The DOI matches its Crossref record; 40 of the 41 references it cites were found in a registry or an index.
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.
Overview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
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?
In the citing paper
“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
Citations
Cites
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
Observational Contrains on the Global Atmospheric Co 2 Budget
Tans, P. P., Fung, I. Y., & Takahashi, T. (1990) · Science · doi:10.1126/science.247.4949.1431 · Cited by 2,066
Coale, K. H., Johnson, K. S., Fitzwater, S. E., Gordon, R. M., Tanner, S., Chavez, F. P., Ferioli, L., Sakamoto, C., Rogers, P., Millero, F., et al. (1996) · Nature · doi:10.1038/383495a0 · Cited by 1,479
Self-citationTesting the iron hypothesis in ecosystems of the equatorial Pacific Ocean
Martin, J. H., Coale, K., Johnson, K., Fitzwater, S., Gordon, R., Tanner, S., Hunter, C., Elrod, V., Nowicki, J., Coley, T., et al. (1994) · Nature · doi:10.1038/371123a0 · Cited by 1,445
Self-citationGenesis and evolution of the 1997-98 El Nino
McPhaden, M. (1999) · Science · doi:10.1126/science.283.5404.950 · Cited by 1,307
Self-citationKolber, Z., Prášil, O., & Falkowski, P. (1998) · Biochimica et Biophysica Acta · doi:10.1016/s0005-2728(98)00135-2 · Cited by 902
Biological Consequences of El Ni�o
Barber, R., & Chavez, F. (1983) · Science · doi:10.1126/science.222.4629.1203 · Cited by 799
Self-citationAn estimate of new production in the equatorial Pacific
Chavez, F., & Barber, R. (1987) · Deep Sea Research Part A Oceanographic Research Papers · doi:10.1016/0198-0149(87)90073-2 · Cited by 483
Self-citationGlobal air-sea flux of CO 2 : An estimate based on measurements of sea–air pCO 2 difference
Takahashi, T., Feely, R. A., Weiss, R. F., Wanninkhof, R. H., Chipman, D. W., Sutherland, S. C., & Takahashi, T. T. (1997) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.94.16.8292 · Cited by 471
Self-citationAtmospheric Predictability and Two-Dimensional Turbulence
Leith, C. E. (1971) · Journal of the Atmospheric Sciences · doi:10.1175/1520-0469(1971)028 · Cited by 460
Flagged first, then by citations
1 of the 41 references couldn’t be matched to a known paper.
Research works printed but not linked: 10
- J. R. Toggweiler and S. Carson in Upwelling the Ocean: Modern Processes and Ancient Records C. P. Summerhayes et al. Eds. (Wiley Chichester UK 1995) pp. 337–360.
- Barnett T. P., Latif M., Kirk E., Roeckner E., J. Clim. 4, 487 (1991). · DOI
- Weller R. A., Anderson S. P., J. Clim. 9, 1959 (1996). · DOI
- Keeling C. D., Revelle R., Meteoritics 20, 437 (1985).
- Inoue H. Y., Sugimura Y., Tellus 44, 1 (1992). · DOI
- D. Meyers and J. J. O'Brien Eos 76 533 (1995). · DOI
- F. P. Chavez and S. L. Smith in Upwelling in the Ocean: Modern Processes and Ancient Records C. P. Summerhayes et al. Eds. (Wiley Chichester UK 1995) pp. 149–169.
- F. P. Chavez and J. R. Toggweiler in Upwelling in the Ocean: Modern Processes and Ancient Records C. P. Summerhayes et al. Eds. (Wiley Chichester UK 1995) pp. 313–320.
- 10.1016/S0304-4203(97)00043-1 · DOI
- Cochlan W. P., Kudela R. M., Eos 76, 177 (1996).
Cited by
Sorted by citations
Items 201–300 of 570
Keller, K., Slater, R., Bender, M., & Key, R. (2001) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(01)00106-0 · Cited by 49
“…trends of the marine biota (Venrick et al., 1987; Karl et al., 1995; McGowan et al., 1998), potentially driven by changes in trace metal supply (Jickells et al., 1998; Chavez et al., 1999), changes in nitrogen fixation (Karl et al., 1995), or changes in mixed-layer depth (Freeland et al., 1997).”
BackgroundInfluentialVinueza, L., Menge, B., Jarrin, D. J. R., & Palacios, D. (2014) · Ecological Monographs · doi:10.1890/13-0169.1 · Cited by 48
“…cycles by humans (Valiela et al. 1997, Vitousek et al. 1997), large-scale environmental perturbations such as El Niño-Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO; Barber and Chavez 1983, Chavez et al. 1999), and human-induced climate change (Post and Pedersen 2008).”
