Influence of strong El Nino on sinking particle fluxes in the 10N thermocline ridge of the northeastern equatorial Pacific
DC Field | Value | Language |
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dc.contributor.author | 김형직 | - |
dc.contributor.author | 형기성 | - |
dc.contributor.author | 유찬민 | - |
dc.contributor.author | 김부근 | - |
dc.date.accessioned | 2020-07-16T13:51:39Z | - |
dc.date.available | 2020-07-16T13:51:39Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2011-12-05 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/27994 | - |
dc.description.abstract | The influence of ENSO (El Niño -Southern Oscillation) variability on sinking particle fluxes was evaluated from time series sediment trap experiments carried out for 8 years from July 1997 – May 1998 and from July 2003 – June 2010 at a station (10°30′N, 131°20´W) located in the 10°N thermocline ridge (9°-13°N, 105°-140°W) of the northeastern equatorial Pacific. During the monitoring period, two strong El Niño events were observed from July 1997 to May 1998 (1997/98 El Niño) and from June 2009 to April 2010 (2009/10 El Niño) that occurred as a cold-tong (CT)-type and warm-pool (WP)-type El Niño, respectively, with SST anomalies centered in eastern equatorial and central equatorial Pacific. Regardless of El Niño types, both events caused almost 3-fold increases of total mass fluxes compared to the average total mass flues of non-ENSO period, which is completely opposite to the general trend observed in the central and eastern equatorial Pacific region. In detail, however, the 1997/98 El Niño event resulted in the most marked increases of biogenic silica and organic carbon fluxes to two to three times higher than non-ENSO level, while the 2009/10 El Niño was accompanied by a significant increase of CaCO3 flux with minor increases in biogenic silica and organic carbon fluxes. The observed meteorological and ocean gy | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | American | - |
dc.relation.isPartOf | AGU fall meeting 2011 | - |
dc.title | Influence of strong El Nino on sinking particle fluxes in the 10N thermocline ridge of the northeastern equatorial Pacific | - |
dc.type | Conference | - |
dc.citation.conferencePlace | US | - |
dc.citation.endPage | 1 | - |
dc.citation.startPage | 1 | - |
dc.citation.title | AGU fall meeting 2011 | - |
dc.contributor.alternativeName | 김형직 | - |
dc.contributor.alternativeName | 형기성 | - |
dc.contributor.alternativeName | 유찬민 | - |
dc.identifier.bibliographicCitation | AGU fall meeting 2011, pp.1 | - |
dc.description.journalClass | 1 | - |