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Mixed-Layer Parameterization in Models of the Indian Ocean, Grant Number N00014-91-J-4008

机译：印度洋模型中的混合层参数化，授权号N00014-91-J-4008

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作者
McCreary, J. P.;
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年度 1992
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总页数 2
原文格式 PDF
正文语种 eng
中图分类工业技术;
关键词
Mixed layer(Marine); Indian Ocean; Digital simulation; Ocean currents;

机译：混合层（海洋）;印度洋;数字模拟;洋流;

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专利

1. SENSITIVITY OF UPPER OCEAN DYNAMICS IN HIGH-RESOLUTION TROPICAL INDIAN OCEAN MODEL TO DIFFERENT FLUX PARAMETERIZATION: CASE STUDY FOR THE BAY OF BENGAL (BOB) [J] . Mallick S. K., Agarwal N., Sharma R., International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences . 2018,第2aW8期

机译：高分辨率热带印度洋模式上洋流动力学对不同通量参数的敏感性：以孟加拉湾（BOB）为例
2. Modeling aerosol effects on shallow cumulus convection under various meteorological conditions observed over the Indian Ocean and implications for development of mass-flux parameterizations for climate models [J] . Hailong Wang, Greg M. McFarquhar Journal of Geophysical Research, D. Atmospheres: JGR . 2008,第d20期

机译：在印度洋上观测到的各种气象条件下，对浅层积云对流的气溶胶效应建模及其对气候模型质量通量参数化发展的启示
3. Improved boreal summer intraseasonal oscillation simulations over the Indian Ocean by modifying moist parameterizations in climate models [J] . Yang Young-Min, Cho Jeong-A, Moon Ja-Yeon, Climate dynamics . 2021,第9a10期

机译：通过修改气候模型的湿润参数，改善了印度洋的北方夏季陷入困境振荡模拟
4. Mixed-layer modelling at ocean weathership station bravo [C] . S. J. D. DAlessio International Conference on Computational Methods in Multiphase Flow . 2001

机译：混合层建模在海洋瓦尔摩站Bravo
5. The Sensitivity of the Tropical Atmosphere to Changes in Mixed-Layer Depth and Ocean Heat Flux Convergence over the Indian Ocean [D] . Cicerone, Teresa. 2020

机译：热带气氛对印度洋的混合层深度和海洋热通量收敛变化的敏感性
6. Modelling temporal dynamics of Culicoides Latreille (Diptera: Ceratopogonidae) populations on Reunion Island (Indian Ocean) vectors of viruses of veterinary importance [O] . Yannick Grimaud, Hélène Guis, Frédéric Chiroleu, 2019

机译：建模留尼汪岛（印度洋）上的Culicoides Latreille（Diptera：Ceratopogonidae）种群的时间动态这是具有重要兽医意义的病毒的载体
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. Mixed-Layer Parameterizations in Models of the Indian Ocean Circulation [R] . Luther, M. E. 1994

机译：印度洋环流模型中的混合层参数化

Mixed-Layer Parameterization in Models of the Indian Ocean, Grant Number N00014-91-J-4008

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