InfluentialNon-native species in Canada’s boreal zone: diversity, impacts, and risk1
Langor, D., Cameron, E., Macquarrie, C., McBeath, A., McClay, A., Peter, B., Pybus, M., Ramsfield, T., Ryall, K., Scarr, T., et al. (2014) · Environmental Reviews · doi:10.1139/er-2013-0083 · Cited by 48
Consequences of regime shifts for marine food webs
Alheit, J. (2007) · International Journal of Earth Sciences · doi:10.1007/s00531-007-0232-9 · Cited by 44
deFrance, S. D. (2005) · Journal of Archaeological Science · doi:10.1016/j.jas.2005.03.001 · Cited by 40
A global analysis of ENSO synchrony: The oceans' biological response to physical forcing
Messié, M., & Chávez, F. P. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2012jc007938 · Cited by 48
Self-citationSeasonal, interannual and event scale variation in North Pacific ecosystems
Yoo, S., Batchelder, H. P., Peterson, W. T., & Sydeman, W. J. (2008) · Progress In Oceanography · doi:10.1016/j.pocean.2008.03.013 · Cited by 46
Comparisons of chlorophyll variability between the four major global eastern boundary currents
Thomas, A., Strub, P., Carr, M., & Weatherbee, R. A. (2004) · doi:10.1080/01431160310001592418 · Cited by 47
“In all four regions, interannual variability is evident in the two years examined, most notably in the two Pacific EBCs (California and Humboldt), where the strong 1997–1998 El Nino event caused large hydrographic and biological anomalies ( Chavez et al. 1999 , Thomas et al.”
BackgroundFormation of a basin‐scale surface chlorophyll pattern by Rossby waves
Kawamiya, M., & Oschlies, A. (2001) · Geophysical Research Letters · doi:10.1029/2001gl013347 · Cited by 47
Godínez-Domínguez, E., Rojo-Vázquez, J., Galván-Piña, V. H., & Aguilar-Palomino, B. (2000) · Estuarine Coastal and Shelf Science · doi:10.1006/ecss.2000.0724 · Cited by 47
Sasaoka, K., Saitoh, S., Asanuma, I., Imai, K., Honda, M., Nojiri, Y., & Saino, T. (2002) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(02)00206-0 · Cited by 47
Liao, E., Resplandy, L., Liu, J., & Bowman, K. W. (2020) · Global Biogeochemical Cycles · doi:10.1029/2020gb006574 · Cited by 84
Thatje, S., Heilmayer, O., & Laudien, J. (2008) · Helgoland Marine Research · doi:10.1007/s10152-008-0104-0 · Cited by 46
“Some of the best data on climate impact available at this time refer to EN as a consequence of the fact that the two strong EN events 1982–1983 and 1997–1998 were exceptionally well documented (e.g. Barber and Chávez 1983; Chávez et al. 1999; Tarazona et al. 2001).”
BackgroundFranco-Gordo, C., Godínez-Domínguez, E., Filonov, A., Tereshchenko, I., & Freire, J. (2004) · Progress In Oceanography · doi:10.1016/j.pocean.2004.10.001 · Cited by 46
“The effects off Central (Chavez et al., 2002) and Southern California (Bograd & Lynn, 2001) were similar to those in the equatorial Pacific (Chavez et al., 1999).”
BackgroundResultAssessment of SeaWiFs atmospheric and marine products for the Northern Adriatic Sea
Mélin, F., Zibordi, G., & Berthon, J. (2003) · IEEE Transactions on Geoscience and Remote Sensing · doi:10.1109/tgrs.2003.809939 · Cited by 46
“End products derived from SeaWiFS imagery are extensively used for the study of marine phytoplankton biomass distribution and production (e.g., [ 2 ]‐[5]), and of aerosol load (e.g., [6] and [7]).”
BackgroundIn-Water Instrumentation and Platforms for Ocean Color Remote Sensing Applications
Twardowski, M. S., Lewis, M. R., Barnard, A. H., & Zaneveld, J. R. V. (2007) · Remote sensing and digital image processing · doi:10.1007/978-1-4020-3100-7_4 · Cited by 41
“While several moored sensor systems have been deployed in the more classical oceanic case 1 remote sensing environments (Clark et al., 1997; Chavez et al., 1999; Dickey et al., 1998, 2001), few have been deployed in more optically complex case 2 environments.”
MethodAcuña-Marrero, D., Smith, A. N. H., Salinas-de-León, P., Harvey, E., Pawley, M., & Anderson, M. (2018) · Marine Ecology Progress Series · doi:10.3354/meps12505 · Cited by 45
“…to December, when the Humboldt Current increases in intensity and the EF moves north and settles just north of the GA (Palacios 2004) In addition, periodical climatic disturbances, such El Niño Southern Oscillations (ENSO), significantly affect the marine communities of the GA (Chavez et al. 1999)”
InfluentialZhang, R.-H., Gao, C., Kang, X., Zhi, H., Wang, Z.-G., & Feng, L.-C. (2015) · Scientific Reports · doi:10.1038/srep18506 · Cited by 45
Equatorial Pacific chemical and biological variability, 1997–2003
Strutton, P., Evans, W., & Chavez, F. (2008) · doi:10.1029/2007gb003045 · Cited by 45
“[12] The mean chlorophyll value for the central region (Figure 4b), based on both satellite and in situ measurements, is very close to the 0.21 mg m 3 calculated for 1980–1998 [Chavez et al., 1999].”
