The abrupt increase in the Aegean sea surface temperature during June 2007 – a marine heatwave event?

Mavrakis Anastasios F.; Tsiros Ioannis X.

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The abrupt increase in the Aegean sea surface temperature during June 2007 – a marine heatwave event?

机译：2007年6月期间爱琴海表面温度突然增加 - 海洋热风事件？

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《Weather》 |2019年第6期|共1页
作者
Mavrakis Anastasios F.; Tsiros Ioannis X.;
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Department of Economic and Regional Development Institute of Urban Environment and Human ResourcesPanteion UniversityAthens;

Meteorology LaboratoryAgricultural University of Athens;

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正文语种 eng
中图分类大气科学（气象学）;
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1. The abrupt increase in the Aegean sea surface temperature during June 2007 – a marine heatwave event? [J] . Mavrakis Anastasios F., Tsiros Ioannis X. Weather . 2019,第6期

机译：2007年6月期间爱琴海表面温度突然增加 - 海洋热风事件？
2. Zooplankton responses to increasing sea surface temperatures in the southeastern Australia global marine hotspot [J] . Kelly Paige, Clementson Lesley, Davies Claire, Estuarine Coastal and Shelf Science . 2016,第octa5期

机译：浮游动物对澳大利亚东南部全球海洋热点海平面温度升高的反应
3. Coral bleaching due to increased sea surface temperature in Gulf of Kachchh Region, India, during June 2016 [J] . Arora Mohit, Chaudhury Nandini Ray, Gujrati Ashwin, Indian Journal of Marine Sciences . 2019,第3期

机译：珊瑚漂白由于印度克拉赫地区海湾的海面温度增加，2016年6月
4. Assessing the utility of thermal Earth observation data to quantify City-scale temperature dynamics during heatwave events [C] . Tomas Holderness, Stuart Barr, Richard Dawson, RSPSoc annual conference and Irish earth observation symposium 2010 . 2010

机译：评估地球热观测数据的实用性，以量化热浪事件期间城市规模的温度动态
5. Seas in Hot Water: Marine Heatwaves on the Move; Following the Heat [D] . Scannell, Hillary A. 2020

机译：海域在热水中：海洋热浪在移动; 在热量之后
6. Impact of marine heatwaves for sea turtle nest temperatures [O] . Graeme C. Hays, William J. Chivers, Jacques-Olivier Laloë, 2021

机译：海龟巢温度的海洋热浪的影响
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. I. Selective Sorption of Bacteria from Seawater. Ii. Mechanism of the Initial Events in the Sorption of Marine Bacteria to Surfaces [R] . Marshall, K. C., Stout, R., Mitchell, R. 1970

机译：I.海水中细菌的选择性吸附。二。海洋细菌吸附到表面的初始事件机制

The abrupt increase in the Aegean sea surface temperature during June 2007 – a marine heatwave event?

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