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First Autonomous Bio-Optical Profiling Float in the Gulf of Mexico Reveals Dynamic Biogeochemistry in Deep Waters

机译:墨西哥湾的第一个自主生物光学剖面浮标揭示了深水中的动态生物地球化学

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摘要

Profiling floats equipped with bio-optical sensors well complement ship-based and satellite ocean color measurements by providing highly-resolved time-series data on the vertical structure of biogeochemical processes in oceanic waters. This is the first study to employ an autonomous profiling (APEX) float in the Gulf of Mexico for measuring spatiotemporal variability in bio-optics and hydrography. During the 17-month deployment (July 2011 to December 2012), the float mission collected profiles of temperature, salinity, chlorophyll fluorescence, particulate backscattering (bbp), and colored dissolved organic matter (CDOM) fluorescence from the ocean surface to a depth of 1,500 m. Biogeochemical variability was characterized by distinct depth trends and local “hot spots”, including impacts from mesoscale processes associated with each of the water masses sampled, from ambient deep waters over the Florida Plain, into the Loop Current, up the Florida Canyon, and eventually into the Florida Straits. A deep chlorophyll maximum (DCM) occurred between 30 and 120 m, with the DCM depth significantly related to the unique density layer ρ = 1023.6 (R2 = 0.62). Particulate backscattering, bbp, demonstrated multiple peaks throughout the water column, including from phytoplankton, deep scattering layers, and resuspension. The bio-optical relationship developed between bbp and chlorophyll (R2 = 0.49) was compared to a global relationship and could significantly improve regional ocean-color algorithms. Photooxidation and autochthonous production contributed to CDOM distributions in the upper water column, whereas in deep water, CDOM behaved as a semi-conservative tracer of water masses, demonstrating a tight relationship with density (R2 = 0.87). In the wake of the Deepwater Horizon oil spill, this research lends support to the use of autonomous drifting profilers as a powerful tool for consideration in the design of an expanded and integrated observing network for the Gulf of Mexico.
机译:配备生物光学传感器的仿形浮标通过提供关于海洋水域生物地球化学过程垂直结构的高度解析的时间序列数据,很好地补充了船基和卫星海洋颜色测量。这是第一项在墨西哥湾采用自动剖析(APEX)浮标来测量​​生物光学和水文学中时空变化的研究。在为期17个月的部署期间(2011年7月至2012年12月),浮动任务收集了从海面到深处的温度,盐度,叶绿素荧光,颗粒反向散射(bbp)和有色溶解有机物(CDOM)荧光的剖面图。 1,500米生物地球化学变异性的特征是明显的深度趋势和局部“热点”,包括中尺度过程与每个采样水团相关的影响,这些过程涉及从佛罗里达平原上的周围深水,环流,佛罗里达峡谷直至最终进入佛罗里达海峡。一个深叶绿素最大值(DCM)出现在30至120 m之间,而DCM深度与唯一密度层ρ= 1023.6(R 2 = 0.62)显着相关。颗粒反向散射bbp在整个水柱中都显示出多个峰,包括浮游植物,深层散射层和重悬物。将bbp与叶绿素之间的生物光学关系(R 2 = 0.49)与全局关系进行比较,可以显着改善区域海洋颜色算法。光氧化和自生产物有助于上层水柱中的CDOM分布,而在深水中,CDOM表现为水团的半保守示踪剂,表明其与密度密切相关(R 2 = 0.87) 。在“深水地平线”溢油事故之后,这项研究为使用自动漂移剖面仪作为强大的工具提供了支持,这是为墨西哥湾设计扩展和集成的观测网络时要考虑的因素。

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