BackgroundResultInfluentialSelf-citationSeasonal variation of the principal tidal constituents in the Bohai Sea
Wang, D.-S., Pan, H.-D., Jin, G., & Lv, X.-Q. (2020) · doi:10.5194/os-16-1-2020 · Cited by 44
“…Dalian is from 1980 to 1997, which are from different eras and may defy comparison because the 1997–1998 El Niño is one of the strongest in the 20th century (Chavez et al., 1999) and changes many of the physical oceanic properties (Nezlin and Mcwilliams, 2003; Shang et al., 2005; Liu et al., 2010).”
BackgroundOcean physics and nutrient fields along 180° during an El Niño-Southern Oscillation cold phase
Eldin, G., & Rodier, M. (2003) · doi:10.1029/2000jc000746 · Cited by 44
Shipe, R., Passow, U., Brzezinski, M., Graham, W. M., Pak, D., Siegel, D., & Alldredge, A. (2002) · doi:10.1016/s0079-6611(02)00045-9 · Cited by 44
“For example, a phytoplankton bloom of exceptionally large spatial extent developed in the equatorial Pacifi c after the 1997–98 El Nin ˜o event ( Chavez et al., 1999 ).”
BackgroundTurk, D., Lewis, M., Harrison, G., Kawano, T., & Asanuma, I. (2001) · doi:10.1029/1999jc000058 · Cited by 44
Variability of fCO2 in the Eastern Tropical Atlantic from a moored buoy
Lefèvre, N., Guillot, A., Beaumont, L., & Danguy, T. (2008) · Journal of Geophysical Research Atmospheres · doi:10.1029/2007jc004146 · Cited by 44
“For example, in the tropical Pacific, some Tropical Atmosphere Ocean (TAO) moorings are now equipped with infrared CO2 instruments [ Chavez et al., 1999 ] and in the Baltic Sea a SAMI-CO2 sensor [DeGrandpre et al., 1995] was installed on a moored platform [Kuss et al., 2006] but high frequency measurements are still s…”
BackgroundReconstructing Global Chlorophyll-a Variations Using a Non-linear Statistical Approach
Martinez, E., Gorgues, T., Lengaigne, M., Sauzède, R., Menkes, C., Uitz, J., Di Lorenzo, E., & Fablet, R. (2020) · Frontiers in Marine Science · doi:10.3389/fmars.2020.00464 · Cited by 43
The impacts of extreme El Niño events on sea turtle nesting populations
Tomillo, P. S., Fonseca, L. G., Ward, M., Tankersley, N., Robinson, N. J., Orrego, C. M., Paladino, F. V., & Saba, V. S. (2020) · Climatic Change · doi:10.1007/s10584-020-02658-w · Cited by 49
Brewin, R., Lavender, S., Hardman-Mountford, N., & Hirata, T. (2010) · doi:10.1007/s13131-010-0018-y · Cited by 43
“Such an index has previously been found to have major impacts on phytoplankton and fisheries (Barber and Chavez, 1983; Chavez et al., 1999; Behrenfeld et al., 2001).”
BackgroundRadenac, M., Menkès, C., Vialard, J., Moulin, C., Dandonneau, Y., Delcroix, T., Dupouy, C., Stoens, A., & Deschamps, P. (2001) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000jc000546 · Cited by 43
“In contrast to the moderate 1991-1992 El Niño when nitrate persisted at the surface [McCarthy et al., 1996], no nitrate is measured in the surface layer in the central Pacific [Chavez et al., 1999] in 1997.”
BackgroundResultInfluentialPalacz, A., John, M. S., Brewin, R., Hirata, T., & Gregg, W. (2013) · Biogeosciences · doi:10.5194/bg-10-7553-2013 · Cited by 42
“Such a response was also indicated by in situ (Chavez et al., 1999), dynamic (Gorgues et al., 2010) and some remote sensing (Masotti et al., 2011) modeling studies, which report that diatoms first decreased and later increased significantly in response to El Niño and La Niña, respectively.”
BackgroundImplications of changing El Niño patterns for biological dynamics in the equatorial Pacific Ocean
Turk, D., Meinen, C. S., Antoine, D., McPhaden, M. J., & Lewis, M. R. (2011) · Geophysical Research Letters · doi:10.1029/2011gl049674 · Cited by 42
“[2] El Niño is known to result in interannual climate fluctuations over the Pacific Ocean, which in turn cause variability in biological production and ecosystem dynamics [e.g., Murtugudde et al., 1999; Chavez et al., 1999; McClain et al., 2002; Wang et al., 2005].”
