북동태평양 적도 Thermocline Ridge 해역에서 영양염(질소, 인, 규소)과 유기탄소(용존 및 입자)의 분포 특성 및 연간 변화
Distribution and Inter-annual Variation of Nutrients (N, P, Si) and Organic Carbon (DOC, POC) in the Equatorial Thermocline Ridge, Northeast Pacific
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The distribution and inter-annual variation of nutrients (N, P, Si) and dissolved/particulate organic carbon were investigated in the equatorial thermocline ridge (7o~11.5oN, 131.5oW) of the northeast Pacific. From the Oceanic Nino Index and Multivariate ENSO Index provided by NOAA, normal condition was observed in July 2003 and August 2005 on the aspect of global climate/ocean change. However, La Niña and El Niño episodes occurred in July 2007 and August 2009, respectively. Thermocline ridge in the study area was located at 9oN in July 2003, 8oN in August 2005, 10oN in July 2007, and 10.5oN in August 2009 under the influence of global climate/ocean change and surface current system (North Equatorial Counter Current and North Equatorial Current) of the northeast Pacific. Maximum depth integrated values (DIV) of nutrients in the upper layer (0~100 m depth range) were shown in July 2007 (mean 21.12 gN/m2, 4.27 gP/m2, 33.72 gSi/m2) and higher variability of DIV in the equatorial thermocline ridge was observed at 10oN during the study periods. Also, maximum concentration of dissolved organic carbon (DOC) in the upper 50 m depth layer was observed in July 2007 (mean 107.48±14.58 μM), and particulate organic carbon (POC, mean 9.42±3.02 μM) was similar to that of DOC. Nutrient concentration in the surface layer increased with effect of upwelling phenomenon in the equatorial thermocline ridge and La Niña episode, which had formed in the central Pacific. This process also resulted in the increasing of organic carbon concentration (DOC and POC) in the surface layer. From these results, it is suggested that spatial and temporal variation of chemical and biological factors were generated by physical processes in the equatorial thermocline ridge.
Abstract
The distribution and inter-annual variation of nutrients (N, P, Si) and dissolved/particulate organic carbon were investigated in the equatorial thermocline ridge (7o~11.5oN, 131.5oW) of the northeast Pacific. From the Oceanic Nino Index and Multivariate ENSO Index provided by NOAA, normal condition was observed in July 2003 and August 2005 on the aspect of global climate/ocean change. However, La Niña and El Niño episodes occurred in July 2007 and August 2009, respectively. Thermocline ridge in the study area was located at 9oN in July 2003, 8oN in August 2005, 10oN in July 2007, and 10.5oN in August 2009 under the influence of global climate/ocean change and surface current system (North Equatorial Counter Current and North Equatorial Current) of the northeast Pacific. Maximum depth integrated values (DIV) of nutrients in the upper layer (0~100 m depth range) were shown in July 2007 (mean 21.12 gN/m2, 4.27 gP/m2, 33.72 gSi/m2) and higher variability of DIV in the equatorial thermocline ridge was observed at 10oN during the study periods. Also, maximum concentration of dissolved organic carbon (DOC) in the upper 50 m depth layer was observed in July 2007 (mean 107.48±14.58 μM), and particulate organic carbon (POC, mean 9.42±3.02 μM) was similar to that of DOC. Nutrient concentration in the surface layer increased with effect of upwelling phenomenon in the equatorial thermocline ridge and La Niña episode, which had formed in the central Pacific. This process also resulted in the increasing of organic carbon concentration (DOC and POC) in the surface layer. From these results, it is suggested that spatial and temporal variation of chemical and biological factors were generated by physical processes in the equatorial thermocline ridge.
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