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Marine Socio-Environmental Covariates: queryable global layers of environmental and anthropogenic variables for marine ecosystem studies

机译：海洋社会环境协变量：海洋生态系统研究的疑问全球环境和人为变量

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Lauren A. Yeager; Philippe Marchand; David A. Gill; Julia K. Baum; Jana M. McPherson;
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1. Comparing Apples to Oranges: Common Trends and Thresholds in Anthropogenic and Environmental Pressures across Multiple Marine Ecosystems [J] . Tam Jamie C., Link Jason S., Large Scott I., Frontiers in Marine Science . 2017,第1期

机译：苹果与橙子的比较：跨多个海洋生态系统的人为压力和环境压力的共同趋势和阈值
2. Evaluating and ranking the vulnerability of global marine ecosystems to anthropogenic threats [J] . Halpern BS, Selkoe KA, Micheli F, Conservation Biology . 2007,第5期

机译：评估和排名全球海洋生态系统对人为威胁的脆弱性
3. An evaluation of Tokyo Bay as a marine space for Porphyra spp. farming: Evaluating marine spaces through quantitative examination of water environmental variables across categorized marine spaces, making use of multiple institutional data [J] . Wakita Kazumi, Yamakita Takehisa, Yamada Katsumasa, 日本水産学会誌 . 2014,第5期

机译：对东京湾作为紫菜属海洋空间的评估。农业：利用多种机构数据，通过对分类海洋空间内水环境变量进行定量检查，评估海洋空间
4. The decline of the southern sea otter (Enhyrda lutris nereis): is it an indicator of contaminant and pathogen pollution, anthropogenic interference, and declining marine ecosystem health? [C] . David A. Jessup, Milissa Chechowitz, Jack Ames Annual Conference of the American Association of Zoo Veterinarians . 2000

机译：南海水獭（苏格拉·卢特里斯Nereis）的衰落：它是污染物和病原体污染，人为干扰和海洋生态系统健康下降的指标吗？
5. Fishers, parks, and power: The socio-environmental dimensions of marine resource decline and protection on the Kenya coast [D] . Glaesel, Heidi 1997

机译：渔民，公园和权力：肯尼亚海岸海洋资源减少和保护的社会环境层面
6. Marine Viruses: Key Players in Marine Ecosystems [O] . Mathias Middelboe, Corina P. D. Brussaard 2017

机译：海洋病毒：海洋生态系统中的关键角色
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

Marine Socio-Environmental Covariates: queryable global layers of environmental and anthropogenic variables for marine ecosystem studies

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