BackgroundSelf-citationSydeman, W. J., Thompson, S. A., García‐Reyes, M., Kahru, M., Peterson, W. T., & Largier, J. L. (2013) · Progress In Oceanography · doi:10.1016/j.pocean.2013.10.017 · Cited by 47
Emerging themes in Population Consequences of Disturbance models
Keen, K., Beltran, R., Pirotta, E., & Costa, D. (2021) · Proceedings of the Royal Society B · doi:10.1098/rspb.2021.0325 · Cited by 41
Patterns and ecological implications of historical marine phytoplankton change
Boyce, D., & Worm, B. (2015) · Marine Ecology Progress Series · doi:10.3354/meps11411 · Cited by 48
“…consequences of marine phytoplankton change derive from studies of the effects of quasiperiodic climate fluctuations, for example from the El Nino Southern Oscillation or North Atlantic Oscillation (NAO; Barber & Chavez 1986, Chavez et al. 1999, Behrenfeld et al. 2006, Martinez et al. 2009).”
BackgroundV., J. M. R. (2006) · Marine Biology · doi:10.1007/s00227-005-0165-4 · Cited by 41
Climate forcing growth rates: doubling down on our Faustian bargain
Hansen, J. E., Kharecha, P. A., & Sato, M. (2013) · Environmental Research Letters · doi:10.1088/1748-9326/8/1/011006 · Cited by 38
“Interannual variability of CO2 growth is correlated with ENSO (El Nino Southern Oscillation) variations of tropical temperatures (figure 2).”
BackgroundInfluentialJuranek, L. W., & Quay, P. D. (2010) · Global Biogeochemical Cycles · doi:10.1029/2009gb003492 · Cited by 43
“Generally, upwelled water bears the signature of organic matter remineralization, including high pCO2 and nutrient content [ Chavez et al., 1999; Feely et al., 2006] and low O2 content [Hendricks et al., 2005; Kaiser et al., 2005].”
BackgroundRevisiting the La Niña 1998 phytoplankton blooms in the equatorial Pacific
Gorgues, T., Menkes, C., Slemons, L. O., Aumont, O., Dandonneau, Y., Radenac, M., Alvain, S., & Moulin, C. (2010) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2009.12.008 · Cited by 40
Reina, R., Spotila, J., Paladino, F., & Dunham, A. (2009) · doi:10.3354/esr00098 · Cited by 40
“The thermal and nutrient shift in the Pacific during this transition resulted in the recovery of the phytoplankton community following an extended period of impoverishment during the El Niño years preceding it (Chavez et al. 1999).”
BackgroundInfluentialEffects of El Niño-driven changes in wind patterns on North Pacific albatrosses
Thorne, L. H., Conners, M. G., Hazen, E. L., Bograd, S. J., Antolos, M., da Costa, D. P., & Shaffer, S. A. (2016) · Journal of The Royal Society Interface · doi:10.1098/rsif.2016.0196 · Cited by 37
Buchan, S. J., Stafford, K., & Hucke-Gaete, R. (2015) · Marine Mammal Science · doi:10.1111/mms.12173 · Cited by 39
Impact of bio-physical feedbacks on the tropical climate in coupled and uncoupled GCMs
Park, J.-Y., Kug, J., Seo, H., & Bader, J. (2014) · Climate Dynamics · doi:10.1007/s00382-013-2009-0 · Cited by 39
“In fact, an observational study showed that a phytoplankton bloom in the upper ocean can induce a significant drawdown of atmospheric carbon dioxide (CO2), implying the existence of ocean biology-induced climate feedback from a geochemical viewpoint (Chavez et al. 1999).”
BackgroundWang, X.-J., Christian, J., Murtugudde, R., & Busalacchi, A. (2006) · doi:10.1029/2005jc002972 · Cited by 39
Hernández-Miranda, E., & Ojeda, F. (2006) · doi:10.1007/s00227-006-0249-9 · Cited by 39
“Other organisms have also been reported to experience changes in their population abundance including algae, invertebrates, larval fish, seabirds, and marine mammals (Soto 1985; Tomicic 1985; Castilla and Camus 1992; Massey et al. 1992; Arntz and Fahrbach 1996; Tsai et al. 1997; Arcos et al. 2001; Riascos 2002; Fiedle…”
BackgroundPérez, V., Fernández, E., Emilio Marañón, C., Serret, P., Varela, R., Bode, A., Varela, M., Varela, M. M., Morán, X. A. G., Woodward, E. M. S., et al. (2005) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2005.01.002 · Cited by 40
Martínez, I., Rincon, D., Yokoyama, Y., & Barrows, T. T. (2004) · doi:10.1016/j.palaeo.2005.10.022 · Cited by 39
“Diatoms and picoplankton are dominant during La Niña and El Niño phases, respectively (Chavez et al., 1999).”
