The Future of Climate Observations in the Global Ocean

Dr. Dean Roemmich; Dr. W. John Gould

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The Future of Climate Observations in the Global Ocean

机译：全球海洋气候观测的未来

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摘要

Global ocean observations for climate research are a major part of the legacy of the World Climate Research Program's (WCRP) Tropical Ocean Global Atmosphere (TOGA) and World Ocean Circulation Experiment (WOCE).

机译：用于气候研究的全球海洋观测是世界气候研究计划（WCRP）热带海洋全球大气（TOGA）和世界海洋环流实验（WOCE）遗产的重要组成部分。

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《Sea Technology: Worldwide Information Leader for Marine Business, Science & Engineering》 |2003年第8期|共5页
作者
Dr. Dean Roemmich; Dr. W. John Gould;
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正文语种 eng
中图分类海洋学;
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1. Exploiting satellite earth observation to quantify current global oceanic DMS flux and its future climate sensitivity [J] . P. E. Land, J. D. Shutler, T. G. Bell, Journal of Geophysical Research, C. Oceans: JGR . 2014,第11期

机译：利用卫星地球观测来量化当前全球海洋DMS通量及其未来的气候敏感性
2. The Future of Climate Observations in the Global Ocean [J] . Dr. Dean Roemmich, Dr. W. John Gould Sea Technology: Worldwide Information Leader for Marine Business, Science & Engineering . 2003,第8期

机译：全球海洋气候观测的未来
3. A review of global ocean temperature observations: Implications for ocean heat content estimates and climate change [J] . Abraham J.P., Baringer M., Bindoff N.L., Reviews of Geophysics . 2013,第3期

机译：全球海洋温度观测综述：对海洋热量含量估算和气候变化的影响
4. Global change in ocean circulation from satellite sea surface temperature records: implications for the future of coral-reefs, fisheries, and climate change [C] . Goreau T.J., Hayes R.L. Oceans MTS/IEEE Conference . 2003

机译：来自卫星海面温度记录的海洋循环的全球变化：对珊瑚礁，渔业和气候变化未来的影响
5. Observations and modeling of the CO2-carbonic acid system on Hawaiian coral reefs: Implications of future ocean acidification and climate change. [D] . Drupp, Patrick S. 2015

机译：夏威夷珊瑚礁上的CO2-碳酸系统的观测和建模：未来海洋酸化和气候变化的影响。
6. Enabling earth observations in support of global coastal ocean and climate change research and monitoring [O] . Gad Levy, Stefano Vignudelli, Jim Gower -1

机译：启用地球观测以支持全球沿海海洋和气候变化研究与监测
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。
8. Toward the Development of an Ocean Observing System for Climate Study and Prediction. Scientific Rationale for Recommending Long-Term, Systematic Ocean Observations to Monitor the Uptake of CO(sub 2) by the Ocean: Now and in the Future [R] . Merlivat, L., Vezina, A. 1992

机译：迈向气候研究与预测海洋观测系统的发展。推荐长期系统海洋观测的科学依据，以监测海洋对CO（sub 2）的吸收：现在和未来

The Future of Climate Observations in the Global Ocean

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