey, C. J., Bednaršek, N., Evans, W., Feely, R. A., Hales, B., Lucey, N., Mathis, J. T., McElhany, P., et al. (2015) · ICES Journal of Marine Science · doi:10.1093/icesjms/fsu231 · Cited by 69
“Over interannual time-scales, large-scale climate phenomena like El Niño/Southern Oscillation can influence upwelling patterns, coastal productivity, carbonate chemistry (Chavez et al., 1999; Friederich et al., 2002) , and thus potentially relationships among pCO 2 and temperature and O 2 .”
Self-citationRafter, P., & Sigman, D. (2016) · Limnology and Oceanography · doi:10.1002/lno.10152 · Cited by 67
Racault, M., Sathyendranath, S., & Platt, T. (2014) · Remote Sensing of Environment · doi:10.1016/j.rse.2014.05.016 · Cited by 89
Effects of fishing, market price, and climate on two South American clam species
Ortega, L., Castilla, J., Espino, M., Yamashiro, C., & Defeo, O. (2012) · Marine Ecology Progress Series · doi:10.3354/meps10016 · Cited by 78
“…2002, Chavez et al. 2003, Montecino & Lange 2009), causing dramatic changes in faunal assemblages (e.g. Barber & Chavez 1983, Castilla & Camus 1992, Chavez et al. 1999, Tarazona & Arntz 2001), and affecting the domestic economy of Chile and Peru (Thatje & Heilmayer 2008), including artisanal…”
BackgroundNam, S., Kim, H.-J., & Send, U. (2011) · Geophysical Research Letters · doi:10.1029/2011gl049549 · Cited by 68
Revisiting the Thermocline Depth in the Equatorial Pacific
Yang, H.-J., & Wang, F. (2009) · doi:10.1175/2009jcli2836.1 · Cited by 67
“…equatorial Pacific, Z20 is broadly used as the DTC for studies (Kessler 1990; Ji et al. 1995; Vialard and Delecluse 1998; Swenson and Hansen 1999; Chavez et al. 1999; Durand and Delcrolx 2000; Vecchi and Harrison 2000; Meinen and McPhaden 2000; Fedorov and Philander 2001; Chepurin et al. 2005)…”
MethodNemoto, K., Midorikawa, T., Wada, A., Ogawa, K., Takatani, S., Kimoto, H., Ishii, M., & Inoue, H. Y. (2009) · doi:10.1016/j.dsr2.2008.12.015 · Cited by 67
“A high-resolution time series of pCO2 sea revealed variations on many scales in the subtropical North Atlantic (Bates et al., 2000), the equatorial Atlantic (Bakker et al., 2001), the Mediterranean Sea (Hood and Merlivat, 2001; Copin-Montégut et al., 2004), the equatorial Pacific (Chavez et al., 1999), and the subtrop…”
BackgroundInfluentialWolanin, A., Rozanov, V. V., Dinter, T., Noël, S., Vountas, M., Burrows, J. P., & Bracher, A. U. (2015) · Remote Sensing of Environment · doi:10.1016/j.rse.2015.05.018 · Cited by 71
“The evident link between biology and the physical environment related to climate variability expressed by MEI has been shown for the Equatorial Pacific in the study by Rousseaux and Gregg (2012).”
BackgroundInfluentialVargas, F. H., Lacy, R., Johnson, P., Steinfurth, A., Crawford, R., Boersma, P., & Macdonald, D. W. (2007) · Biological Conservation · doi:10.1016/j.biocon.2007.02.005 · Cited by 64
“The two most extreme El Niño events in the past century occurred in 1982–1983 and 1997–1998 (Chavez et al., 1999; McPhaden, 1999), and it is thought that such severe events are now more common than was previously (before mid1970s) the case (Trenberth and Hoar, 1996).”