BackgroundBrunskill, G. (2004) · doi:10.1016/j.csr.2004.08.001 · Cited by 39
Kang, X., Zhang, R.-H., Gao, C., & Zhu, J.-S. (2017) · Scientific Reports · doi:10.1038/s41598-017-17390-2 · Cited by 38
Influence of phytoplankton on the global radiation budget
Frouin, R., & Iacobellis, S. F. (2002) · Journal of Geophysical Research: Atmospheres · doi:10.1029/2001jd000562 · Cited by 37
Ryan, J., Green, J., Espinoza, E., & Hearn, A. (2017) · PLoS ONE · doi:10.1371/journal.pone.0182599 · Cited by 37
A rainy northern Atacama Desert during the last interglacial
Contreras, S., Lange, C., Pantoja, S., Lavik, G., Rincón-Martínez, D., & Kuypers, M. (2010) · doi:10.1029/2010gl045728 · Cited by 37
“[10] The presence of warm surface waters along the Peruvian coast increases stability in the water column, enhances stratification, and thus, reduces nutrient supply, primary productivity, and ultimately TOC flux to the sediment [Chavez et al., 1999].”
BackgroundAn exploratory modeling study on bio-physical processes associated with ENSO
Park, J.-Y., Kug, J., & Park, Y.-G. (2014) · doi:10.1016/j.pocean.2014.03.013 · Cited by 36
Liu, Y.-Y., Xie, L., Morrison, J., Kamykowski, D., & Sweet, W. (2014) · doi:10.1155/2014/198686 · Cited by 36
The rocky road from research to operations for satellite ocean-colour data in fishery management
Wilson, C. (2011) · ICES Journal of Marine Science · doi:10.1093/icesjms/fsq168 · Cited by 36
Hydrographic and biological changes in the Taiwan Strait during the 1997–1998 El Niño winter
Shang, S., Zhang, C., Hong, H., Liu, Q.-Y., Wong, G. T., Hu, C.-M., & Huang, B.-Q. (2005) · doi:10.1029/2005gl022578 · Cited by 36
“The El Nin˜o event of 1997–1998 was one of the strongest on record and it reached its peak in the winter of 1998 [ Chavez et al. , 1999] (Winter in a given year is defined in this paper as the three-month period between December 1 of the preceding year through the February of the given year).”
BackgroundGlobal eddy permitting simulations of surface ocean nitrogen, iron, sulfur cycling.
Chu, S.-P., Elliott, S., & Maltrud, M. (2003) · Chemosphere · doi:10.1016/s0045-6535(02)00162-5 · Cited by 36
Cui, T., Green, H., Selleck, P., Zhang, Z.-F., O'Brien, R., Gold, A., Keywood, M., Kroll, J., & Surratt, J. (2019) · ACS Earth and Space Chemistry · doi:10.1021/acsearthspacechem.9b00061 · Cited by 35
Impacts of ENSO on air‐sea oxygen exchange: Observations and mechanisms
Eddebbar, Y. A., Long, M. C., Resplandy, L., Rödenbeck, C., Rodgers, K. B., Manizza, M., & Keeling, R. F. (2017) · Global Biogeochemical Cycles · doi:10.1002/2017gb005630 · Cited by 53
“In the eastern equatorial Pacific, changes in net primary productivity are especially sensitive to the effects of Kelvin waves on the depth of the nutricline [Chavez et al., 1999].”
BackgroundInfluentialPhytoplankton blooms detected by SeaWiFS along the central and southern California coast
Nezlin, N. P., Sutula, M. A., Stumpf, R. P., & Sengupta, A. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jc007773 · Cited by 34
“The positive effect of stormwater nutrient discharge may have been counterbalanced by negative effect of stronger than normal nutrient limitation that resulted from El Niño-driven deep pycnocline (e.g., Chavez et al. 1998, 1999).”
BackgroundShi, W., Wang, M., Li, X.-F., & Pichel, W. (2011) · doi:10.1016/j.rse.2011.03.015 · Cited by 35
Legeckis, R., Brown, C., Bonjean, F., & Johnson, E. S. (2004) · doi:10.1029/2004gl021637 · Cited by 35
“1998, an unprecedented phytoplankton bloom appeared at the equator as described by Chavez et al. [1999] .”
BackgroundFox, M., Guillaume‐Castel, R., Edwards, C., Glanz, J., Gove, J., Green, J. A. M., Juhlin, E., Smith, J. E., & Williams, G. J. (2023) · Science Advances · doi:10.1126/sciadv.add5032 · Cited by 34
“The central Pacific provides an opportunity to explore the impact of declining pelagic subsidies, primarily nutrient concentrations and planktonic biomass, to coral reefs during heat waves because sea surface temperature and primary production are inversely related during strong El Niños ( 14 ).”
