[A-OS16] 海洋化学・生物学

[AOS16-P03] 太平洋熱帯域における表層CO₂分圧・栄養塩の季節・経年変動

*安中 さやか¹、纐纈 慎也¹、P.G. Strutton²、A.J. Sutton³、村田 昌彦¹、中岡 慎一郎⁴、野尻 幸宏⁴ (1.国立研究開発法人　海洋研究開発機構、2.University of Tasmania、3.NOAA、4.NIES)

We present a synthesis of surface water partial pressure of CO₂ (pCO₂) and nutrient observations in the tropical Pacific from 1981 to 2015. The e-folding scale for interannual variability of pCO₂ is estimated to be 6° in latitude, 13° in longitude, and 2 months with a signal-to-noise ratio of 4. When El Niño occurs, pCO₂ along the equator is reduced due to weakening of the easterly wind and reduced upwelling of CO₂ rich subsurface water. The surface seawater pCO₂ trend is positive in all regions with an area average of 1.8 ± 0.1 μatm/yr. However, along the equator the trend is > 2 μatm/yr linked to the Pacific Decadal Oscillation forcing. Surface nutrient concentrations in the central to eastern tropics along the equator decreased during El Niño periods, but there are not enough data to characterize the trends of nutrients in the tropical Pacific.