利用实地考察获得的现场数据确定哥斯达黎加东热带太平洋氧气最少区(OMZ)的特征

Alejandro Rodríguez, Erick J. Alfaro, Jorge Cortés
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引用次数: 0

摘要

为了保护和可持续渔业,通过分析温度、盐度、密度和氧气剖面,确定哥斯达黎加东热带太平洋(ETP)甲烷渗漏区及其周围的氧气最小区(OMZ)的特征非常重要。这项工作中使用的数据是 2009 年至 2019 年期间在太平洋大陆边缘和哥斯达黎加近海的几次海洋研究活动中收集的,使用 CTDs 作为水柱物理参数剖面仪。总体而言,观察到溶解氧随着深度的增加而逐渐减少,直至温跃层,然后溶解氧浓度迅速下降并保持在较低水平,这表明存在OMZ,并在更深的深度略有增加。甲烷渗漏附近和周围的 OMZ 平均垂直延伸深度为 763 米,最小溶解氧值的平均深度为 393 米。总体而言,在混合层内观察到的氧气异常值变化较大,而在温跃层下,氧气异常值保持稳定,约为零。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterizing the Oxygen Minimum Zone (OMZ) in the Costa Rican Eastern Tropical Pacific using in situ data from field campaigns
For conservation and sustainable fisheries, it is important to characterize the Oxygen Minimum Zones or OMZ in and around the methane seeps of the Eastern Tropical Pacific (ETP), Costa Rica, through the analysis of temperature, salinity, density, and oxygen profiles. The data used in this work were collected during several oceanographic research campaigns in the Pacific continental margin and offshore of Costa Rica, between 2009 and 2019, using a CTDs, as the profiler of physical parameters of the water column. In general, it was observed that dissolved oxygen gradually decreases with depth to the thermocline, then its concentration decreases more rapidly and remains low, indicating the presence of the OMZ and tends to increase slightly at greater depths. Mean vertical extension of the OMZ near and around the seeps was 763 m and the mean depth for the minimum dissolved oxygen value was 393 m. Spatial differences of measurements taken at stations near the methane seeps were calculated with respect to the measurements at the station located above them. Overall, a greater variability of the oxygen anomalies was observed within the mixed layer, while under the thermocline their values remain stable and around zero.
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