Dewitte, B., & Takahashi, K. I. (2017) · Climate Dynamics · doi:10.1007/s00382-017-4051-9 · Cited by 44
“2013), owed to its dramatic societal and economical consequences (Glantz 2001; Chavez et al. 1999), it is now recognized that a substantial share of the interannual SST variability in the tropical Pacific is associated with moderate El Niño events (Rasmusson and Carpenter 1982; Ashok et al.”
BackgroundBrady, R., Lovenduski, N., Alexander, M., Jacox, M., & Gruber, N. (2018) · Biogeosciences · doi:10.5194/bg-2018-415 · Cited by 34
Modeling the ENSO impact of orbitally induced mean state climate changes
Salau, O., Schneider, B., Park, W., Khon, V., & Latif, M. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jc007742 · Cited by 34
“The phenomenon influences not only climate and biosphere, but also the economies of several countries through impacts on agriculture and fisheries, thereby affecting human societies in many different ways [McPhaden et al., 2006; Chavez et al., 1999].”
BackgroundCan bottom-up ocean CO2 fluxes be reconciled with atmospheric 13C observations?
Alden, C., Miller, J. B., & White, J. (2010) · Tellus B · doi:10.1111/j.1600-0889.2010.00481.x · Cited by 34
“, 1993; Ciais et al., 1995, Francey et al., 1995). Randerson et al. (2002) invoked irregular discrimination as a way to reconcile differences in variability between isotopic and non-isotopic calculations of land and ocean fluxes.”
BackgroundMethodInfluentialOptimal merging of LAC and GAC data from SeaWiFS
Mélin, F., Steinich, C., Gobron, N., Pinty, B., & Verstraete, M. (2002) · doi:10.1080/01431160110073129 · Cited by 34
“Expected marine features can be observed from these monthly averaged patterns: The chlorophyll bloom distorted by tropical instability waves in the Equatorial Paci c after the 1997–1998 El Niño event (Chavez et al. 1999) is particularly noticeable.”
BackgroundValsala, V. K., Roxy, M. K., Ashok, K., & Murtugudde, R. G. (2014) · Journal of Geophysical Research Oceans · doi:10.1002/2014jc010212 · Cited by 40
“CO2 fluxes from central and eastern equatorial Pacific during the mature phase of 1997-98 El Niño reduced to 0.2±0.15 moles m -2 yr -1 and after the recovery from El Niño, these values surged to 2~6 moles m -2 yr -1 [Chavez et al., 1999].”
InfluentialElemental composition of equatorial Pacific diatoms exposed to additions of silicic acid and iron
Baines, S., Twining, B., Vogt, S., Balch, W., Fisher, N., & Nelson, D. (2011) · doi:10.1016/j.dsr2.2010.08.003 · Cited by 33
Seasonal and interannual dynamics in diatom production in the Cariaco Basin, Venezuela
Romero, O. E., Thunell, R. C., Astor, Y., & Varela, R. (2008) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2008.12.005 · Cited by 40
“The occurrence of ENSO conditions from October 1997 through April 1998 (Chavez et al., 1999) appears to have interrupted the winter/ summer pattern of high/low diatom production and sedimentation in Cariaco Basin.”
BackgroundLagrangian study of tropical instability vortices in the Atlantic
Dutrieux, P., Menkes, C., Vialard, J., Flament, P., & Blanke, B. (2008) · Journal of Physical Oceanography · doi:10.1175/2007jpo3763.1 · Cited by 33
“…spring and summer in the tropical Atlantic and Pacific Oceans, the equatorial upwelling front exhibits north–south undulations on a scale of 1000 km (Legeckis 1977; Chavez et al. 1999) that shape the sea surface temperature and surface chlorophyll tracer fields in a series of troughs and crests.”
BackgroundWang, X.-J., Borgne, R. L., Murtugudde, R., Busalacchi, A., & Behrenfeld, M. (2008) · doi:10.5194/bg-5-1705-2008 · Cited by 32
Genetic Impact of a Severe El Niño Event on Galápagos Marine Iguanas (Amblyrhynchus cristatus)
Steinfartz, S., Glaberman, S., Lanterbecq, D., Márquez, C., Rassmann, K., & Caccone, A. (2007) · PLoS ONE · doi:10.1371/journal.pone.0001285 · Cited by 32
Bearzi, M. (2004) · J. Cetacean Res. Manage. · doi:10.47536/jcrm.v7i1.761 · Cited by 32
“By contrast, La Niña is characterised by upwelling-favourable trade winds that restore levels of primary productivity (Chavez et al. , 1999).”
