1996
DOI: 10.1016/0967-0645(96)00035-5
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Primary productivity and its regulation in the equatorial Pacific during and following the 1991–1992 El Niño

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Cited by 226 publications
(125 citation statements)
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“…In agreement with Longhurst (1998), Radhakrishna et al (1978), Nair and Pillai (1983) and Jochem et al (1993) report mean values around 60 mmol C m\ d\ for the NE Monsoon and Intermonsoon periods; and, while 60 mmol C m\ d\ is low compared to SW Monsoon primary productivity values, it is high relative to other areas of the tropical and temperate ocean (Barber et al, 1996;Karl et al, 1996). For example, the tropical Paci"c Ocean in 1992 had mean values of 29 mmol C m\ d\ north and south of the equatorial zone, and even the enriched equatorial Paci"c zone of 103N } 103S had a mean of only 52$7 mmol C m\ d\ (Barber et al, 1996). Thus Longhurst's (1998) 60 mmol C m\ d\ prediction is a relatively high level of productivity for an o!shore region that was considered to be oligotrophic for the non-SW Monsoon period of the year (Smith, 1991).…”
Section: Primary Productivity During the Non-sw Monsoon Periodsupporting
confidence: 62%
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“…In agreement with Longhurst (1998), Radhakrishna et al (1978), Nair and Pillai (1983) and Jochem et al (1993) report mean values around 60 mmol C m\ d\ for the NE Monsoon and Intermonsoon periods; and, while 60 mmol C m\ d\ is low compared to SW Monsoon primary productivity values, it is high relative to other areas of the tropical and temperate ocean (Barber et al, 1996;Karl et al, 1996). For example, the tropical Paci"c Ocean in 1992 had mean values of 29 mmol C m\ d\ north and south of the equatorial zone, and even the enriched equatorial Paci"c zone of 103N } 103S had a mean of only 52$7 mmol C m\ d\ (Barber et al, 1996). Thus Longhurst's (1998) 60 mmol C m\ d\ prediction is a relatively high level of productivity for an o!shore region that was considered to be oligotrophic for the non-SW Monsoon period of the year (Smith, 1991).…”
Section: Primary Productivity During the Non-sw Monsoon Periodsupporting
confidence: 62%
“…9 and 10). P in the "lament was 14.72 mmol C mg Chl a\ d\ (Table 2), a value considerably higher than those observed during EqPac (Barber et al, 1996), NABE (Chipman et al, 1993) or the Southern Ocean (Smith et al, in press). Clearly, the "lament supported both high speci"c rates and high biomass accumulation.…”
Section: Filaments and Eddiesmentioning
confidence: 78%
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