BackgroundOceanic and atmospheric anomalies of tropical instability waves
Polito, P. S., Ryan, J. P., Liu, W. T., & Chávez, F. P. (2001) · Geophysical Research Letters · doi:10.1029/2000gl012400 · Cited by 59
Self-citationThe Impact of Climate Change and Feedback Processes on the Ocean Carbon Cycle
Boyd, P. W., & Doney, S. C. (2003) · Springer eBooks · doi:10.1007/978-3-642-55844-3_8 · Cited by 54
“Phytoplankton – pico to large diatoms Equatorial Pacific Chavez et al. (1999)”
BackgroundInfluentialWitman, J., Brandt, M., & Smith, F. (2010) · doi:10.1890/08-1922.1 · Cited by 63
Kienast, M., Calvert, S., Pelejero, C., & Grimalt, J. (2001) · Global Biogeochemical Cycles · doi:10.1029/2000gb001285 · Cited by 62
Wolff, M., Ruiz, D., & Taylor, M. (2012) · Marine Ecology Progress Series · doi:10.3354/meps09542 · Cited by 61
“…which brought extended periods (of about 8 mo) of unusually warm (>26°C, occasionally up to 29°C) and nutrient-depleted waters to the surface layer (Chavez et al. 1999, Enfield 2001, Glynn et al. 2001, Wellington et al. 2001), and phytoplankton biomass that was reduced by 50 to 70% of the mean…”
BackgroundJellyfish bycatch diminishes profit in an anchovy fishery off Peru
Quiñones, J., Monroy, A., Acha, E. M., & Mianzan, H. (2013) · doi:10.1016/j.fishres.2012.04.014 · Cited by 61
Cosca, C., Feely, R., Boutin, J., Etcheto, J., McPhaden, M., Chavez, F., & Strutton, P. (2003) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000jc000677 · Cited by 61
Self-citationZhang, R.-H., Zheng, F., Zhu, J.-S., Pei, Y.-H., Zheng, Q., & Wang, Z.-G. (2012) · Advances in Atmospheric Sciences · doi:10.1007/s00376-012-1235-4 · Cited by 60
Surface Mooring Network in the Kuroshio Extension
Cronin, M., Meinig, C., Sabine, C., Ichikawa, H., & Tomita, H. (2008) · IEEE Systems Journal · doi:10.1109/jsyst.2008.925982 · Cited by 60
“It was envisioned that the moored time series could be used to investigate and monitor air–sea fluxes and air–sea interaction, water mass formation and transformation, carbon cycling, and biogeochemical and ecosystem changes.”
BackgroundSandweiss, D., Maasch, K., Chai, F., Andrus, C., & Reitz, E. (2004) · Quaternary Research · doi:10.1016/j.yqres.2004.02.008 · Cited by 60
“During El Niño, reduced nutrient flux dramatically reduces productivity and disrupts the food web across the equatorial and coastal environments of the eastern tropical Pacific (Barber and Chavez, 1983; Chavez et al., 1999).”
BackgroundEffects of Spectral Bandpass on SeaWiFS-Retrieved Near-Surface Optical Properties of the Ocean.
Wang, M.-H., Franz, B., Barnes, R. A., & McClain, C. R. (2001) · Applied Optics · doi:10.1364/ao.40.000343 · Cited by 60
El Niño Southern Oscillation (ENSO) impact on tuna fisheries in Indian Ocean
Kumar, P. S., Pillai, G. N., & Manjusha, U. (2014) · SpringerPlus · doi:10.1186/2193-1801-3-591 · Cited by 59
“…(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 (Diaz and Markgraf 1992; Lehodey et al. 1997, 2003; Chavez et al. 1999).”
BackgroundProductivity patterns in the equatorial Pacific over the last 30,000 years
Costa, K. M., Jacobel, A. W., McManus, J. F., Anderson, R. F., Winckler, G., & Thiagarajan, N. (2017) · Global Biogeochemical Cycles · doi:10.1002/2016gb005579 · Cited by 77
Sarma, V. V. (2006) · Journal of Earth System Science · doi:10.1007/bf02702872 · Cited by 59
“…chlorophyll a (Chl a), and primary production decreased by > 50–60% during El Niño compared to the normal period due to deepening of thermocline and nitracline that results in decreased supply of nutrients to the photic zone in the eastern equatorial Pacific (Feely et al 2002; Chavez et al 1999).”