BackgroundTorres, R., Turner, D., Rutllant, J., & Lefévre, N. (2003) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000jc000569 · Cited by 32
Ocean Chlorophyll as a Precursor of ENSO: An Earth System Modeling Study
Park, J.-Y., Dunne, J., & Stock, C. (2018) · Geophysical Research Letters · doi:10.1002/2017gl076077 · Cited by 31
“Dominant mechanisms governing the chlorophyll response to ENSO include changes in equatorial upwelling and thermocline depth (Chavez et al., 1999; Radenac et al., 2001; Wilson & Coles, 2005), and zonal advection (Picaut et al., 2001; Radenac et al., 2012; Stoens et al., 1999), all linked to…”
BackgroundIron sources and pathways into the Pacific Equatorial Undercurrent
Qin, X., Menviel, L., Gupta, A. S., & van Sebille, E. (2016) · doi:10.1002/2016gl070501 · Cited by 31
Thompson, P., Bonham, P., Thomson, P., Rochester, W., Doblin, M., Waite, A., Richardson, A., & Rousseaux, C. (2015) · doi:10.1093/plankt/fbv069 · Cited by 31
Wang, X.-J., Christian, J., Murtugudde, R., & Busalacchi, A. (2006) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/j.dsr2.2006.01.023 · Cited by 31
Yen, P. P., Sydeman, W., Morgan, K., & Whitney, F. (2005) · doi:10.1016/j.dsr2.2004.12.018 · Cited by 31
“…measurements at appropriately large spatial scales, since the profound effects of ocean climate on coastal and open-ocean ecological communities are often characterized by temporal lags and non-linear responses (Chavez et al., 1999; Hyrenbach and Veit, 2003; McGowan et al., 2003).”
BackgroundChanges in dominance of copepods off Baja California during the 1997-1999 El Niño and La Niña.
Jiménez-Pérez, L., & Lavaniegos, B. (2004) · Marine Ecology Progress Series · doi:10.3354/meps277147 · Cited by 30
“Nutrients and chlorophyll decreased sharply in the equatorial Pacific (Chavez et al. 1999) and relatively strongly in central California (Chavez et al. 2002), Oregon (Corwith & Wheeler 2002), and the Gulf of Alaska (Whitney & Welch 2002).”
BackgroundPersistent equatorial Pacific iron limitation under ENSO forcing
Browning, T., Saito, M., Garaba, S., Wang, X., Achterberg, E., Moore, C. M., Engel, A., Mcllvin, M. R., Moran, D. M., Voß, D., et al. (2023) · Nature · doi:10.1038/s41586-023-06439-0 · Cited by 30
“As expected, sea surface temperature anomalies (ΔSST) for the Niño3 region (Fig.”
BackgroundInfluentialModulation of ENSO evolution by strong tropical volcanic eruptions
Wang, T., Guo, D., Gao, Y., Wang, H., Zheng, F., Zhu, Y., Miao, J., & Hu, Y. (2017) · Climate Dynamics · doi:10.1007/s00382-017-4021-2 · Cited by 36
Villegas-Amtmann, S., McDonald, B. I., Páez-Rosas, D., Aurioles‐Gamboa, D., & Costa, D. (2017) · doi:10.1016/j.dsr2.2016.05.015 · Cited by 30
“In November 1997, close to the peak of El Niño event, chlorophyll concentrations were less than 0.05 mg/m3 in the central and eastern equatorial Pacific and mean primary productivity was 35–40 mmol of C/m2/day-about half the climatological mean (Chavez et al., 1996; Chavez et al., 1999).”
BackgroundInfluentialBond, A., Jones, I., Sydeman, W., Major, H., Minobe, S., Williams, J. C., & Byrd, G. V. (2011) · Marine Ecology Progress Series · doi:10.3354/meps08975 · Cited by 30
“While linkage between climatic and oceanographic variability has been found in many marine organisms (Beamish et al. 1997, Mantua et al. 1997, Chavez et al. 1999, Hunt et al. 2002, 2008, Durant et al. 2006, Byrd et al. 2008), most studies did not address spatial components in climatic and…”
BackgroundDefining isoscapes in the Northeast Pacific as an index of ocean productivity
Espinasse, B., Hunt, B., Batten, S., & Pakhomov, E. (2020) · Global Ecology and Biogeography · doi:10.1111/geb.13022 · Cited by 29
Franco-Gordo, C., Godínez-Domínguez, E., Suárez‐Morales, E., & Freire, J. (2008) · Fisheries Oceanography · doi:10.1111/j.1365-2419.2008.00463.x · Cited by 25
A Lagrangian study of surface pCO2 dynamics in the eastern equatorial Pacific Ocean
DeGrandpre, M., Wanninkhof, R., McGillis, W., & Strutton, P. (2004) · doi:10.1029/2003jc002089 · Cited by 29
“Sea surface pCO2-SST relationships have been extensively examined in the equatorial Pacific [e.g., Boutin et al., 1999; Chavez et al., 1999; Cosca et al., 2003].”
BackgroundSelf-citationThe US JGOFS Synthesis and Modeling Project – An introduction
Doney, S., Kleypas, J., Sarmiento, J., & Falkowski, P. (2001) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(01)00092-3 · Cited by 29
“For example, Christian et al. (2002a) (Pacific regional model) and Gregg (2002) (global model) successfully simulate the large biological signals in the tropical Indo-Pacific associated with ENSO (Chavez et al., 1999).”
