Global ocean heat content 1955-2008 in light of recently revealed instrumentation problems

S. Levitus; J. I. Antonov; T. P. Boyer; R. A. Locarnini; H. E. Garcia; A. V. Mishonov

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Global ocean heat content 1955-2008 in light of recently revealed instrumentation problems

机译：鉴于最近发现的仪器仪表问题，1955-2008年全球海洋热含量

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We provide estimates of the warming of the world ocean for 1955-2008 based on historical data not previously available, additional modern data, correcting for instrumental biases of bathythermograph data, and correcting or excluding some Argo float data. The strong interdecadal variability of global ocean heat content reported previously by us is reduced in magnitude but the linear trend in ocean heat content remain similar to our earlier estimate.

机译：我们根据以前无法获得的历史数据，其他现代数据，校正水温计数据的仪器偏差以及校正或排除某些Argo浮标数据，提供1955-2008年世界海洋变暖的估算值。我们先前报告的全球海洋热量含量的年代际强变化幅度减小了，但海洋热量含量的线性趋势仍与我们先前的估计相似。

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《Geophysical Research Letters》 |2009年第7期|共5页
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S. Levitus; J. I. Antonov; T. P. Boyer; R. A. Locarnini; H. E. Garcia; A. V. Mishonov;
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1. Global ocean heat content 1955-2008 in light of recently revealed instrumentation problems [J] . S. Levitus, J. I. Antonov, T. P. Boyer, Geophysical Research Letters . 2009,第7期

机译：鉴于最近发现的仪器仪表问题，1955-2008年全球海洋热含量
2. A global probabilistic study of the ocean heat content low-frequency variability: Atmospheric forcing versus oceanic chaos [J] . Serazin Guillaume, Jaymond Alexandre, Leroux Stephanie, Geophysical Research Letters . 2017,第11期

机译：海洋热含量低频变异性的全球概率研究：大气强制与海洋混乱
3. The upper ocean heat content of the western equatorial Pacific: processes controlling its change during the Tropical Ocean-Global Atmosphere Coupled Ocean-Atmosphere Response Experiment [J] . Richards KJ., Inall ME. Journal of Geophysical Research. Biogeosciences . 2000,第C8期

机译：赤道西太平洋的高层海洋热量：在热带海洋-全球大气耦合海洋-大气响应实验期间控制其变化的过程
4. A REVISED ESTIMATE OF UPPER OCEAN HEAT CONTENT AND IMPLICATIONS FOR THE GLOBAL ENERGY BALANCE [C] . Josh Willis Symposium on 20 Years of Progress in Radar Altimetry . 2013

机译：修订的上海热含量估计和全球能量平衡的影响
5. Possible global surface warming "hiatus" and regional climate response: From a perspective of ocean heat content. [D] . Wu, Xiangbai. 2015

机译：全球表面变暖的可能“裂口”和区域气候响应：从海洋热量含量的角度。
6. Estimating global ocean heat content from tidal magnetic satellite observations [O] . Christopher Irrgang, Jan Saynisch, Maik Thomas -1

机译：根据潮汐卫星观测资料估算全球海洋热量
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。

Global ocean heat content 1955-2008 in light of recently revealed instrumentation problems

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