Ocean surface slicks-pollution, productivity, climate and life-saving

机译：海洋表面浮油-污染，生产力，气候和救生

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Reviews the physical mechanisms relevant to slicks; their observation; their role in complicating pollution detection; and their potential uses for ocean and climate studies. The multi-disciplinary nature of slicks research-needing expertise from organic chemistry through colloid physics and fluid mechanics to radar imaging-makes it a particularly interesting and challenging field of research.

机译：审查与浮油有关的物理机制;他们的观察;它们在使污染检测复杂化方面的作用;及其在海洋和气候研究中的潜在用途。浮油的多学科性质，需要从有机化学到胶体物理学，流体力学到雷达成像等领域的研究专业知识，使其成为一个特别有趣且具有挑战性的研究领域。

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《Geoscience and Remote Sensing Symposium, 1999. IGARSS '99 Proceedings. IEEE 1999 International》|1999年|P.1463-1468|共6页
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Scott; J.C.;
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中图分类无线电电子学、电信技术;
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1. Climate-induced primary productivity change and fishing impacts on the Central North Pacific ecosystem and Hawaii-based pelagic longline fishery. (Special Issue: Climate and oceanic fisheries.) [J] . Howell E. A., Wabnitz C. C. C., Dunne J. P., Climatic Change . 2013,第1期

机译：气候导致的初级生产力变化以及捕鱼对中北部太平洋生态系统和夏威夷中上层延绳钓渔业的影响。（特刊：气候和海洋渔业。）
2. Respiration of new and old carbon in the surface ocean: Implications for estimates of global oceanic gross primary productivity [J] . Carvalho Matheus C., Schulz Kai G., Eyre Bradley D. Global Biogeochemical Cycles . 2017,第6期

机译：表面海洋中新碳呼吸的呼吸：全球海洋总初级生产力估计的含义
3. Book reviews - Climatic Atlas of the Indian Ocean Part I: Surface Climate and Atmospheric Circulation; Part II: The Oceanic Heat Budget (Stefan Hasternrath and Peter J. Lamb), Rainbows, Halos, and Glories (Robert Greenler), The Hurricane and Its Impact (Robert H. Simpson) [J] . Not available Australian Meteorological Oceanographic Journal: Southern hemisphere journal of atmospheric, oceanic and related sciences . 1981,第4期

机译：书评-印度洋气候地图集第一部分：地表气候和大气环流;第二部分：海洋热收支（Stefan Hasternrath和Peter J. Lamb），彩虹，光晕和荣耀（罗伯特·格林勒），飓风及其影响（罗伯特·辛普森）
4. Ocean surface slicks-pollution, productivity, climate and life-saving [C] . Scott J.C., Institute of Electric and Electronic Engineer IEEE International Geoscience and Remote Sensing Symposium . 1999

机译：海面光滑污染，生产力，气候和救生
5. MODES OF SURFACE CIRCULATION AND CLIMATE OVER THE TROPICAL ATLANTIC, EASTERN PACIFIC, AND INDIAN OCEANS. [D] . WOLTER, KLAUS (EDUARD). 1987

机译：热带大西洋，东太平洋和印度洋的地表环流和气候模式。
6. From the Cover: Climate change decouples oceanic primary and export productivity and organic carbon burial [O] . Cristina Lopes, Michal Kucera, Alan C. Mix 2015

机译：从封面看：气候变化使海洋初级生产力和出口生产力与有机碳埋葬脱钩
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。

Ocean surface slicks-pollution, productivity, climate and life-saving

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