BackgroundRoussillon, J., Fablet, R., Gorgues, T., Drumetz, L., Littaye, J., & Martinez, E. (2023) · Frontiers in Marine Science · doi:10.3389/fmars.2023.1077623 · Cited by 28
“…the fi rst Chl OC-CCI EOF mode illustrates the strong spatio-temporal signature of ENSO events observed in the Paci fi c Ocean (Figure 6C), with opposite Chl responses to ENSO-related physical anomalies observed in the eastern Paci fi c compared to the western Paci fi c (Chavez et al., 1999).”
BackgroundXiu, P., Dai, M., Chai, F., Zhou, K., Zeng, L., & Du, C.-J. (2018) · Limnology and Oceanography · doi:10.1002/lno.11055 · Cited by 28
“The variability in tropical Pacific Chl primarily arises from the modification of the east–west thermocline slope during the El Niño–Southern Oscillation (ENSO) (e.g., Chavez et al. 1999; Wang et al. 2009; Schollaert Uz et al. 2017).”
BackgroundRosset, S. L., D'Angelo, C., & Wiedenmann, J. (2015) · Frontiers in Marine Science · doi:10.3389/fmars.2015.00103 · Cited by 28
“…coral die-off at Galapagos when the El Niño Southern Oscillation (ENSO)-mediated reduction of major upwelling resulted in nutrient deficiency (Chavez et al., 1999) and an associated drop in surface water productivity in combination with exceptionally high water temperatures (Riegl et al.,…”
BackgroundOcean chlorophyll response to two types of El Niño events in an ocean‐biogeochemical coupled model
Lee, K., Yeh, S., Kug, J., & Park, J. (2014) · Journal of Geophysical Research Oceans · doi:10.1002/2013jc009050 · Cited by 35
Biogeochemical impact of a model western iron source in the Pacific Equatorial Undercurrent
Slemons, L. O., Gorguès, T., Aumont, O., Menkès, C., & Murray, J. W. (2009) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2009.08.005 · Cited by 35
“Variability in iron fields is expected, both from variations in transport of the EUC on interannual (ENSO) and decadal timescales (Chavez et al., 1999; Le Qu er e et al., 2003; Le Borgne et al., 2002; Rodgers et al., 2008) and from variations in candidate sources, like the strength and depth of the…”
BackgroundThe impact of equatorial Pacific tropical instability waves on hydrography and nutrients: 2004-2005
Strutton, P., Palacz, A., Dugdale, R., Chai, F., Marchi, A., Parker, A., Hogue, V. E., & Wilkerson, F. (2011) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/j.dsr2.2010.08.015 · Cited by 27
“El Niño events occur every 3 to 7 years and are characterized by warmer sea surface temperatures (SSTs), weak or absent equatorial upwelling, reduced primary productivity and a smaller ocean to atmosphere CO2 flux (Chavez et al., 1999; McPhaden, 1999).”
BackgroundSelf-citationMessié, M., Radenac, M., Lefèvre, J., & Marchesiello, P. (2006) · doi:10.1029/2006gl026033 · Cited by 27
The Transboundary Nature of Seabird Ecology
Jodice, P., & Suryan, R. (2010) · Springer eBooks · doi:10.1007/978-90-481-9575-6_8 · Cited by 27
“…El Niño-Southern Oscillation) affect currents, temperature, and prey availability (i.e., distribution and abundance) thousands of kilometers away in the North and South Pacific and beyond (including terrestrial habitats over the Americas and Asia; Black et al. 2009; Chavez et al. 1999, 2003).”
BackgroundSantoro, C., Gayo, E., Carter, C., Standen, V., Castro, V., Valenzuela, D., Pol-Holz, R. D., Marquet, P., & Latorre, C. (2017) · Frontiers in Earth Science · doi:10.3389/feart.2017.00077 · Cited by 26
“Indeed, the impacts of ENSO across the Pacific rely on large-scale oceanographicatmospheric perturbations that are rapidly and consistently transmitted along the Pacific coast of South America at interannual timescales (Chavez et al., 1999).”
BackgroundInfluentialSlow science: the value of long ocean biogeochemistry records
Henson, S. (2014) · Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences · doi:10.1098/rsta.2013.0334 · Cited by 26
Messié, M., & Chávez, F. P. (2013) · Journal of Geophysical Research Oceans · doi:10.1002/jgrc.20278 · Cited by 27
Self-citationMacías, D., Franks, P., Ohman, M., & Landry, M. (2012) · doi:10.1016/j.jmarsys.2011.11.011 · Cited by 26
“This climatic pattern emerges as the 2nd dominant mode of sea surface height variability in the Northeast Pacific and is well correlated with upwelling intensity and primary production along the California coast.”
BackgroundInfluential
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
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