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Impact of the Ocean Mixed Layer Diurnal Variations on the Intraseasonal Variability of Sea Surface Temperatures in the Atlantic Ocean*

机译：海洋混合层昼夜变化对大西洋海面温度的综合变异性的影响*

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International audience

机译：国际观众

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作者
Virginie Guemas; David Salas-Mélia; Masa Kageyama; Hervé Giordani; Aurore Voldoire;
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年度 2011
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正文语种 eng
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1. Impact of the ocean mixed layer diurnal variations on the intraseasonal variability of sea surface temperatures in the Atlantic Ocean. [J] . Guemas V., Salas-Melia D., Kageyama M., Journal of Climate . 2011,第12期

机译：海洋混合层日变化对大西洋海表温度季节内变化的影响。
2. Impact of intraseasonal wind bursts on sea surface temperature variability in the far eastern tropical Atlantic Ocean during boreal spring 2005 and 2006: focus on the mid-May 2005 event [J] . Herbert Ga?lle, Bourlès Bernard Ocean science . 2018,第4期

机译：在2005年春季和2006年春季期间，季节内风爆发对远东热带大西洋海表温度变化的影响：重点关注2005年5月中旬的事件
3. Impact of intraseasonal wind bursts on sea surface temperature variability in the far eastern tropical Atlantic Ocean during boreal spring 2005 and 2006: focus on the mid-May 2005 event [J] . Herbert Gaelle, Bourles Bernard Ocean science . 2018,第4期

机译：2005年和2006年鲍尔春春季远东热带大西洋海面温度变异性的影响：专注于2005年5月中旬活动
4. The Relationship Between the Sea Surface Temperature Variability within the Southwest Atlantic Ocean and Multivariate ENSO Index [C] . Yu-Chen Hsu, Yi-Chun Liao, Ke-Hsien Fu, International offshore and polar engineering conference . 2013

机译：西南大西洋海表温度变化与多元ENSO指数的关系
5. The influence of variations in penetrating solar radiation on the diurnal and intraseasonal structure of the oceanic boundary layer. [D] . Van Roekel, Luke P. 2010

机译：穿透太阳辐射的变化对海洋边界层的昼夜结构和季节内结构的影响。
6. Bacterial Communities of Surface Mixed Layer in the Pacific Sector of the Western Arctic Ocean during Sea-Ice Melting [O] . Dukki Han, Ilnam Kang, Ho Kyung Ha, -1

机译：西冰洋太平洋冰期融化过程中表面混合层的细菌群落
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。

Impact of the Ocean Mixed Layer Diurnal Variations on the Intraseasonal Variability of Sea Surface Temperatures in the Atlantic Ocean*

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