BackgroundHearn, A., Martínez, P., Toral-Granda, M. V., Murillo, J., & Polovina, J. (2005) · doi:10.1111/j.1365-2419.2005.00342.x · Cited by 59
Takesue, R., van Geen, A., Carriquiry, J., Ortiz, E., Godínez-Orta, L., Granados, I., Saldívar, M., Ortlieb, L., Escribano, R., Guzmán, N., et al. (2004) · doi:10.1029/2003jc001856 · Cited by 59
“[3] On interannual and decadal timescales, dramatic shifts in nearshore productivity and ecosystems, many of which have significant biological, social, and economic consequences [FAO, 1998], have been linked to changes in atmospheric and oceanic circulation (e.g., the El Nin˜o-Southern Oscillation (ENSO) [Chavez, 1996…”
BackgroundThe History of Climate Dynamics in the Late Quaternary
Labeyrie, L. D., Cole, J. E., Alverson, K., & Stocker, T. F. (2003) · Global change - the IGBP series · doi:10.1007/978-3-642-55828-3_3 · Cited by 71
“…in the rates of atmospheric pCO2 increase are attributable to ENSO variability, through changes in surface ocean temperature and upwelling patterns (Chavez et al. 1999, Feely et al. 1999) together with the response of terrestrial productivity to changes in water balance and nutrient feedbacks…”
BackgroundFeely, R., Wanninkhof, R., McGillis, W., Carr, M., & Cosca, C. (2004) · Journal of Geophysical Research Atmospheres · doi:10.1029/2003jc001896 · Cited by 58
“This region, particularly the central and eastern equatorial Pacific, exhibits a large amount of spatial and temporal variability in surface water carbon dioxide fugacity (fCO2) due to El Nin˜o–Southern Oscillation (ENSO)-driven physical and biological changes [ Chavez et al., 1999; Feely et al., 2002].”
BackgroundSelf-citationSahoo, B., Thomas, P. J., Thomas, P., & Greve, M. M. (2025) · ACS Sensors · doi:10.1021/acssensors.4c02670 · Cited by 57
Thomas, A., Strub, P., Weatherbee, R. A., & James, C. (2012) · doi:10.1016/j.dsr2.2012.04.008 · Cited by 57
“Deep-S the El Niño Southern Oscillation (ENSO), can be of similar magnitude or larger than local seasonal cycles (e.g., Chavez et al., 1999; Martinez et al., 2009; Vantrepotte and Mélin, 2011; Yoder and Kennelly, 2003), transmitted through atmospheric teleconnections (e.g., Chhak and DiLorenzo,…”
BackgroundWang, X.-J., Christian, J., Murtugudde, R., & Busalacchi, A. (2005) · Geophysical Research Letters · doi:10.1029/2004gl021538 · Cited by 57
Park, J.-Y., Kug, J., Park, J., Yeh, S., & Jang, C. (2011) · doi:10.1029/2011jc007056 · Cited by 56
“[7] In contrast to the impact of climatic variability on the marine ecosystem, another line of studies argued that phytoplankton can also provide biological feedback in the climate system [Lewis et al., 1990; Arrigo et al., 1999; Chavez et al., 1999; Nakamoto et al., 2000; Timmermann and Jin, 2002; Lengaigne et al., 2…”
BackgroundMethodResultInfluentialBouteiller, A. L., Leynaert, A., Landry, M., Borgne, R. L., Neveux, J., Rodier, M., Blanchot, J., & Brown, S. L. (2003) · Journal of Geophysical Research Atmospheres · doi:10.1029/2001jc000914 · Cited by 56
Ambriz-Arreola, I., Gómez-Gutiérrez, J., Franco-Gordo, M. D. C., Lavaniegos, B., & Godínez-Domínguez, E. (2012) · doi:10.3354/meps09607 · Cited by 55
Pradhan, Y., Lavender, S., Hardman-Mountford, N. J., & Aiken, J. (2006) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/j.dsr2.2006.05.016 · Cited by 55
“ENSO-related hydrographic and phytoplankton anomalies have been reported extensively for Pacific EBCs (Chavez et al., 1999; Thomas et al., 2001a; Thomas et al., 2004).”
BackgroundYang, E. J., Choi, J. K., & Hyun, J. (2004) · Marine Biology · doi:10.1007/s00227-004-1412-9 · Cited by 54
“A dramatic recovery, which led to La Nin˜ a conditions after the El Nin˜ o event of 1997, began in mid-1998 ( Chavez et al. 1999 ).”
BackgroundThe impact of El Niño events on populations of mesopelagic hydromedusae
Raskoff, K. A. (2001) · Hydrobiologia · doi:10.1023/a:1011812812662 · Cited by 34
Sánchez‐Velasco, L., Beier, E., Godínez, V. M., Barton, E. D., Santamaría‐del‐Ángel, E., Jiménez-Rosemberg, S. P. A., & Marinone, S. G. (2017) · Journal of Geophysical Research Oceans · doi:10.1002/2016jc012622 · Cited by 62
Legler, D., Freeland, H., Lumpkin, R., Ball, G., McPhaden, M., North, S., Crowley, R., Goni, G., Send, U., & Merrifield, M. (2015) · doi:10.1080/1755876x.2015.1049883 · Cited by 54
“Chavez et al. (1999) also took advantage of data from the array and other satellite and in situ data sources to comprehensively describe the marine biological and chemical consequences of the 1997/ 1998 El Niño.”
