通过 RemoTe 传感(EXPORTS)实地活动评估北大西洋海洋出口过程中的海洋状况

IF 3.8 3区 地球科学 Q1 OCEANOGRAPHY
Leah Johnson , David A. Siegel , Andrew F. Thompson , Erik Fields , Zachary K. Erickson , Ivona Cetinic , Craig M. Lee , Eric A. D'Asaro , Norman B. Nelson , Melissa M. Omand , Michaela Sten , Shawnee Traylor , David P. Nicholson , Jason R. Graff , Deborah K. Steinberg , Heidi M. Sosik , Ken O. Buesseler , Mark A. Brzezinski , Inia Soto Ramos , Filipa Carvalho , Stephanie A. Henson
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引用次数: 0

摘要

本手稿概述了美国国家航空航天局(NASA)在北大西洋开展的 "2021 年北大西洋遥感海洋出口过程"(EXPORTS NA)实地活动,并对研究期间调节水体变化的物理过程进行了定量和动态描述。该计划的一个主要目标是以拉格朗日模式进行采样,以便观测到独立于物理平流过程的海洋生态和生物地球化学变化。为实现这一目标,EXPORTS NA 在一个有韧性的反气旋模式水涡中开展了多船、多资产实地取样计划。在整个实验过程中,拉格朗日取样设备始终停留在漩涡核心水域(ECWs)的水下 100 米深处,表明模式水漩涡内的 ECWs 具有潴留作用。然而,四次暴风雨带来的强西风将漩涡模式水核心上方表层核心水(SCWs)的混合层(ML)加深了 25-40 米,并通过埃克曼传输将部分 SCWs 与漩涡外的表层水交换。冲刷时间估计为 5 到 8 天,表层交换率为 20% 到 75%,与地转和 Ekman 速度共同作用下的颗粒跟踪平流相一致。水平和垂直平流对 ECW 示踪剂变化的相对贡献取决于该示踪剂的水平和垂直梯度。例如,水平平流对 ECW 盐度通量的影响较大,而垂直夹带对进入 SCW ML 的营养物质通量的影响较大。每次风暴都会将营养物和低氧水注入海洋底质,之后表层海洋生态系统会作出反应,降低营养物浓度,提高氧气饱和度。总体而言,ECW 的叶绿素和 POC 值在实地考察开始时最大,并在整个考察过程中下降。所做的分析为 EXPORTS NA 实地考察期间所做的许多测量提供了一个物理海洋学背景,同时说明了即使在拉格朗日框架下进行生产-通量实验所面临的许多挑战,以及解释在欧拉参考框架下收集的生物碳泵观测数据所固有的不确定性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of oceanographic conditions during the North Atlantic EXport processes in the ocean from RemoTe sensing (EXPORTS) field campaign

This manuscript presents an overview of NASA’s EXport Processes in the Ocean from Remote Sensing 2021 Field Campaign in the North Atlantic (EXPORTS NA) and provides quantitative and dynamical descriptions of the physical processes modulating water transformations during the study. A major programmatic goal was to conduct the sampling in a Lagrangian mode so that ocean ecological and biogeochemical changes can be observed independent from physical advective processes. To accomplish this goal, EXPORTS NA conducted a multi-ship, multi-asset field sampling program within a retentive, anticyclonic mode water eddy. Beneath depths of ∼ 100 m, Lagrangian sampling assets remained within the eddy core waters (ECWs) throughout the experiment, demonstrating that the ECWs within the mode water eddy were retentive. However, strong westerly winds from four storm events deepened the mixed layer (ML) of the surface core waters (SCWs) above the eddy’s mode water core by 25–40 m and exchanged some of the SCWs with surface waters outside of the eddy via Ekman transport. Estimates of flushing times ranged from 5 to 8 days, with surface exchange fractions ranging from 20 to 75 % and were consistent with particle tracking advected by combined geostrophic and Ekman velocities. The relative contributions of horizontal and vertical advection on changes in ECW tracers depended on the horizontal and vertical gradients of that tracer. For example, horizontal advection played a large role in ECW salinity fluxes, while vertical entrainment played a larger role in the fluxes of nutrients into SCW ML. Each storm injected nutrients and low oxygen waters into the ML, after which the surface ocean ecosystem responded by reducing nutrient concentrations and increasing %O2 saturation levels. Overall, ECW values of chlorophyll and POC were the largest at the onset of the field program and decreased throughout the campaign. The analysis presented provides a physical oceanographic context for the many measurements made during the EXPORTS NA field campaign while illustrating the many challenges of conducting a production-flux experiment, even in a Lagrangian frame, and the inherent uncertainties of interpreting biological carbon pump observations that were collected in a Eulerian frame of reference.

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来源期刊
Progress in Oceanography
Progress in Oceanography 地学-海洋学
CiteScore
7.20
自引率
4.90%
发文量
138
审稿时长
3 months
期刊介绍: Progress in Oceanography publishes the longer, more comprehensive papers that most oceanographers feel are necessary, on occasion, to do justice to their work. Contributions are generally either a review of an aspect of oceanography or a treatise on an expanding oceanographic subject. The articles cover the entire spectrum of disciplines within the science of oceanography. Occasionally volumes are devoted to collections of papers and conference proceedings of exceptional interest. Essential reading for all oceanographers.
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