首页> 外文期刊>Journal of Oceanography and Marine Science >On the influence of interseasonal sea surface temperature on surface water pCO2 at 49.0N/16.5W and 56.5N/52.6W in the North Atlantic Ocean
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On the influence of interseasonal sea surface temperature on surface water pCO2 at 49.0N/16.5W and 56.5N/52.6W in the North Atlantic Ocean

机译:北大西洋49.0N / 16.5W和56.5N / 52.6W季节间海表温度对地表水pCO2的影响

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The sea surface temperature (SST) and partial pressure of carbon dioxide (pCO2) derived from hourly in situ measurements at Northwest (56.5°N, 52.6°W) and Northeast (49.0°N, 16.5°W) subpolar sites of the Atlantic Ocean from 2003 – 2005 were employed to investigate the seasonal pCO2–SST relationship. The results indicate weak to moderately strong significant negative relationships (r = -0.04 to -0.89, p0.0001) and (r = -0.56 to -0.97, p0.0001) between SST and pCO2 for the Northeast and Northwest observed data respectively. At the Northwestern site, the variation in surface water pCO2 might be partly controlled by the seasonal change in SST as well as biological activities and other physical processes. The variability in pCO2 distribution at the Northeastern oceanographic site were attributed principally to mixing and stratification processes during the autumn and spring seasons, while the pCO2–SST interrelationship obtained during summertime suggested that pCO2 variability could have been induced mainly by thermodynamic effects.
机译:每小时西北大西洋(56.5°N,52.6°W)和东北(49.0°N,16.5°W)亚极站点的原位测量得出的海表温度(SST)和二氧化碳分压(pCO2)从2003年至2005年,我们调查了季节性pCO2与SST的关系。结果表明,分别在东北和西北观测数据中,SST和pCO2之间存在弱到中等强的显着负相关(r = -0.04至-0.89,p <0.0001)和(r = -0.56至-0.97,p <0.0001)。在西北地区,地表水pCO2的变化可能部分受到SST季节变化以及生物活动和其他物理过程的控制。东北海洋站点pCO2分布的变化主要归因于秋季和春季的混合和分层过程,而夏季获得的pCO2-SST相互关系表明,pCO2的变化可能主要是由热力学效应引起的。

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