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Using Autonomous Vehicles to Estimate Vertical Fluxes and Remineralization Rates of Particulate Organic Matter in the Ocean: A Conceptual Approach

机译:使用自主车辆估算海洋中颗粒有机质的垂直助熔剂和再矿化率:概念方法

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Autonomous vehicles are able to sample continuously and over different spatial and temporal scales. They routinely determine biological properties, such as phytoplankton fluorescence and optical backscatter. Using appropriate calibration samples taken in close proximity to the vehicles, these properties can be converted to absolute quantities of chlorophyll and particulate organic carbon (POC), respectively. By sampling through time in a relatively uniform and restricted area, the vertical distributions of particulate organic carbon can be determined, and when coupled to an estimate of surface phytoplankton production, an estimate of the vertical flux of carbon can be made from the changes in POC through time. These flux estimates in turn can be used to determine the extent of remineralization within the water column. Such remineralization rates are difficult to determine using alternative sampling techniques, and using autonomous vehicles in this manner can greatly improve our understanding of the rates of vertical flux of organic matter from the upper layers of the ocean to the deep sea, as well as the time varying rates of remineralization. These data can then provide critical inputs into global carbon cycle estimates and the role of the ocean in sequestering carbon.
机译:自治车辆能够连续和在不同的空间和时间尺度上进行样品。它们常规确定生物学性质,例如浮游植物荧光和光学反向散射。使用适当的校准样品靠近车辆,可以分别转化为绝对量的叶绿素和颗粒状有机碳(PoC)的绝对量。通过在相对均匀和限制的区域中取出时间,可以确定颗粒状有机碳的垂直分布,并且当与表面浮游植物产生的估计相结合时,可以从POC的变化进行碳的垂直通量的估计通过时间。这些助焊剂估计又可以用于确定水柱内的再矿化程度。这种倒立率难以确定使用替代采样技术,并以这种方式使用自主车辆可以大大提高我们对从海洋上层到深海的有机物质的垂直通量速率的理解,以及时间不同的再矿化率。然后,这些数据可以向全局碳循环估计和海洋在螯合碳中的作用提供关键输入。

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