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Profiling float-based observations of net respiration beneath the mixed layer

机译:基于浮点的混合层下净呼吸观测

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We employ profiling floats with dissolved oxygen sensors to observe in situ temporal oxygen evolution below the mixed layer, allowing us to characterize net respiration of organic carbon in eight distinct regions over the globe. Export and export efficiency are generally high in locations with strong seasonal variability and low in locations of weak seasonality. Vertically integrated respiration is weakly, yet significantly, correlated with remote observations of chlorophyll, net primary production, and planktonic community size structure. These correlations suggest that regimes of high net primary production and large phytoplankton fuel elevated respiration at depth. Several regions of float-based observations intersect with sites of other detailed observations (e.g., Hawaii and Sargasso Sea), which allows us to compare our results to independent studies. We find that there is good agreement among export production estimates at highly seasonal locations, and that float-based observations may be biased low at weakly seasonal locations. We posit that the reason for the low-latitude discrepancy is the relative steady state of oxygen concentration caused by weak seasonality and shallow wintertime mixed layer depths.
机译:我们使用带有溶解氧传感器的仿形浮标来观察混合层以下的原位瞬时氧气逸出,从而使我们能够表征全球八个不同区域中有机碳的净呼吸。在季节性变化较大的地区,出口和出口效率通常较高,在季节性较弱的地区,出口和出口效率较低。垂直整合的呼吸与叶绿素,净初级生产力和浮游生物群落大小结构的远距离观测相关,但微弱但显着。这些相关性表明,高净初级生产力和大型浮游植物的燃料消耗增加了深度呼吸。基于浮点的观测的几个区域与其他详细观测的站点(例如,夏威夷和Sargasso海)相交,这使我们可以将结果与独立研究进行比较。我们发现,在季节性旺盛的地区,出口估计的产量之间存在很好的一致性,在季节性较弱的地区,基于浮动的观测值可能偏低。我们认为,低纬度差异的原因是由季节性弱和冬季混合层深度较浅引起的氧浓度相对稳定状态。

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