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Trends and interannual variability of the South China Sea surface winds, surface height, and surface temperature in the recent decade

机译：南海地表风，表面高度和近年来表面温度的趋势和际变化

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Guohong Fang; Haiying Chen; Zexun Wei; Yonggang Wang; Xinyi Wang; Chunyan Li;
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1. Trends and interannual variability of the South China Sea surface winds, surface height, and surface temperature in the recent decade [J] . Guohong Fang, Haiying Chen, Zexun Wei, Journal of Geophysical Research, C. Oceans: JGR . 2006,第c11期

机译：近十年来南海地表风，地表高度和地表温度的趋势和年际变化
2. Interannual variability and trends in sea surface temperature, sea surface wind, and sea level anomaly in the South China Sea [J] . Liu Chunli, Li Xue, Wang Sufen, International journal of remote sensing . 2020,第11a12期

机译：南海海面温度，海面风和海平面异常的依赖性变异性和趋势
3. Trends and Interannual Variability of Satellite-Based Wind and Sea Surface Temperature over the Southern Ocean in the Recent Decade [J] . Shailesh Mohan Pednekar International Journal of Geosciences . 2015,第2期

机译：近十年来南大洋基于卫星的风和海面温度的趋势和年际变化
4. Seasonal and interannual variability of sea surface wind over the China seas and its adjacent ocean from QuikSCAT and ASCAT data during 2000-2011 [C] . Xiaoyan Chen, Delu Pan, Xianqiang He, Conference on remote sensing of the ocean, sea ice, coastal waters, and large water regions . 2012

机译：从2000-2011年QuikSCAT和ASCAT数据看中国海及其邻近海域海面风的季节和年际变化。
5. Interannual variability of the sea surface temperature and the overlying atmospheric circulation in the western South Atlantic [D] . Venegas, Silvia Andrea. 1996

机译：南大西洋西部海表温度和上层大气环流的年际变化
6. The role of atmospheric internal variability on the prediction skill of interannual North Pacific sea-surface temperatures [O] . Balachandrudu Narapusetty -1

机译：大气内部变化对北太平洋海表温度年际预报技术的作用
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。

Trends and interannual variability of the South China Sea surface winds, surface height, and surface temperature in the recent decade

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