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首页> 外文期刊>Frontiers in Marine Science >Subsurface Ocean Warming Hotspots and Potential Impacts on Marine Species: The Southwest South Atlantic Ocean Case Study
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Subsurface Ocean Warming Hotspots and Potential Impacts on Marine Species: The Southwest South Atlantic Ocean Case Study

机译:地下海洋变暖热点及对海洋物种的潜在影响:西南南大西洋案例研究

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In the southwest South Atlantic Ocean (SWAO) strong ocean surface warming hotspots have been observed mainly along the path of the Brazil Current (BC), Brazil-Malvinas Confluence (BMC), and in the Río de la Plata (RdlP). However, there is no knowledge about the signature of ocean hotspots below the surface and the potential effects of ocean warming on marine biota. In this work, we provide initial evidence of how deep the hotspots of the SWAO extend in the water column, in particular at mid-water and bottom layers where two marine species ?the green turtle (Chelonia mydas) and the Patagonian scallop (Zygochlamys patagonica)? inhabit. We compare 15 years (2003–2017) of Copernicus Marine Environment Monitoring Service (CMEMS) ARMOR3D high‐resolution (1/4°) 3-D temperatures reprocessed from combined satellite and in-situ observations with high‐resolution (1/12°) Mercator ocean reanalysis. We also use location data of C. mydas and Z. patagonica to discuss the potential impacts of warming on these species in terms of geographic distribution, phenological shifts and thermal tolerance. The potential distribution of C. mydas changes in relation to the sea surface temperature (SST) and the bathymetry. The warming of the whole water column in the RdlP ( 0.4°C/decade) and the southward movement of the mean surface isotherms, which likely drove turtle displacements, could enable the opening up of novel optimal thermal habitats and/or a longer seasonal residency for the species. At the BMC, warming is driven by the southward displacement of the BC during the past decades. Ocean model temperature indicates cooling/warming in deep waters along the outer shelf and shelf break regions, which vary according the displacements of the BMC. The expected warming of the waters over the Patagonian scallop largest bed could exceed the thermal tolerance of this species and its survival. Given the lack of long-term monitoring programs to address the impacts of climate change on marine biota in the SWAO, our results provide the first effort to call the attention of stakeholders and decision makers on marine conservation and fishery management to work towards better management strategies in the context of climate change.
机译:在西南大西洋(萨瓦)强烈的海洋表面温暖热点主要沿着巴西当前(BC),巴西 - Malvinas汇合(BMC)以及RíoDaPlata(RDLP)的路径观察。然而,没有关于海洋热点签名的知识以及海洋生物群海洋暖的潜在影响。在这项工作中,我们提供了雄性柱延伸的热点的初始证据,特别是在中水和底层,其中两种海洋物种?绿龟(Chelonia Mydas)和巴塔哥尼亚·扇贝(ZygoChlamys Patagonica )?居住于。我们比较哥白尼海洋环境监测服务(CMEMS)ARMOR3D高分辨率(1/4°)3-D温度,从组合卫星和原位观察的高分辨率(1/4°)的高分辨率(1/12°) )Mercator Ocean Reanalysis。我们还使用C. Mydas和Z.Potagonica的位置数据,以讨论在地理分布,鉴生素质和耐热性方面对这些物种的潜在影响。 C. Mydas的潜在分布与海面温度(SST)和碱度相比变化。在RDLP(> 0.4°C /十年)中的整个水柱的变暖和平均表面等温度的南方运动可能使龟位移能够开放新颖的最佳热栖息地和/或更长的季节性居住物种。在BMC,在过去的几十年中,BC的南向位移是推动的。海洋模型温度表示沿着外部搁板和货架断开区域在深水中冷却/升温,因此根据BMC的位移而变化。水域在巴塔哥数最大床上的预期升温可能超过该物种的热耐受性及其存活率。鉴于缺乏长期监测方案来解决气候变化对萨瓦的海洋生物田的影响,我们的结果提供了第一次呼吁利益相关者和决策者对海洋保护和渔业管理的关注,以促进更好的管理策略在气候变化的背景下。

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