BackgroundSelf-citationAtmospheric forcing on chlorophyll concentration in the Mediterranean
Katara, I., Illian, J., Pierce, G., Scott, B., & Wang, J. (2008) · Hydrobiologia · doi:10.1007/s10750-008-9492-z · Cited by 54
“On a less extensive scale, the most profound and best-studied large-scale, oceanic-atmospheric phenomenon, affecting phytoplankton concentration, is El Nin ˜o. The mechanisms proposed to link changes in the atmosphere to primary productivity during these events include the presence of upwelling favourable winds, the p…”
BackgroundBucaram, S. J., Hearn, A. R., Trujillo, A. M. T., Rentería, W., Bustamante, R. H., Morán, G., Reck, G. K., & García, J. L. (2017) · Marine Policy · doi:10.1016/j.marpol.2017.10.002 · Cited by 77
Biogeochemical impact of tropical instability waves in the equatorial Pacific
Gorgues, T., Menkes, C., Aumont, O., Vialard, J., Dandonneau, Y., & Bopp, L. (2005) · Geophysical Research Letters · doi:10.1029/2005gl024110 · Cited by 52
Nezlin, N., & Li, B.-L. (2003) · doi:10.1016/s0924-7963(03)00030-7 · Cited by 52
“The 1997–1998 El Niño event was the strongest in the 20th century (Chavez et al., 1999; Kahru and Mitchell, 2000; McPhaden, 1999).”
BackgroundCCE IV: El Niño-related zooplankton variability in the southern California Current System
Lilly, L. E., & Ohman, M. (2018) · Deep Sea Research Part I: Oceanographic Research Papers · doi:10.1016/j.dsr.2018.07.015 · Cited by 51
Large-scale shifts in phytoplankton groups in the Equatorial Pacific during ENSO cycles
Masotti, I., Moulin, C., Alvain, S., Bopp, L., Tagliabue, A., & Antoine, D. (2010) · Biogeosciences · doi:10.5194/bg-8-539-2011 · Cited by 51
Water column productivity and temperature predict coral reef regeneration across the Indo-Pacific
Riegl, B., Glynn, P., Wieters, E., Purkis, S., D'Angelo, C., & Wiedenmann, J. (2015) · Scientific Reports · doi:10.1038/srep08273 · Cited by 50
Warming increases the top-down effects and metabolism of a subtidal herbivore
Carr, L. A., & Bruno, J. (2013) · PeerJ · doi:10.7717/peerj.109 · Cited by 50
“This annual cycle is interrupted during ENSO events (Barber & Chavez, 1983; Chavez et al., 1999).”
BackgroundWallace, B. P., & Saba, V. (2009) · doi:10.3354/esr00177 · Cited by 50
“…productivity (NPP), the base of the marine food web, in the foraging areas of EP leatherbacks (Morreale et al. 1996, Eckert & Sarti 1997, Shillinger et al. 2008) is affected by ENSO events every 3 to 7 yr (Chavez et al. 1999) and by multi-decadal variability every 20 to 30 yr (Chavez et al. 2003).”
BackgroundRole of ocean biology‐induced climate feedback in the modulation of El Niño‐Southern Oscillation
Zhang, R.-H., Busalacchi, A., Wang, X.-J., Ballabrera-Poy, J., Murtugudde, R., Hackert, E., & Chen, D.-K. (2009) · doi:10.1029/2008gl036568 · Cited by 50
Duffy-Anderson, J., Busby, M. S., Mier, K., Deliyanides, C. M., & Stabeno, P. (2006) · doi:10.1111/j.1365-2419.2005.00348.x · Cited by 50
“While not all El Nin˜o events manifest Nin˜o North effects, the El Nin˜o event of 1997‐98 was particularly intense ( Chavez et al., 1999, 2002 ) and unusual conditions occurred in the EBS in 1997.”
BackgroundKobayashi, F., & Takahashi, K. (2002) · doi:10.1016/s0967-0645(02)00059-0 · Cited by 50
Robidart, J., Preston, C., Paerl, R. W., Turk, K., Mosier, A., Francis, C. A., Scholin, C., & Zehr, J. (2011) · The ISME Journal · doi:10.1038/ismej.2011.127 · Cited by 49
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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